triplets
list | passage
stringlengths 56
13.5k
| label_str
stringlengths 5
48
| passage_id
float64 58
38.4k
⌀ | __index_level_0__
int64 0
529k
|
|---|---|---|---|---|
[
"Koloshma",
"country",
"Russia"
] |
Find the relation between <e1>Koloshma<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
country
| null | 41,279 |
[
"Nozhema Rivers",
"country",
"Russia"
] |
Find the relation between <e1>Nozhema Rivers<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
country
| null | 41,280 |
[
"Khvalevskoye Manor",
"country",
"Russia"
] |
Find the relation between <e1>Khvalevskoye Manor<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
country
| null | 41,281 |
[
"Borisovo",
"country",
"Russia"
] |
Find the relation between <e1>Borisovo<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
country
| null | 41,282 |
[
"Kolp",
"country",
"Russia"
] |
Find the relation between <e1>Kolp<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
country
| null | 41,283 |
[
"Andoga",
"country",
"Russia"
] |
Find the relation between <e1>Andoga<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
country
| null | 41,285 |
[
"Rybinsk Reservoir",
"country",
"Russia"
] |
Find the relation between <e1>Rybinsk Reservoir<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
country
| null | 41,287 |
[
"Vologda Oblast",
"located in the administrative territorial entity",
"Russia"
] |
Find the relation between <e1>Vologda Oblast<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
located in the administrative territorial entity
| null | 41,289 |
[
"Vologda Oblast",
"country",
"Russia"
] |
Find the relation between <e1>Vologda Oblast<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
country
| null | 41,290 |
[
"Belozersky",
"country",
"Russia"
] |
Find the relation between <e1>Belozersky<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
country
| null | 41,297 |
[
"Belozersky",
"located in the administrative territorial entity",
"Vologda Oblast"
] |
Find the relation between <e1>Belozersky<\e1> and <e2>Vologda Oblast<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
located in the administrative territorial entity
| null | 41,298 |
[
"Boksitogorsky District",
"country",
"Russia"
] |
Find the relation between <e1>Boksitogorsky District<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
country
| null | 41,299 |
[
"Vytegorsky",
"country",
"Russia"
] |
Find the relation between <e1>Vytegorsky<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
country
| null | 41,300 |
[
"Vytegorsky",
"located in the administrative territorial entity",
"Vologda Oblast"
] |
Find the relation between <e1>Vytegorsky<\e1> and <e2>Vologda Oblast<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
located in the administrative territorial entity
| null | 41,301 |
[
"Ustyuzhensky Districts",
"country",
"Russia"
] |
Find the relation between <e1>Ustyuzhensky Districts<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
country
| null | 41,302 |
[
"Ustyuzhensky Districts",
"located in the administrative territorial entity",
"Vologda Oblast"
] |
Find the relation between <e1>Ustyuzhensky Districts<\e1> and <e2>Vologda Oblast<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
located in the administrative territorial entity
| null | 41,303 |
[
"Tikhvinsky",
"country",
"Russia"
] |
Find the relation between <e1>Tikhvinsky<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
country
| null | 41,304 |
[
"Tikhvinsky",
"located in the administrative territorial entity",
"Leningrad Oblast"
] |
Find the relation between <e1>Tikhvinsky<\e1> and <e2>Leningrad Oblast<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
located in the administrative territorial entity
| null | 41,305 |
[
"Podporozhsky Districts",
"country",
"Russia"
] |
Find the relation between <e1>Podporozhsky Districts<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
country
| null | 41,306 |
[
"Podporozhsky Districts",
"located in the administrative territorial entity",
"Leningrad Oblast"
] |
Find the relation between <e1>Podporozhsky Districts<\e1> and <e2>Leningrad Oblast<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
located in the administrative territorial entity
| null | 41,307 |
[
"Suda",
"country",
"Russia"
] |
Find the relation between <e1>Suda<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
country
| null | 41,308 |
[
"Suda",
"located in the administrative territorial entity",
"Vologda Oblast"
] |
Find the relation between <e1>Suda<\e1> and <e2>Vologda Oblast<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
located in the administrative territorial entity
| null | 41,311 |
[
"Sudsky",
"country",
"Russia"
] |
Find the relation between <e1>Sudsky<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
country
| null | 41,312 |
[
"Sudskoye",
"country",
"Russia"
] |
Find the relation between <e1>Sudskoye<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
country
| null | 41,313 |
[
"Boksitogorsky District",
"located in the administrative territorial entity",
"Leningrad Oblast"
] |
Find the relation between <e1>Boksitogorsky District<\e1> and <e2>Leningrad Oblast<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
located in the administrative territorial entity
| null | 41,314 |
[
"Kaduysky",
"capital",
"Kaduy"
] |
Find the relation between <e1>Kaduysky<\e1> and <e2>Kaduy<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
capital
| null | 41,315 |
[
"Kaduy",
"capital of",
"Kaduysky"
] |
Find the relation between <e1>Kaduy<\e1> and <e2>Kaduysky<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
capital of
| null | 41,317 |
[
"Kaduy",
"located in the administrative territorial entity",
"Kaduysky"
] |
Find the relation between <e1>Kaduy<\e1> and <e2>Kaduysky<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
located in the administrative territorial entity
| null | 41,323 |
[
"Volga River",
"located in the administrative territorial entity",
"Russia"
] |
Find the relation between <e1>Volga River<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
located in the administrative territorial entity
| null | 41,324 |
[
"Voron",
"located in the administrative territorial entity",
"Russia"
] |
Find the relation between <e1>Voron<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
located in the administrative territorial entity
| null | 41,325 |
[
"Kaduy",
"located in the administrative territorial entity",
"Russia"
] |
Find the relation between <e1>Kaduy<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
located in the administrative territorial entity
| null | 41,326 |
[
"Lake Andozero",
"located in the administrative territorial entity",
"Russia"
] |
Find the relation between <e1>Lake Andozero<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
located in the administrative territorial entity
| null | 41,327 |
[
"Babayevsky",
"located in the administrative territorial entity",
"Russia"
] |
Find the relation between <e1>Babayevsky<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
located in the administrative territorial entity
| null | 41,328 |
[
"Kaduysky",
"located in the administrative territorial entity",
"Russia"
] |
Find the relation between <e1>Kaduysky<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
located in the administrative territorial entity
| null | 41,329 |
[
"Cherepovetsky",
"located in the administrative territorial entity",
"Russia"
] |
Find the relation between <e1>Cherepovetsky<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
located in the administrative territorial entity
| null | 41,330 |
[
"Shogda",
"located in the administrative territorial entity",
"Russia"
] |
Find the relation between <e1>Shogda<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
located in the administrative territorial entity
| null | 41,331 |
[
"Petukh",
"located in the administrative territorial entity",
"Russia"
] |
Find the relation between <e1>Petukh<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
located in the administrative territorial entity
| null | 41,332 |
[
"Koloshma",
"located in the administrative territorial entity",
"Russia"
] |
Find the relation between <e1>Koloshma<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
located in the administrative territorial entity
| null | 41,333 |
[
"Nozhema Rivers",
"located in the administrative territorial entity",
"Russia"
] |
Find the relation between <e1>Nozhema Rivers<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
located in the administrative territorial entity
| null | 41,334 |
[
"Khvalevskoye Manor",
"located in the administrative territorial entity",
"Russia"
] |
Find the relation between <e1>Khvalevskoye Manor<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
located in the administrative territorial entity
| null | 41,335 |
[
"Borisovo",
"located in the administrative territorial entity",
"Russia"
] |
Find the relation between <e1>Borisovo<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
located in the administrative territorial entity
| null | 41,336 |
[
"Kolp",
"located in the administrative territorial entity",
"Russia"
] |
Find the relation between <e1>Kolp<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
located in the administrative territorial entity
| null | 41,337 |
[
"Andoga",
"located in the administrative territorial entity",
"Russia"
] |
Find the relation between <e1>Andoga<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
located in the administrative territorial entity
| null | 41,338 |
[
"Rybinsk Reservoir",
"located in the administrative territorial entity",
"Russia"
] |
Find the relation between <e1>Rybinsk Reservoir<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
located in the administrative territorial entity
| null | 41,339 |
[
"Belozersky",
"located in the administrative territorial entity",
"Russia"
] |
Find the relation between <e1>Belozersky<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
located in the administrative territorial entity
| null | 41,340 |
[
"Boksitogorsky District",
"located in the administrative territorial entity",
"Russia"
] |
Find the relation between <e1>Boksitogorsky District<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
located in the administrative territorial entity
| null | 41,341 |
[
"Vytegorsky",
"located in the administrative territorial entity",
"Russia"
] |
Find the relation between <e1>Vytegorsky<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
located in the administrative territorial entity
| null | 41,342 |
[
"Ustyuzhensky Districts",
"located in the administrative territorial entity",
"Russia"
] |
Find the relation between <e1>Ustyuzhensky Districts<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
located in the administrative territorial entity
| null | 41,343 |
[
"Tikhvinsky",
"located in the administrative territorial entity",
"Russia"
] |
Find the relation between <e1>Tikhvinsky<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
located in the administrative territorial entity
| null | 41,344 |
[
"Podporozhsky Districts",
"located in the administrative territorial entity",
"Russia"
] |
Find the relation between <e1>Podporozhsky Districts<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
located in the administrative territorial entity
| null | 41,345 |
[
"Suda",
"located in the administrative territorial entity",
"Russia"
] |
Find the relation between <e1>Suda<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
located in the administrative territorial entity
| null | 41,346 |
[
"Sudsky",
"located in the administrative territorial entity",
"Russia"
] |
Find the relation between <e1>Sudsky<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
located in the administrative territorial entity
| null | 41,347 |
[
"Sudskoye",
"located in the administrative territorial entity",
"Russia"
] |
Find the relation between <e1>Sudskoye<\e1> and <e2>Russia<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
located in the administrative territorial entity
| null | 41,348 |
[
"Kaduy",
"located in the administrative territorial entity",
"Vologda Oblast"
] |
Find the relation between <e1>Kaduy<\e1> and <e2>Vologda Oblast<\e2>.
The Suda () is a river in Babayevsky, Kaduysky, and Cherepovetsky Districts of Vologda Oblast in Russia. It flows into the Rybinsk Reservoir of the Volga River. It is long, with a drainage basin of and an average discharge of. Its main tributaries are the Shogda, the Andoga, the Kolp, the Voron and the Petukh rivers. The source of the Suda is the confluence of the Koloshma and the Nozhema Rivers in the northwest of Babayevsky District of Vologda Oblast, close to the border with Leningrad Oblast. The river flows in the general direction southeast. Almost the whole valley of the Suda is populated. The selo of Borisovo - Sudskoye, located in the upper course of the river, is named after the Suda. Between 1927 and 1959 it was an administrative center of Borisovo - Sudsky District of Leningrad Oblast and of Vologda Oblast. The historic Khvalevskoye Manor is located in the selo of Borisovo - Sudskoye on a 30-meter high banks of the Suda river. In the lower course, between the mouths of the Kolp (left) and the Andoga (right) the Suda runs close to the urban - type settlement of Kaduy, the center of Kaduysky District, located on the left bank. The mouth of the Suda is located in the settlement of Suda, and the lower course is essentially a bay of the Rybinsk Reservoir. The river basin of the Suda comprises vast area in the west of Vologda Oblast, in particular, almost all of Babayevsky District, almost all of Kaduysky District, large areas in Belozersky and Cherepovetsky District of Vologda Oblast and in Boksitogorsky District of Leningrad Oblast, as well as minor areas in Vytegorsky and Ustyuzhensky Districts of Vologda Oblast and Tikhvinsky and Podporozhsky Districts of Leningrad Oblast. There are many lakes in the river basin of the Suda, mostly of glacial origin. The biggest of the lakes is Lake Andozero in Belozersky District. The lower course of the Suda () is listed in the State Water Register of Russia as navigable, however, there is no passenger navigation.
|
located in the administrative territorial entity
| null | 41,349 |
[
"Channel Five",
"owned by",
"Sony Pictures Television International"
] |
Find the relation between <e1>Channel Five<\e1> and <e2>Sony Pictures Television International<\e2>.
Sofia's Diary is a drama that is shown online through the social networking site Bebo, which is the same site that hosts KateModern. A version of Sofia's Diary originally came out in 2003 in Portugal. This means it actually predates the first video of lonelygirl15 which came out in 2006. Sofia is played by 22-year - old Rachel Hyde - Harvey. Sofia's Diary was the second internet based show to make the transition to UK TV (Tiscali Showcase on C4 being the first in 2007) following its acquisition by Channel Five (from Sony Pictures Television International) on 17 April 2008. The first two seasons of the show were broadcast on' Fiver' (previously' Five Life'). Following an 8-month break, Sofia's Diary returned to Bebo to begin a 6-week third season, from 29 May 2009. This season differs to the first two, in that new episodes are only being shown on Tuesdays and Fridays, as opposed to every weekday. Sure Girl originally sponsored Sofia's Diary. Season 3 of the show is being exclusively sponsored by Transport for London (TfL), to help increase awareness among teenagers of its road safety campaign.
|
owned by
| null | 42,109 |
[
"Alfred Louis Olivier Legrand Des Cloizeaux",
"member of",
"French Academy of Sciences"
] |
Find the relation between <e1>Alfred Louis Olivier Legrand Des Cloizeaux<\e1> and <e2>French Academy of Sciences<\e2>.
Alfred Louis Olivier Legrand Des Cloizeaux (17 October 18176 May 1897) was a French mineralogist. Des Cloizeaux was born at Beauvais, in the department of Oise. He studied with Jean - Baptiste Biot at the Collège de France. He became professor of mineralogy at the École Normale Supérieure and afterwards at the Muséum National d'Histoire Naturelle in Paris. He studied the geysers of Iceland, and wrote also on the classification of some of the eruptive rocks. His main work consisted in the systematic examination of the crystals of numerous minerals, in researches on their optical properties and on the subject of light polarization. He demonstrated the circular polarization of cinnabar. He wrote especially on the means of determining the different feldspars, and is credited with the discovery of microcline (a triclinic potash - feldspar). He named the minerals montebrasite (1871), binnite (a variety of tennantite) and Christianite (in honor of Christian VIII of Denmark). In 1854, Alexis Damour dedicated the mineral descloizite in honor of Des Cloizeaux. Des Cloizeaux was elected as a member of the French Academy of Sciences in 1869, and was its President in 1889. He was awarded the Wollaston Medal by the Geological Society of London in 1886. His best - known books are Leçons de cristallographie (1861) and Manuel de minéralogie (2 vols. , Paris, 1862, 1874 and 1893).
|
member of
| null | 42,257 |
[
"Alfred Louis Olivier Legrand Des Cloizeaux",
"place of birth",
"Beauvais"
] |
Find the relation between <e1>Alfred Louis Olivier Legrand Des Cloizeaux<\e1> and <e2>Beauvais<\e2>.
Alfred Louis Olivier Legrand Des Cloizeaux (17 October 18176 May 1897) was a French mineralogist. Des Cloizeaux was born at Beauvais, in the department of Oise. He studied with Jean - Baptiste Biot at the Collège de France. He became professor of mineralogy at the École Normale Supérieure and afterwards at the Muséum National d'Histoire Naturelle in Paris. He studied the geysers of Iceland, and wrote also on the classification of some of the eruptive rocks. His main work consisted in the systematic examination of the crystals of numerous minerals, in researches on their optical properties and on the subject of light polarization. He demonstrated the circular polarization of cinnabar. He wrote especially on the means of determining the different feldspars, and is credited with the discovery of microcline (a triclinic potash - feldspar). He named the minerals montebrasite (1871), binnite (a variety of tennantite) and Christianite (in honor of Christian VIII of Denmark). In 1854, Alexis Damour dedicated the mineral descloizite in honor of Des Cloizeaux. Des Cloizeaux was elected as a member of the French Academy of Sciences in 1869, and was its President in 1889. He was awarded the Wollaston Medal by the Geological Society of London in 1886. His best - known books are Leçons de cristallographie (1861) and Manuel de minéralogie (2 vols. , Paris, 1862, 1874 and 1893).
|
place of birth
| null | 42,258 |
[
"Paris",
"country",
"French"
] |
Find the relation between <e1>Paris<\e1> and <e2>French<\e2>.
Alfred Louis Olivier Legrand Des Cloizeaux (17 October 18176 May 1897) was a French mineralogist. Des Cloizeaux was born at Beauvais, in the department of Oise. He studied with Jean - Baptiste Biot at the Collège de France. He became professor of mineralogy at the École Normale Supérieure and afterwards at the Muséum National d'Histoire Naturelle in Paris. He studied the geysers of Iceland, and wrote also on the classification of some of the eruptive rocks. His main work consisted in the systematic examination of the crystals of numerous minerals, in researches on their optical properties and on the subject of light polarization. He demonstrated the circular polarization of cinnabar. He wrote especially on the means of determining the different feldspars, and is credited with the discovery of microcline (a triclinic potash - feldspar). He named the minerals montebrasite (1871), binnite (a variety of tennantite) and Christianite (in honor of Christian VIII of Denmark). In 1854, Alexis Damour dedicated the mineral descloizite in honor of Des Cloizeaux. Des Cloizeaux was elected as a member of the French Academy of Sciences in 1869, and was its President in 1889. He was awarded the Wollaston Medal by the Geological Society of London in 1886. His best - known books are Leçons de cristallographie (1861) and Manuel de minéralogie (2 vols. , Paris, 1862, 1874 and 1893).
|
country
| null | 42,260 |
[
"Christian VIII",
"country of citizenship",
"Denmark"
] |
Find the relation between <e1>Christian VIII<\e1> and <e2>Denmark<\e2>.
Alfred Louis Olivier Legrand Des Cloizeaux (17 October 18176 May 1897) was a French mineralogist. Des Cloizeaux was born at Beauvais, in the department of Oise. He studied with Jean - Baptiste Biot at the Collège de France. He became professor of mineralogy at the École Normale Supérieure and afterwards at the Muséum National d'Histoire Naturelle in Paris. He studied the geysers of Iceland, and wrote also on the classification of some of the eruptive rocks. His main work consisted in the systematic examination of the crystals of numerous minerals, in researches on their optical properties and on the subject of light polarization. He demonstrated the circular polarization of cinnabar. He wrote especially on the means of determining the different feldspars, and is credited with the discovery of microcline (a triclinic potash - feldspar). He named the minerals montebrasite (1871), binnite (a variety of tennantite) and Christianite (in honor of Christian VIII of Denmark). In 1854, Alexis Damour dedicated the mineral descloizite in honor of Des Cloizeaux. Des Cloizeaux was elected as a member of the French Academy of Sciences in 1869, and was its President in 1889. He was awarded the Wollaston Medal by the Geological Society of London in 1886. His best - known books are Leçons de cristallographie (1861) and Manuel de minéralogie (2 vols. , Paris, 1862, 1874 and 1893).
|
country of citizenship
| null | 42,261 |
[
"French Academy of Sciences",
"country",
"French"
] |
Find the relation between <e1>French Academy of Sciences<\e1> and <e2>French<\e2>.
Alfred Louis Olivier Legrand Des Cloizeaux (17 October 18176 May 1897) was a French mineralogist. Des Cloizeaux was born at Beauvais, in the department of Oise. He studied with Jean - Baptiste Biot at the Collège de France. He became professor of mineralogy at the École Normale Supérieure and afterwards at the Muséum National d'Histoire Naturelle in Paris. He studied the geysers of Iceland, and wrote also on the classification of some of the eruptive rocks. His main work consisted in the systematic examination of the crystals of numerous minerals, in researches on their optical properties and on the subject of light polarization. He demonstrated the circular polarization of cinnabar. He wrote especially on the means of determining the different feldspars, and is credited with the discovery of microcline (a triclinic potash - feldspar). He named the minerals montebrasite (1871), binnite (a variety of tennantite) and Christianite (in honor of Christian VIII of Denmark). In 1854, Alexis Damour dedicated the mineral descloizite in honor of Des Cloizeaux. Des Cloizeaux was elected as a member of the French Academy of Sciences in 1869, and was its President in 1889. He was awarded the Wollaston Medal by the Geological Society of London in 1886. His best - known books are Leçons de cristallographie (1861) and Manuel de minéralogie (2 vols. , Paris, 1862, 1874 and 1893).
|
country
| null | 42,262 |
[
"Beauvais",
"located in the administrative territorial entity",
"Oise"
] |
Find the relation between <e1>Beauvais<\e1> and <e2>Oise<\e2>.
Alfred Louis Olivier Legrand Des Cloizeaux (17 October 18176 May 1897) was a French mineralogist. Des Cloizeaux was born at Beauvais, in the department of Oise. He studied with Jean - Baptiste Biot at the Collège de France. He became professor of mineralogy at the École Normale Supérieure and afterwards at the Muséum National d'Histoire Naturelle in Paris. He studied the geysers of Iceland, and wrote also on the classification of some of the eruptive rocks. His main work consisted in the systematic examination of the crystals of numerous minerals, in researches on their optical properties and on the subject of light polarization. He demonstrated the circular polarization of cinnabar. He wrote especially on the means of determining the different feldspars, and is credited with the discovery of microcline (a triclinic potash - feldspar). He named the minerals montebrasite (1871), binnite (a variety of tennantite) and Christianite (in honor of Christian VIII of Denmark). In 1854, Alexis Damour dedicated the mineral descloizite in honor of Des Cloizeaux. Des Cloizeaux was elected as a member of the French Academy of Sciences in 1869, and was its President in 1889. He was awarded the Wollaston Medal by the Geological Society of London in 1886. His best - known books are Leçons de cristallographie (1861) and Manuel de minéralogie (2 vols. , Paris, 1862, 1874 and 1893).
|
located in the administrative territorial entity
| null | 42,263 |
[
"Collège de France",
"country",
"French"
] |
Find the relation between <e1>Collège de France<\e1> and <e2>French<\e2>.
Alfred Louis Olivier Legrand Des Cloizeaux (17 October 18176 May 1897) was a French mineralogist. Des Cloizeaux was born at Beauvais, in the department of Oise. He studied with Jean - Baptiste Biot at the Collège de France. He became professor of mineralogy at the École Normale Supérieure and afterwards at the Muséum National d'Histoire Naturelle in Paris. He studied the geysers of Iceland, and wrote also on the classification of some of the eruptive rocks. His main work consisted in the systematic examination of the crystals of numerous minerals, in researches on their optical properties and on the subject of light polarization. He demonstrated the circular polarization of cinnabar. He wrote especially on the means of determining the different feldspars, and is credited with the discovery of microcline (a triclinic potash - feldspar). He named the minerals montebrasite (1871), binnite (a variety of tennantite) and Christianite (in honor of Christian VIII of Denmark). In 1854, Alexis Damour dedicated the mineral descloizite in honor of Des Cloizeaux. Des Cloizeaux was elected as a member of the French Academy of Sciences in 1869, and was its President in 1889. He was awarded the Wollaston Medal by the Geological Society of London in 1886. His best - known books are Leçons de cristallographie (1861) and Manuel de minéralogie (2 vols. , Paris, 1862, 1874 and 1893).
|
country
| null | 42,264 |
[
"École Normale Supérieure",
"headquarters location",
"Paris"
] |
Find the relation between <e1>École Normale Supérieure<\e1> and <e2>Paris<\e2>.
Alfred Louis Olivier Legrand Des Cloizeaux (17 October 18176 May 1897) was a French mineralogist. Des Cloizeaux was born at Beauvais, in the department of Oise. He studied with Jean - Baptiste Biot at the Collège de France. He became professor of mineralogy at the École Normale Supérieure and afterwards at the Muséum National d'Histoire Naturelle in Paris. He studied the geysers of Iceland, and wrote also on the classification of some of the eruptive rocks. His main work consisted in the systematic examination of the crystals of numerous minerals, in researches on their optical properties and on the subject of light polarization. He demonstrated the circular polarization of cinnabar. He wrote especially on the means of determining the different feldspars, and is credited with the discovery of microcline (a triclinic potash - feldspar). He named the minerals montebrasite (1871), binnite (a variety of tennantite) and Christianite (in honor of Christian VIII of Denmark). In 1854, Alexis Damour dedicated the mineral descloizite in honor of Des Cloizeaux. Des Cloizeaux was elected as a member of the French Academy of Sciences in 1869, and was its President in 1889. He was awarded the Wollaston Medal by the Geological Society of London in 1886. His best - known books are Leçons de cristallographie (1861) and Manuel de minéralogie (2 vols. , Paris, 1862, 1874 and 1893).
|
headquarters location
| null | 42,265 |
[
"École Normale Supérieure",
"country",
"French"
] |
Find the relation between <e1>École Normale Supérieure<\e1> and <e2>French<\e2>.
Alfred Louis Olivier Legrand Des Cloizeaux (17 October 18176 May 1897) was a French mineralogist. Des Cloizeaux was born at Beauvais, in the department of Oise. He studied with Jean - Baptiste Biot at the Collège de France. He became professor of mineralogy at the École Normale Supérieure and afterwards at the Muséum National d'Histoire Naturelle in Paris. He studied the geysers of Iceland, and wrote also on the classification of some of the eruptive rocks. His main work consisted in the systematic examination of the crystals of numerous minerals, in researches on their optical properties and on the subject of light polarization. He demonstrated the circular polarization of cinnabar. He wrote especially on the means of determining the different feldspars, and is credited with the discovery of microcline (a triclinic potash - feldspar). He named the minerals montebrasite (1871), binnite (a variety of tennantite) and Christianite (in honor of Christian VIII of Denmark). In 1854, Alexis Damour dedicated the mineral descloizite in honor of Des Cloizeaux. Des Cloizeaux was elected as a member of the French Academy of Sciences in 1869, and was its President in 1889. He was awarded the Wollaston Medal by the Geological Society of London in 1886. His best - known books are Leçons de cristallographie (1861) and Manuel de minéralogie (2 vols. , Paris, 1862, 1874 and 1893).
|
country
| null | 42,266 |
[
"Muséum National d'Histoire Naturelle",
"located in the administrative territorial entity",
"Paris"
] |
Find the relation between <e1>Muséum National d'Histoire Naturelle<\e1> and <e2>Paris<\e2>.
Alfred Louis Olivier Legrand Des Cloizeaux (17 October 18176 May 1897) was a French mineralogist. Des Cloizeaux was born at Beauvais, in the department of Oise. He studied with Jean - Baptiste Biot at the Collège de France. He became professor of mineralogy at the École Normale Supérieure and afterwards at the Muséum National d'Histoire Naturelle in Paris. He studied the geysers of Iceland, and wrote also on the classification of some of the eruptive rocks. His main work consisted in the systematic examination of the crystals of numerous minerals, in researches on their optical properties and on the subject of light polarization. He demonstrated the circular polarization of cinnabar. He wrote especially on the means of determining the different feldspars, and is credited with the discovery of microcline (a triclinic potash - feldspar). He named the minerals montebrasite (1871), binnite (a variety of tennantite) and Christianite (in honor of Christian VIII of Denmark). In 1854, Alexis Damour dedicated the mineral descloizite in honor of Des Cloizeaux. Des Cloizeaux was elected as a member of the French Academy of Sciences in 1869, and was its President in 1889. He was awarded the Wollaston Medal by the Geological Society of London in 1886. His best - known books are Leçons de cristallographie (1861) and Manuel de minéralogie (2 vols. , Paris, 1862, 1874 and 1893).
|
located in the administrative territorial entity
| null | 42,267 |
[
"Muséum National d'Histoire Naturelle",
"country",
"French"
] |
Find the relation between <e1>Muséum National d'Histoire Naturelle<\e1> and <e2>French<\e2>.
Alfred Louis Olivier Legrand Des Cloizeaux (17 October 18176 May 1897) was a French mineralogist. Des Cloizeaux was born at Beauvais, in the department of Oise. He studied with Jean - Baptiste Biot at the Collège de France. He became professor of mineralogy at the École Normale Supérieure and afterwards at the Muséum National d'Histoire Naturelle in Paris. He studied the geysers of Iceland, and wrote also on the classification of some of the eruptive rocks. His main work consisted in the systematic examination of the crystals of numerous minerals, in researches on their optical properties and on the subject of light polarization. He demonstrated the circular polarization of cinnabar. He wrote especially on the means of determining the different feldspars, and is credited with the discovery of microcline (a triclinic potash - feldspar). He named the minerals montebrasite (1871), binnite (a variety of tennantite) and Christianite (in honor of Christian VIII of Denmark). In 1854, Alexis Damour dedicated the mineral descloizite in honor of Des Cloizeaux. Des Cloizeaux was elected as a member of the French Academy of Sciences in 1869, and was its President in 1889. He was awarded the Wollaston Medal by the Geological Society of London in 1886. His best - known books are Leçons de cristallographie (1861) and Manuel de minéralogie (2 vols. , Paris, 1862, 1874 and 1893).
|
country
| null | 42,268 |
[
"Alfred Louis Olivier Legrand Des Cloizeaux",
"award received",
"Wollaston Medal"
] |
Find the relation between <e1>Alfred Louis Olivier Legrand Des Cloizeaux<\e1> and <e2>Wollaston Medal<\e2>.
Alfred Louis Olivier Legrand Des Cloizeaux (17 October 18176 May 1897) was a French mineralogist. Des Cloizeaux was born at Beauvais, in the department of Oise. He studied with Jean - Baptiste Biot at the Collège de France. He became professor of mineralogy at the École Normale Supérieure and afterwards at the Muséum National d'Histoire Naturelle in Paris. He studied the geysers of Iceland, and wrote also on the classification of some of the eruptive rocks. His main work consisted in the systematic examination of the crystals of numerous minerals, in researches on their optical properties and on the subject of light polarization. He demonstrated the circular polarization of cinnabar. He wrote especially on the means of determining the different feldspars, and is credited with the discovery of microcline (a triclinic potash - feldspar). He named the minerals montebrasite (1871), binnite (a variety of tennantite) and Christianite (in honor of Christian VIII of Denmark). In 1854, Alexis Damour dedicated the mineral descloizite in honor of Des Cloizeaux. Des Cloizeaux was elected as a member of the French Academy of Sciences in 1869, and was its President in 1889. He was awarded the Wollaston Medal by the Geological Society of London in 1886. His best - known books are Leçons de cristallographie (1861) and Manuel de minéralogie (2 vols. , Paris, 1862, 1874 and 1893).
|
award received
| null | 42,269 |
[
"Jean-Baptiste Biot",
"member of",
"French Academy of Sciences"
] |
Find the relation between <e1>Jean-Baptiste Biot<\e1> and <e2>French Academy of Sciences<\e2>.
Alfred Louis Olivier Legrand Des Cloizeaux (17 October 18176 May 1897) was a French mineralogist. Des Cloizeaux was born at Beauvais, in the department of Oise. He studied with Jean - Baptiste Biot at the Collège de France. He became professor of mineralogy at the École Normale Supérieure and afterwards at the Muséum National d'Histoire Naturelle in Paris. He studied the geysers of Iceland, and wrote also on the classification of some of the eruptive rocks. His main work consisted in the systematic examination of the crystals of numerous minerals, in researches on their optical properties and on the subject of light polarization. He demonstrated the circular polarization of cinnabar. He wrote especially on the means of determining the different feldspars, and is credited with the discovery of microcline (a triclinic potash - feldspar). He named the minerals montebrasite (1871), binnite (a variety of tennantite) and Christianite (in honor of Christian VIII of Denmark). In 1854, Alexis Damour dedicated the mineral descloizite in honor of Des Cloizeaux. Des Cloizeaux was elected as a member of the French Academy of Sciences in 1869, and was its President in 1889. He was awarded the Wollaston Medal by the Geological Society of London in 1886. His best - known books are Leçons de cristallographie (1861) and Manuel de minéralogie (2 vols. , Paris, 1862, 1874 and 1893).
|
member of
| null | 42,271 |
[
"Alfred Louis Olivier Legrand Des Cloizeaux",
"country of citizenship",
"French"
] |
Find the relation between <e1>Alfred Louis Olivier Legrand Des Cloizeaux<\e1> and <e2>French<\e2>.
Alfred Louis Olivier Legrand Des Cloizeaux (17 October 18176 May 1897) was a French mineralogist. Des Cloizeaux was born at Beauvais, in the department of Oise. He studied with Jean - Baptiste Biot at the Collège de France. He became professor of mineralogy at the École Normale Supérieure and afterwards at the Muséum National d'Histoire Naturelle in Paris. He studied the geysers of Iceland, and wrote also on the classification of some of the eruptive rocks. His main work consisted in the systematic examination of the crystals of numerous minerals, in researches on their optical properties and on the subject of light polarization. He demonstrated the circular polarization of cinnabar. He wrote especially on the means of determining the different feldspars, and is credited with the discovery of microcline (a triclinic potash - feldspar). He named the minerals montebrasite (1871), binnite (a variety of tennantite) and Christianite (in honor of Christian VIII of Denmark). In 1854, Alexis Damour dedicated the mineral descloizite in honor of Des Cloizeaux. Des Cloizeaux was elected as a member of the French Academy of Sciences in 1869, and was its President in 1889. He was awarded the Wollaston Medal by the Geological Society of London in 1886. His best - known books are Leçons de cristallographie (1861) and Manuel de minéralogie (2 vols. , Paris, 1862, 1874 and 1893).
|
country of citizenship
| null | 42,272 |
[
"Alfred Louis Olivier Legrand Des Cloizeaux",
"place of death",
"Paris"
] |
Find the relation between <e1>Alfred Louis Olivier Legrand Des Cloizeaux<\e1> and <e2>Paris<\e2>.
Alfred Louis Olivier Legrand Des Cloizeaux (17 October 18176 May 1897) was a French mineralogist. Des Cloizeaux was born at Beauvais, in the department of Oise. He studied with Jean - Baptiste Biot at the Collège de France. He became professor of mineralogy at the École Normale Supérieure and afterwards at the Muséum National d'Histoire Naturelle in Paris. He studied the geysers of Iceland, and wrote also on the classification of some of the eruptive rocks. His main work consisted in the systematic examination of the crystals of numerous minerals, in researches on their optical properties and on the subject of light polarization. He demonstrated the circular polarization of cinnabar. He wrote especially on the means of determining the different feldspars, and is credited with the discovery of microcline (a triclinic potash - feldspar). He named the minerals montebrasite (1871), binnite (a variety of tennantite) and Christianite (in honor of Christian VIII of Denmark). In 1854, Alexis Damour dedicated the mineral descloizite in honor of Des Cloizeaux. Des Cloizeaux was elected as a member of the French Academy of Sciences in 1869, and was its President in 1889. He was awarded the Wollaston Medal by the Geological Society of London in 1886. His best - known books are Leçons de cristallographie (1861) and Manuel de minéralogie (2 vols. , Paris, 1862, 1874 and 1893).
|
place of death
| null | 42,273 |
[
"Collège de France",
"located in the administrative territorial entity",
"Paris"
] |
Find the relation between <e1>Collège de France<\e1> and <e2>Paris<\e2>.
Alfred Louis Olivier Legrand Des Cloizeaux (17 October 18176 May 1897) was a French mineralogist. Des Cloizeaux was born at Beauvais, in the department of Oise. He studied with Jean - Baptiste Biot at the Collège de France. He became professor of mineralogy at the École Normale Supérieure and afterwards at the Muséum National d'Histoire Naturelle in Paris. He studied the geysers of Iceland, and wrote also on the classification of some of the eruptive rocks. His main work consisted in the systematic examination of the crystals of numerous minerals, in researches on their optical properties and on the subject of light polarization. He demonstrated the circular polarization of cinnabar. He wrote especially on the means of determining the different feldspars, and is credited with the discovery of microcline (a triclinic potash - feldspar). He named the minerals montebrasite (1871), binnite (a variety of tennantite) and Christianite (in honor of Christian VIII of Denmark). In 1854, Alexis Damour dedicated the mineral descloizite in honor of Des Cloizeaux. Des Cloizeaux was elected as a member of the French Academy of Sciences in 1869, and was its President in 1889. He was awarded the Wollaston Medal by the Geological Society of London in 1886. His best - known books are Leçons de cristallographie (1861) and Manuel de minéralogie (2 vols. , Paris, 1862, 1874 and 1893).
|
located in the administrative territorial entity
| null | 42,274 |
[
"Jean-Baptiste Biot",
"employer",
"Collège de France"
] |
Find the relation between <e1>Jean-Baptiste Biot<\e1> and <e2>Collège de France<\e2>.
Alfred Louis Olivier Legrand Des Cloizeaux (17 October 18176 May 1897) was a French mineralogist. Des Cloizeaux was born at Beauvais, in the department of Oise. He studied with Jean - Baptiste Biot at the Collège de France. He became professor of mineralogy at the École Normale Supérieure and afterwards at the Muséum National d'Histoire Naturelle in Paris. He studied the geysers of Iceland, and wrote also on the classification of some of the eruptive rocks. His main work consisted in the systematic examination of the crystals of numerous minerals, in researches on their optical properties and on the subject of light polarization. He demonstrated the circular polarization of cinnabar. He wrote especially on the means of determining the different feldspars, and is credited with the discovery of microcline (a triclinic potash - feldspar). He named the minerals montebrasite (1871), binnite (a variety of tennantite) and Christianite (in honor of Christian VIII of Denmark). In 1854, Alexis Damour dedicated the mineral descloizite in honor of Des Cloizeaux. Des Cloizeaux was elected as a member of the French Academy of Sciences in 1869, and was its President in 1889. He was awarded the Wollaston Medal by the Geological Society of London in 1886. His best - known books are Leçons de cristallographie (1861) and Manuel de minéralogie (2 vols. , Paris, 1862, 1874 and 1893).
|
employer
| null | 42,275 |
[
"Alfred Louis Olivier Legrand Des Cloizeaux",
"educated at",
"Collège de France"
] |
Find the relation between <e1>Alfred Louis Olivier Legrand Des Cloizeaux<\e1> and <e2>Collège de France<\e2>.
Alfred Louis Olivier Legrand Des Cloizeaux (17 October 18176 May 1897) was a French mineralogist. Des Cloizeaux was born at Beauvais, in the department of Oise. He studied with Jean - Baptiste Biot at the Collège de France. He became professor of mineralogy at the École Normale Supérieure and afterwards at the Muséum National d'Histoire Naturelle in Paris. He studied the geysers of Iceland, and wrote also on the classification of some of the eruptive rocks. His main work consisted in the systematic examination of the crystals of numerous minerals, in researches on their optical properties and on the subject of light polarization. He demonstrated the circular polarization of cinnabar. He wrote especially on the means of determining the different feldspars, and is credited with the discovery of microcline (a triclinic potash - feldspar). He named the minerals montebrasite (1871), binnite (a variety of tennantite) and Christianite (in honor of Christian VIII of Denmark). In 1854, Alexis Damour dedicated the mineral descloizite in honor of Des Cloizeaux. Des Cloizeaux was elected as a member of the French Academy of Sciences in 1869, and was its President in 1889. He was awarded the Wollaston Medal by the Geological Society of London in 1886. His best - known books are Leçons de cristallographie (1861) and Manuel de minéralogie (2 vols. , Paris, 1862, 1874 and 1893).
|
educated at
| null | 42,276 |
[
"Alfred Louis Olivier Legrand Des Cloizeaux",
"employer",
"Muséum National d'Histoire Naturelle"
] |
Find the relation between <e1>Alfred Louis Olivier Legrand Des Cloizeaux<\e1> and <e2>Muséum National d'Histoire Naturelle<\e2>.
Alfred Louis Olivier Legrand Des Cloizeaux (17 October 18176 May 1897) was a French mineralogist. Des Cloizeaux was born at Beauvais, in the department of Oise. He studied with Jean - Baptiste Biot at the Collège de France. He became professor of mineralogy at the École Normale Supérieure and afterwards at the Muséum National d'Histoire Naturelle in Paris. He studied the geysers of Iceland, and wrote also on the classification of some of the eruptive rocks. His main work consisted in the systematic examination of the crystals of numerous minerals, in researches on their optical properties and on the subject of light polarization. He demonstrated the circular polarization of cinnabar. He wrote especially on the means of determining the different feldspars, and is credited with the discovery of microcline (a triclinic potash - feldspar). He named the minerals montebrasite (1871), binnite (a variety of tennantite) and Christianite (in honor of Christian VIII of Denmark). In 1854, Alexis Damour dedicated the mineral descloizite in honor of Des Cloizeaux. Des Cloizeaux was elected as a member of the French Academy of Sciences in 1869, and was its President in 1889. He was awarded the Wollaston Medal by the Geological Society of London in 1886. His best - known books are Leçons de cristallographie (1861) and Manuel de minéralogie (2 vols. , Paris, 1862, 1874 and 1893).
|
employer
| null | 42,277 |
[
"French Academy of Sciences",
"located in the administrative territorial entity",
"Paris"
] |
Find the relation between <e1>French Academy of Sciences<\e1> and <e2>Paris<\e2>.
Alfred Louis Olivier Legrand Des Cloizeaux (17 October 18176 May 1897) was a French mineralogist. Des Cloizeaux was born at Beauvais, in the department of Oise. He studied with Jean - Baptiste Biot at the Collège de France. He became professor of mineralogy at the École Normale Supérieure and afterwards at the Muséum National d'Histoire Naturelle in Paris. He studied the geysers of Iceland, and wrote also on the classification of some of the eruptive rocks. His main work consisted in the systematic examination of the crystals of numerous minerals, in researches on their optical properties and on the subject of light polarization. He demonstrated the circular polarization of cinnabar. He wrote especially on the means of determining the different feldspars, and is credited with the discovery of microcline (a triclinic potash - feldspar). He named the minerals montebrasite (1871), binnite (a variety of tennantite) and Christianite (in honor of Christian VIII of Denmark). In 1854, Alexis Damour dedicated the mineral descloizite in honor of Des Cloizeaux. Des Cloizeaux was elected as a member of the French Academy of Sciences in 1869, and was its President in 1889. He was awarded the Wollaston Medal by the Geological Society of London in 1886. His best - known books are Leçons de cristallographie (1861) and Manuel de minéralogie (2 vols. , Paris, 1862, 1874 and 1893).
|
located in the administrative territorial entity
| null | 42,278 |
[
"Alfred Louis Olivier Legrand Des Cloizeaux",
"employer",
"École Normale Supérieure"
] |
Find the relation between <e1>Alfred Louis Olivier Legrand Des Cloizeaux<\e1> and <e2>École Normale Supérieure<\e2>.
Alfred Louis Olivier Legrand Des Cloizeaux (17 October 18176 May 1897) was a French mineralogist. Des Cloizeaux was born at Beauvais, in the department of Oise. He studied with Jean - Baptiste Biot at the Collège de France. He became professor of mineralogy at the École Normale Supérieure and afterwards at the Muséum National d'Histoire Naturelle in Paris. He studied the geysers of Iceland, and wrote also on the classification of some of the eruptive rocks. His main work consisted in the systematic examination of the crystals of numerous minerals, in researches on their optical properties and on the subject of light polarization. He demonstrated the circular polarization of cinnabar. He wrote especially on the means of determining the different feldspars, and is credited with the discovery of microcline (a triclinic potash - feldspar). He named the minerals montebrasite (1871), binnite (a variety of tennantite) and Christianite (in honor of Christian VIII of Denmark). In 1854, Alexis Damour dedicated the mineral descloizite in honor of Des Cloizeaux. Des Cloizeaux was elected as a member of the French Academy of Sciences in 1869, and was its President in 1889. He was awarded the Wollaston Medal by the Geological Society of London in 1886. His best - known books are Leçons de cristallographie (1861) and Manuel de minéralogie (2 vols. , Paris, 1862, 1874 and 1893).
|
employer
| null | 42,280 |
[
"Christian VIII",
"applies to jurisdiction",
"Denmark"
] |
Find the relation between <e1>Christian VIII<\e1> and <e2>Denmark<\e2>.
Alfred Louis Olivier Legrand Des Cloizeaux (17 October 18176 May 1897) was a French mineralogist. Des Cloizeaux was born at Beauvais, in the department of Oise. He studied with Jean - Baptiste Biot at the Collège de France. He became professor of mineralogy at the École Normale Supérieure and afterwards at the Muséum National d'Histoire Naturelle in Paris. He studied the geysers of Iceland, and wrote also on the classification of some of the eruptive rocks. His main work consisted in the systematic examination of the crystals of numerous minerals, in researches on their optical properties and on the subject of light polarization. He demonstrated the circular polarization of cinnabar. He wrote especially on the means of determining the different feldspars, and is credited with the discovery of microcline (a triclinic potash - feldspar). He named the minerals montebrasite (1871), binnite (a variety of tennantite) and Christianite (in honor of Christian VIII of Denmark). In 1854, Alexis Damour dedicated the mineral descloizite in honor of Des Cloizeaux. Des Cloizeaux was elected as a member of the French Academy of Sciences in 1869, and was its President in 1889. He was awarded the Wollaston Medal by the Geological Society of London in 1886. His best - known books are Leçons de cristallographie (1861) and Manuel de minéralogie (2 vols. , Paris, 1862, 1874 and 1893).
|
applies to jurisdiction
| null | 42,281 |
[
"Paris",
"located in the administrative territorial entity",
"French"
] |
Find the relation between <e1>Paris<\e1> and <e2>French<\e2>.
Alfred Louis Olivier Legrand Des Cloizeaux (17 October 18176 May 1897) was a French mineralogist. Des Cloizeaux was born at Beauvais, in the department of Oise. He studied with Jean - Baptiste Biot at the Collège de France. He became professor of mineralogy at the École Normale Supérieure and afterwards at the Muséum National d'Histoire Naturelle in Paris. He studied the geysers of Iceland, and wrote also on the classification of some of the eruptive rocks. His main work consisted in the systematic examination of the crystals of numerous minerals, in researches on their optical properties and on the subject of light polarization. He demonstrated the circular polarization of cinnabar. He wrote especially on the means of determining the different feldspars, and is credited with the discovery of microcline (a triclinic potash - feldspar). He named the minerals montebrasite (1871), binnite (a variety of tennantite) and Christianite (in honor of Christian VIII of Denmark). In 1854, Alexis Damour dedicated the mineral descloizite in honor of Des Cloizeaux. Des Cloizeaux was elected as a member of the French Academy of Sciences in 1869, and was its President in 1889. He was awarded the Wollaston Medal by the Geological Society of London in 1886. His best - known books are Leçons de cristallographie (1861) and Manuel de minéralogie (2 vols. , Paris, 1862, 1874 and 1893).
|
located in the administrative territorial entity
| null | 42,282 |
[
"French Academy of Sciences",
"located in the administrative territorial entity",
"French"
] |
Find the relation between <e1>French Academy of Sciences<\e1> and <e2>French<\e2>.
Alfred Louis Olivier Legrand Des Cloizeaux (17 October 18176 May 1897) was a French mineralogist. Des Cloizeaux was born at Beauvais, in the department of Oise. He studied with Jean - Baptiste Biot at the Collège de France. He became professor of mineralogy at the École Normale Supérieure and afterwards at the Muséum National d'Histoire Naturelle in Paris. He studied the geysers of Iceland, and wrote also on the classification of some of the eruptive rocks. His main work consisted in the systematic examination of the crystals of numerous minerals, in researches on their optical properties and on the subject of light polarization. He demonstrated the circular polarization of cinnabar. He wrote especially on the means of determining the different feldspars, and is credited with the discovery of microcline (a triclinic potash - feldspar). He named the minerals montebrasite (1871), binnite (a variety of tennantite) and Christianite (in honor of Christian VIII of Denmark). In 1854, Alexis Damour dedicated the mineral descloizite in honor of Des Cloizeaux. Des Cloizeaux was elected as a member of the French Academy of Sciences in 1869, and was its President in 1889. He was awarded the Wollaston Medal by the Geological Society of London in 1886. His best - known books are Leçons de cristallographie (1861) and Manuel de minéralogie (2 vols. , Paris, 1862, 1874 and 1893).
|
located in the administrative territorial entity
| null | 42,283 |
[
"Collège de France",
"located in the administrative territorial entity",
"French"
] |
Find the relation between <e1>Collège de France<\e1> and <e2>French<\e2>.
Alfred Louis Olivier Legrand Des Cloizeaux (17 October 18176 May 1897) was a French mineralogist. Des Cloizeaux was born at Beauvais, in the department of Oise. He studied with Jean - Baptiste Biot at the Collège de France. He became professor of mineralogy at the École Normale Supérieure and afterwards at the Muséum National d'Histoire Naturelle in Paris. He studied the geysers of Iceland, and wrote also on the classification of some of the eruptive rocks. His main work consisted in the systematic examination of the crystals of numerous minerals, in researches on their optical properties and on the subject of light polarization. He demonstrated the circular polarization of cinnabar. He wrote especially on the means of determining the different feldspars, and is credited with the discovery of microcline (a triclinic potash - feldspar). He named the minerals montebrasite (1871), binnite (a variety of tennantite) and Christianite (in honor of Christian VIII of Denmark). In 1854, Alexis Damour dedicated the mineral descloizite in honor of Des Cloizeaux. Des Cloizeaux was elected as a member of the French Academy of Sciences in 1869, and was its President in 1889. He was awarded the Wollaston Medal by the Geological Society of London in 1886. His best - known books are Leçons de cristallographie (1861) and Manuel de minéralogie (2 vols. , Paris, 1862, 1874 and 1893).
|
located in the administrative territorial entity
| null | 42,284 |
[
"École Normale Supérieure",
"located in the administrative territorial entity",
"French"
] |
Find the relation between <e1>École Normale Supérieure<\e1> and <e2>French<\e2>.
Alfred Louis Olivier Legrand Des Cloizeaux (17 October 18176 May 1897) was a French mineralogist. Des Cloizeaux was born at Beauvais, in the department of Oise. He studied with Jean - Baptiste Biot at the Collège de France. He became professor of mineralogy at the École Normale Supérieure and afterwards at the Muséum National d'Histoire Naturelle in Paris. He studied the geysers of Iceland, and wrote also on the classification of some of the eruptive rocks. His main work consisted in the systematic examination of the crystals of numerous minerals, in researches on their optical properties and on the subject of light polarization. He demonstrated the circular polarization of cinnabar. He wrote especially on the means of determining the different feldspars, and is credited with the discovery of microcline (a triclinic potash - feldspar). He named the minerals montebrasite (1871), binnite (a variety of tennantite) and Christianite (in honor of Christian VIII of Denmark). In 1854, Alexis Damour dedicated the mineral descloizite in honor of Des Cloizeaux. Des Cloizeaux was elected as a member of the French Academy of Sciences in 1869, and was its President in 1889. He was awarded the Wollaston Medal by the Geological Society of London in 1886. His best - known books are Leçons de cristallographie (1861) and Manuel de minéralogie (2 vols. , Paris, 1862, 1874 and 1893).
|
located in the administrative territorial entity
| null | 42,285 |
[
"Muséum National d'Histoire Naturelle",
"located in the administrative territorial entity",
"French"
] |
Find the relation between <e1>Muséum National d'Histoire Naturelle<\e1> and <e2>French<\e2>.
Alfred Louis Olivier Legrand Des Cloizeaux (17 October 18176 May 1897) was a French mineralogist. Des Cloizeaux was born at Beauvais, in the department of Oise. He studied with Jean - Baptiste Biot at the Collège de France. He became professor of mineralogy at the École Normale Supérieure and afterwards at the Muséum National d'Histoire Naturelle in Paris. He studied the geysers of Iceland, and wrote also on the classification of some of the eruptive rocks. His main work consisted in the systematic examination of the crystals of numerous minerals, in researches on their optical properties and on the subject of light polarization. He demonstrated the circular polarization of cinnabar. He wrote especially on the means of determining the different feldspars, and is credited with the discovery of microcline (a triclinic potash - feldspar). He named the minerals montebrasite (1871), binnite (a variety of tennantite) and Christianite (in honor of Christian VIII of Denmark). In 1854, Alexis Damour dedicated the mineral descloizite in honor of Des Cloizeaux. Des Cloizeaux was elected as a member of the French Academy of Sciences in 1869, and was its President in 1889. He was awarded the Wollaston Medal by the Geological Society of London in 1886. His best - known books are Leçons de cristallographie (1861) and Manuel de minéralogie (2 vols. , Paris, 1862, 1874 and 1893).
|
located in the administrative territorial entity
| null | 42,286 |
[
"India",
"part of",
"South Asia"
] |
Find the relation between <e1>India<\e1> and <e2>South Asia<\e2>.
Lashkar (Persian : لشکر) may refer to :Lascar, a type of sailor or militiaman employed by the British in South Asia (modern Bangladesh, India, and Pakistan)Lashkar (film), a 1989 Bollywood filmLaskhar (novel), a 2008 military action thriller by Mukul Deva, published by HarperCollins. This is the first of a 4-book bestseller series. The motion picture rights of this novel were purchased by Planman Motion Pictures. Lashkargah, a city in southern Afghanistan, capital of Helmand ProvinceLashkar, Iran, a village in Kerman Province, IranLashkar, Gwalior, an area of the city of Gwalior, formerly a separate townLashkar - e - Jhangvi, a militant organization in PakistanLashkar - e - Omar, a Pakistani Islamic fundamentalist organizationLashkar - e - Qahhar, an Islamist group that claimed responsibility for the 11 July 2006 Mumbai Train BombingsLashkar - e - Taiba, an Islamist terrorist organization in South Asia
|
part of
| null | 42,445 |
[
"Lashkargah",
"country",
"Afghanistan"
] |
Find the relation between <e1>Lashkargah<\e1> and <e2>Afghanistan<\e2>.
Lashkar (Persian : لشکر) may refer to :Lascar, a type of sailor or militiaman employed by the British in South Asia (modern Bangladesh, India, and Pakistan)Lashkar (film), a 1989 Bollywood filmLaskhar (novel), a 2008 military action thriller by Mukul Deva, published by HarperCollins. This is the first of a 4-book bestseller series. The motion picture rights of this novel were purchased by Planman Motion Pictures. Lashkargah, a city in southern Afghanistan, capital of Helmand ProvinceLashkar, Iran, a village in Kerman Province, IranLashkar, Gwalior, an area of the city of Gwalior, formerly a separate townLashkar - e - Jhangvi, a militant organization in PakistanLashkar - e - Omar, a Pakistani Islamic fundamentalist organizationLashkar - e - Qahhar, an Islamist group that claimed responsibility for the 11 July 2006 Mumbai Train BombingsLashkar - e - Taiba, an Islamist terrorist organization in South Asia
|
country
| null | 42,446 |
[
"Lashkargah",
"capital of",
"Helmand Province"
] |
Find the relation between <e1>Lashkargah<\e1> and <e2>Helmand Province<\e2>.
Lashkar (Persian : لشکر) may refer to :Lascar, a type of sailor or militiaman employed by the British in South Asia (modern Bangladesh, India, and Pakistan)Lashkar (film), a 1989 Bollywood filmLaskhar (novel), a 2008 military action thriller by Mukul Deva, published by HarperCollins. This is the first of a 4-book bestseller series. The motion picture rights of this novel were purchased by Planman Motion Pictures. Lashkargah, a city in southern Afghanistan, capital of Helmand ProvinceLashkar, Iran, a village in Kerman Province, IranLashkar, Gwalior, an area of the city of Gwalior, formerly a separate townLashkar - e - Jhangvi, a militant organization in PakistanLashkar - e - Omar, a Pakistani Islamic fundamentalist organizationLashkar - e - Qahhar, an Islamist group that claimed responsibility for the 11 July 2006 Mumbai Train BombingsLashkar - e - Taiba, an Islamist terrorist organization in South Asia
|
capital of
| null | 42,447 |
[
"Helmand Province",
"capital",
"Lashkargah"
] |
Find the relation between <e1>Helmand Province<\e1> and <e2>Lashkargah<\e2>.
Lashkar (Persian : لشکر) may refer to :Lascar, a type of sailor or militiaman employed by the British in South Asia (modern Bangladesh, India, and Pakistan)Lashkar (film), a 1989 Bollywood filmLaskhar (novel), a 2008 military action thriller by Mukul Deva, published by HarperCollins. This is the first of a 4-book bestseller series. The motion picture rights of this novel were purchased by Planman Motion Pictures. Lashkargah, a city in southern Afghanistan, capital of Helmand ProvinceLashkar, Iran, a village in Kerman Province, IranLashkar, Gwalior, an area of the city of Gwalior, formerly a separate townLashkar - e - Jhangvi, a militant organization in PakistanLashkar - e - Omar, a Pakistani Islamic fundamentalist organizationLashkar - e - Qahhar, an Islamist group that claimed responsibility for the 11 July 2006 Mumbai Train BombingsLashkar - e - Taiba, an Islamist terrorist organization in South Asia
|
capital
| null | 42,449 |
[
"Helmand Province",
"located in the administrative territorial entity",
"Afghanistan"
] |
Find the relation between <e1>Helmand Province<\e1> and <e2>Afghanistan<\e2>.
Lashkar (Persian : لشکر) may refer to :Lascar, a type of sailor or militiaman employed by the British in South Asia (modern Bangladesh, India, and Pakistan)Lashkar (film), a 1989 Bollywood filmLaskhar (novel), a 2008 military action thriller by Mukul Deva, published by HarperCollins. This is the first of a 4-book bestseller series. The motion picture rights of this novel were purchased by Planman Motion Pictures. Lashkargah, a city in southern Afghanistan, capital of Helmand ProvinceLashkar, Iran, a village in Kerman Province, IranLashkar, Gwalior, an area of the city of Gwalior, formerly a separate townLashkar - e - Jhangvi, a militant organization in PakistanLashkar - e - Omar, a Pakistani Islamic fundamentalist organizationLashkar - e - Qahhar, an Islamist group that claimed responsibility for the 11 July 2006 Mumbai Train BombingsLashkar - e - Taiba, an Islamist terrorist organization in South Asia
|
located in the administrative territorial entity
| null | 42,450 |
[
"Helmand Province",
"country",
"Afghanistan"
] |
Find the relation between <e1>Helmand Province<\e1> and <e2>Afghanistan<\e2>.
Lashkar (Persian : لشکر) may refer to :Lascar, a type of sailor or militiaman employed by the British in South Asia (modern Bangladesh, India, and Pakistan)Lashkar (film), a 1989 Bollywood filmLaskhar (novel), a 2008 military action thriller by Mukul Deva, published by HarperCollins. This is the first of a 4-book bestseller series. The motion picture rights of this novel were purchased by Planman Motion Pictures. Lashkargah, a city in southern Afghanistan, capital of Helmand ProvinceLashkar, Iran, a village in Kerman Province, IranLashkar, Gwalior, an area of the city of Gwalior, formerly a separate townLashkar - e - Jhangvi, a militant organization in PakistanLashkar - e - Omar, a Pakistani Islamic fundamentalist organizationLashkar - e - Qahhar, an Islamist group that claimed responsibility for the 11 July 2006 Mumbai Train BombingsLashkar - e - Taiba, an Islamist terrorist organization in South Asia
|
country
| null | 42,451 |
[
"Kerman Province",
"located in the administrative territorial entity",
"Iran"
] |
Find the relation between <e1>Kerman Province<\e1> and <e2>Iran<\e2>.
Lashkar (Persian : لشکر) may refer to :Lascar, a type of sailor or militiaman employed by the British in South Asia (modern Bangladesh, India, and Pakistan)Lashkar (film), a 1989 Bollywood filmLaskhar (novel), a 2008 military action thriller by Mukul Deva, published by HarperCollins. This is the first of a 4-book bestseller series. The motion picture rights of this novel were purchased by Planman Motion Pictures. Lashkargah, a city in southern Afghanistan, capital of Helmand ProvinceLashkar, Iran, a village in Kerman Province, IranLashkar, Gwalior, an area of the city of Gwalior, formerly a separate townLashkar - e - Jhangvi, a militant organization in PakistanLashkar - e - Omar, a Pakistani Islamic fundamentalist organizationLashkar - e - Qahhar, an Islamist group that claimed responsibility for the 11 July 2006 Mumbai Train BombingsLashkar - e - Taiba, an Islamist terrorist organization in South Asia
|
located in the administrative territorial entity
| null | 42,453 |
[
"Kerman Province",
"country",
"Iran"
] |
Find the relation between <e1>Kerman Province<\e1> and <e2>Iran<\e2>.
Lashkar (Persian : لشکر) may refer to :Lascar, a type of sailor or militiaman employed by the British in South Asia (modern Bangladesh, India, and Pakistan)Lashkar (film), a 1989 Bollywood filmLaskhar (novel), a 2008 military action thriller by Mukul Deva, published by HarperCollins. This is the first of a 4-book bestseller series. The motion picture rights of this novel were purchased by Planman Motion Pictures. Lashkargah, a city in southern Afghanistan, capital of Helmand ProvinceLashkar, Iran, a village in Kerman Province, IranLashkar, Gwalior, an area of the city of Gwalior, formerly a separate townLashkar - e - Jhangvi, a militant organization in PakistanLashkar - e - Omar, a Pakistani Islamic fundamentalist organizationLashkar - e - Qahhar, an Islamist group that claimed responsibility for the 11 July 2006 Mumbai Train BombingsLashkar - e - Taiba, an Islamist terrorist organization in South Asia
|
country
| null | 42,454 |
[
"Laskhar",
"publisher",
"HarperCollins"
] |
Find the relation between <e1>Laskhar<\e1> and <e2>HarperCollins<\e2>.
Lashkar (Persian : لشکر) may refer to :Lascar, a type of sailor or militiaman employed by the British in South Asia (modern Bangladesh, India, and Pakistan)Lashkar (film), a 1989 Bollywood filmLaskhar (novel), a 2008 military action thriller by Mukul Deva, published by HarperCollins. This is the first of a 4-book bestseller series. The motion picture rights of this novel were purchased by Planman Motion Pictures. Lashkargah, a city in southern Afghanistan, capital of Helmand ProvinceLashkar, Iran, a village in Kerman Province, IranLashkar, Gwalior, an area of the city of Gwalior, formerly a separate townLashkar - e - Jhangvi, a militant organization in PakistanLashkar - e - Omar, a Pakistani Islamic fundamentalist organizationLashkar - e - Qahhar, an Islamist group that claimed responsibility for the 11 July 2006 Mumbai Train BombingsLashkar - e - Taiba, an Islamist terrorist organization in South Asia
|
publisher
| null | 42,457 |
[
"Lashkargah",
"located in the administrative territorial entity",
"Helmand Province"
] |
Find the relation between <e1>Lashkargah<\e1> and <e2>Helmand Province<\e2>.
Lashkar (Persian : لشکر) may refer to :Lascar, a type of sailor or militiaman employed by the British in South Asia (modern Bangladesh, India, and Pakistan)Lashkar (film), a 1989 Bollywood filmLaskhar (novel), a 2008 military action thriller by Mukul Deva, published by HarperCollins. This is the first of a 4-book bestseller series. The motion picture rights of this novel were purchased by Planman Motion Pictures. Lashkargah, a city in southern Afghanistan, capital of Helmand ProvinceLashkar, Iran, a village in Kerman Province, IranLashkar, Gwalior, an area of the city of Gwalior, formerly a separate townLashkar - e - Jhangvi, a militant organization in PakistanLashkar - e - Omar, a Pakistani Islamic fundamentalist organizationLashkar - e - Qahhar, an Islamist group that claimed responsibility for the 11 July 2006 Mumbai Train BombingsLashkar - e - Taiba, an Islamist terrorist organization in South Asia
|
located in the administrative territorial entity
| null | 42,459 |
[
"Lashkar-e-Jhangvi",
"country",
"Pakistan"
] |
Find the relation between <e1>Lashkar-e-Jhangvi<\e1> and <e2>Pakistan<\e2>.
Lashkar (Persian : لشکر) may refer to :Lascar, a type of sailor or militiaman employed by the British in South Asia (modern Bangladesh, India, and Pakistan)Lashkar (film), a 1989 Bollywood filmLaskhar (novel), a 2008 military action thriller by Mukul Deva, published by HarperCollins. This is the first of a 4-book bestseller series. The motion picture rights of this novel were purchased by Planman Motion Pictures. Lashkargah, a city in southern Afghanistan, capital of Helmand ProvinceLashkar, Iran, a village in Kerman Province, IranLashkar, Gwalior, an area of the city of Gwalior, formerly a separate townLashkar - e - Jhangvi, a militant organization in PakistanLashkar - e - Omar, a Pakistani Islamic fundamentalist organizationLashkar - e - Qahhar, an Islamist group that claimed responsibility for the 11 July 2006 Mumbai Train BombingsLashkar - e - Taiba, an Islamist terrorist organization in South Asia
|
country
| null | 42,460 |
[
"Laskhar",
"author",
"Mukul Deva"
] |
Find the relation between <e1>Laskhar<\e1> and <e2>Mukul Deva<\e2>.
Lashkar (Persian : لشکر) may refer to :Lascar, a type of sailor or militiaman employed by the British in South Asia (modern Bangladesh, India, and Pakistan)Lashkar (film), a 1989 Bollywood filmLaskhar (novel), a 2008 military action thriller by Mukul Deva, published by HarperCollins. This is the first of a 4-book bestseller series. The motion picture rights of this novel were purchased by Planman Motion Pictures. Lashkargah, a city in southern Afghanistan, capital of Helmand ProvinceLashkar, Iran, a village in Kerman Province, IranLashkar, Gwalior, an area of the city of Gwalior, formerly a separate townLashkar - e - Jhangvi, a militant organization in PakistanLashkar - e - Omar, a Pakistani Islamic fundamentalist organizationLashkar - e - Qahhar, an Islamist group that claimed responsibility for the 11 July 2006 Mumbai Train BombingsLashkar - e - Taiba, an Islamist terrorist organization in South Asia
|
author
| null | 42,461 |
[
"Lashkar-e-Omar",
"country",
"Pakistan"
] |
Find the relation between <e1>Lashkar-e-Omar<\e1> and <e2>Pakistan<\e2>.
Lashkar (Persian : لشکر) may refer to :Lascar, a type of sailor or militiaman employed by the British in South Asia (modern Bangladesh, India, and Pakistan)Lashkar (film), a 1989 Bollywood filmLaskhar (novel), a 2008 military action thriller by Mukul Deva, published by HarperCollins. This is the first of a 4-book bestseller series. The motion picture rights of this novel were purchased by Planman Motion Pictures. Lashkargah, a city in southern Afghanistan, capital of Helmand ProvinceLashkar, Iran, a village in Kerman Province, IranLashkar, Gwalior, an area of the city of Gwalior, formerly a separate townLashkar - e - Jhangvi, a militant organization in PakistanLashkar - e - Omar, a Pakistani Islamic fundamentalist organizationLashkar - e - Qahhar, an Islamist group that claimed responsibility for the 11 July 2006 Mumbai Train BombingsLashkar - e - Taiba, an Islamist terrorist organization in South Asia
|
country
| null | 42,462 |
[
"South Asia",
"has part(s)",
"India"
] |
Find the relation between <e1>South Asia<\e1> and <e2>India<\e2>.
Lashkar (Persian : لشکر) may refer to :Lascar, a type of sailor or militiaman employed by the British in South Asia (modern Bangladesh, India, and Pakistan)Lashkar (film), a 1989 Bollywood filmLaskhar (novel), a 2008 military action thriller by Mukul Deva, published by HarperCollins. This is the first of a 4-book bestseller series. The motion picture rights of this novel were purchased by Planman Motion Pictures. Lashkargah, a city in southern Afghanistan, capital of Helmand ProvinceLashkar, Iran, a village in Kerman Province, IranLashkar, Gwalior, an area of the city of Gwalior, formerly a separate townLashkar - e - Jhangvi, a militant organization in PakistanLashkar - e - Omar, a Pakistani Islamic fundamentalist organizationLashkar - e - Qahhar, an Islamist group that claimed responsibility for the 11 July 2006 Mumbai Train BombingsLashkar - e - Taiba, an Islamist terrorist organization in South Asia
|
has part(s)
| null | 42,463 |
[
"Mukul Deva",
"notable work",
"Laskhar"
] |
Find the relation between <e1>Mukul Deva<\e1> and <e2>Laskhar<\e2>.
Lashkar (Persian : لشکر) may refer to :Lascar, a type of sailor or militiaman employed by the British in South Asia (modern Bangladesh, India, and Pakistan)Lashkar (film), a 1989 Bollywood filmLaskhar (novel), a 2008 military action thriller by Mukul Deva, published by HarperCollins. This is the first of a 4-book bestseller series. The motion picture rights of this novel were purchased by Planman Motion Pictures. Lashkargah, a city in southern Afghanistan, capital of Helmand ProvinceLashkar, Iran, a village in Kerman Province, IranLashkar, Gwalior, an area of the city of Gwalior, formerly a separate townLashkar - e - Jhangvi, a militant organization in PakistanLashkar - e - Omar, a Pakistani Islamic fundamentalist organizationLashkar - e - Qahhar, an Islamist group that claimed responsibility for the 11 July 2006 Mumbai Train BombingsLashkar - e - Taiba, an Islamist terrorist organization in South Asia
|
notable work
| null | 42,464 |
[
"Lashkargah",
"located in the administrative territorial entity",
"Afghanistan"
] |
Find the relation between <e1>Lashkargah<\e1> and <e2>Afghanistan<\e2>.
Lashkar (Persian : لشکر) may refer to :Lascar, a type of sailor or militiaman employed by the British in South Asia (modern Bangladesh, India, and Pakistan)Lashkar (film), a 1989 Bollywood filmLaskhar (novel), a 2008 military action thriller by Mukul Deva, published by HarperCollins. This is the first of a 4-book bestseller series. The motion picture rights of this novel were purchased by Planman Motion Pictures. Lashkargah, a city in southern Afghanistan, capital of Helmand ProvinceLashkar, Iran, a village in Kerman Province, IranLashkar, Gwalior, an area of the city of Gwalior, formerly a separate townLashkar - e - Jhangvi, a militant organization in PakistanLashkar - e - Omar, a Pakistani Islamic fundamentalist organizationLashkar - e - Qahhar, an Islamist group that claimed responsibility for the 11 July 2006 Mumbai Train BombingsLashkar - e - Taiba, an Islamist terrorist organization in South Asia
|
located in the administrative territorial entity
| null | 42,465 |
[
"Lashkar-e-Jhangvi",
"located in the administrative territorial entity",
"Pakistan"
] |
Find the relation between <e1>Lashkar-e-Jhangvi<\e1> and <e2>Pakistan<\e2>.
Lashkar (Persian : لشکر) may refer to :Lascar, a type of sailor or militiaman employed by the British in South Asia (modern Bangladesh, India, and Pakistan)Lashkar (film), a 1989 Bollywood filmLaskhar (novel), a 2008 military action thriller by Mukul Deva, published by HarperCollins. This is the first of a 4-book bestseller series. The motion picture rights of this novel were purchased by Planman Motion Pictures. Lashkargah, a city in southern Afghanistan, capital of Helmand ProvinceLashkar, Iran, a village in Kerman Province, IranLashkar, Gwalior, an area of the city of Gwalior, formerly a separate townLashkar - e - Jhangvi, a militant organization in PakistanLashkar - e - Omar, a Pakistani Islamic fundamentalist organizationLashkar - e - Qahhar, an Islamist group that claimed responsibility for the 11 July 2006 Mumbai Train BombingsLashkar - e - Taiba, an Islamist terrorist organization in South Asia
|
located in the administrative territorial entity
| null | 42,466 |
[
"Lashkar-e-Omar",
"located in the administrative territorial entity",
"Pakistan"
] |
Find the relation between <e1>Lashkar-e-Omar<\e1> and <e2>Pakistan<\e2>.
Lashkar (Persian : لشکر) may refer to :Lascar, a type of sailor or militiaman employed by the British in South Asia (modern Bangladesh, India, and Pakistan)Lashkar (film), a 1989 Bollywood filmLaskhar (novel), a 2008 military action thriller by Mukul Deva, published by HarperCollins. This is the first of a 4-book bestseller series. The motion picture rights of this novel were purchased by Planman Motion Pictures. Lashkargah, a city in southern Afghanistan, capital of Helmand ProvinceLashkar, Iran, a village in Kerman Province, IranLashkar, Gwalior, an area of the city of Gwalior, formerly a separate townLashkar - e - Jhangvi, a militant organization in PakistanLashkar - e - Omar, a Pakistani Islamic fundamentalist organizationLashkar - e - Qahhar, an Islamist group that claimed responsibility for the 11 July 2006 Mumbai Train BombingsLashkar - e - Taiba, an Islamist terrorist organization in South Asia
|
located in the administrative territorial entity
| null | 42,467 |
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