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Aruba | Spanish ranch | Spanish ranch
thumb|Goats in Arikok National Park
The conquistadors brought European cattle to Aruba. Over time, they also introduced goats, sheep, dogs, donkeys, cows, pigs, and possibly even cats. It is believed that rabbits, brought by the Dutch, later became wild on the island. Aruba essentially became a Spanish ranch, with cattle roaming freely in search of food. Despite more trees in the past, the overall vegetation was similar to today. The horses introduced were lighter than Dutch ones, and their hooves became so hard from roaming freely that they did not need horseshoes. To avoid stallions injuring each other during mating battles, horseshoes were impractical. After three weeks of service, particularly in the dry season, the horses were released to recover. Occasionally, a small group of Spaniards would disembark on the island, but typically Aruba was left to fend for itself. According to Dutch geographer Joannes De Laet, by 1630 there were few Indians and some Spaniards on Aruba. |
Aruba | Early Dutch period | Early Dutch period |
Aruba | Dutch conquest: salt | Dutch conquest: salt
The Dutch were compelled to venture into forbidden waters of the Caribbean, known as Spain's mare clausum, because of their need for salt, in open defiance of Phillip II. Since the mid-15th century, the prosperous Dutch herring industry had been steadily expanding. The towns of Hoorn, Enkhuizen, and Medemblik were particularly active in the salt trade, thanks to their thriving fishing industries. Herring was a crucial commodity for Dutch commerce, requiring salt for preservation. Salt also played a vital role in the butter and cheese industry, as well as in preserving food during long voyages. The curing or pickling process for herring was well established during the Middle Ages. After catching the herring, the packers would remove the internal organs, mix them with salt to create a brine, and pack them in barrels along with additional salt. While Zeeland was not heavily involved in fishing, they were renowned for their salt whitening process, which was highly sought after throughout Europe.
Salt importation began in the 15th century when the Dutch discovered high-quality salt in Setúbal the Iberian coast. This sea salt was good for preserving herring because of its magnesium sulfate and magnesium chloride content. However, the Eighty Years' War prompted Phillip II to halt this trade. With the salt supply cut off, the Dutch were forced to seek new trade routes. Their quest for salt led them to the West Indies. Seeking alternative sources, they turned their attention to Punta de Araya in Tierra Firme by the 17th century. The salt reserves in Punta de Araya were abundant and of high quality, surpassing that of the Iberian peninsula. Rather than being a rock salt deposit, it was a gem salt derived from the clay of the surrounding hills. However, following the Truce of twelve years, the Dutch discovered that the Spaniards had fortified the saltpans, forcing them to give up their stake in Araya salt.
After hostilities resumed, the Dutch established the West India Company (WIC) with the main objective of engaging in strategic military actions and privateering organization against Spain. This was the or reason for the existence of the WIC. Their secondary objective was focused on commerce and colonization, a choice that ultimately led to the downfall of the WIC in 1674. The WIC also gathered information on Spanish treasure fleets. In 1623, the first official fleet of the new WIC, a small squadron of only three ships commanded by Pieter Schouten, set sail for the Caribbean to engage in looting and plundering in the Lesser Antilles and the Yucátan peninsula. It was during this voyage that the Dutch first encountered Aruba.
Around 1628 or 1629, the Dutch started obtaining salt regularly on Tortuga. Governor Francisco Núñez Melián of Venezuela destroyed the saltpans and took some Dutch prisoners, forced them to cut Brazilwood in Curaçao. One of these Dutchmen, Jan Janszoon Otzen, carefully assessed the island's excellent harbor and profitable saltpans, which he later communicated to the WIC. Recognizing their struggle for salt, the Dutch realized the need to establish a base in these waters to secure Curaçao. WIC agent Johannes van Walbeeck was appointed as the expedition's commander and future Governor of Curaçao, Bonaire, and Aruba. Curaçao was captured and acquired by the WIC in June 1634, primarily by their desire to obtain salt. In Van Walbeeck's report of 1634, Aruba is mentioned only in relation to Curaçao, where he refers to Bonaire and Aruba collectively as the "islands of Curaçao".
By 1816, Aruba possessed seven salt pans, all of which yielded salt of subpar quality. The salt production was just sufficient to meet the local demand. Aruban laborers, often assisted by donkeys, were tasked with gathering the salt, which was subsequently distributed among the island's inhabitants. Around 1924, salt extraction at Rancho had limited benefits, primarily being used in the preservation of fish during shipping. Paardenbaai (Horses' Bay) contained salt pans up until 1949 when it was dredged and disappeared beneath the sand. |
Aruba | New Netherland | New Netherland
Between the Peace of Westphalia in 1648 and the Peace of Nijmegen in 1678, there were 30 years of crisis in the Dutch Antilles and the entire Caribbean region. By 1648, Curaçao had lost its importance as a military outpost. Governor Peter Stuyvesant had a plan to strengthen the connections between the islands and New Netherland. He believed that the two colonies could support each other: New Netherland would provide food in exchange for slaves from Curaçao, horses from Aruba, and salt from Bonaire. But Stuyvesant did not anticipate the rivalry between the two colonies, which prevented them from working together effectively. The Dutch in Curaçao preferred to sell their goods to other Caribbean islands where they could get a better price, rather than trading with their fellow countrymen in New Netherland. Additionally, the islands were involved in illegal trade with the Spanish mainland and did not want to switch to legal trade with New Netherland. Stuyvesant needed slaves to strengthen New Amsterdam's defenses, but he mostly received old or sick slaves, called mancarrons, in response to his requests. The better slaves were sold elsewhere to the highest bidder. However, the people in New Netherland were not motivated by unselfish reasons or a strong sense of patriotism. They continued to trade with their French, English, and Swedish neighbors across the border. Only in extreme situations did their shared heritage become more important than making money. For example, when the islands faced famine due to a series of dry seasons, Stuyvesant came to the rescue by sending a ship with food just in time.
The troubled relationship between the Curaçao islands and New Netherland came to a sudden end in 1664. At that time, even though a war between England and the United Provinces had not been officially declared, an English fleet led by Richard Nicolls demanded that New Amsterdam surrender. While the Dutch briefly regained control of the colony in 1673, it was once again used as leverage in 1674 to show the English the dangers of their alliance with France. During the 17th century, the Dutch considered England their main adversary, as evidenced by the three wars they fought against the English. The Second Anglo-Dutch War and the subsequent peace treaty in 1667 marked a pivotal moment in Caribbean colonial possessions. Dutch supremacy waned, and the enforcement of English Navigation Acts left a lasting impact on regional trade. Nevertheless, the Caribbean islands eventually regained stability and prosperity, experiencing fewer changes in colonial holdings for centuries to come. |
Aruba | Slavery | Slavery
In the 16th century, Spaniards engaged in coercive labor practices, deporting Arawak Indians to Hispaniola in 1515. Colonists exerted control over Indians on the "useless islands", mirroring the hardships of these faced by subsequent African slaves, marked by a denial of freedom and forced labor. After 1775 the names of African slaves began appearing in records, with examples such as "Cecilia" and "Apolinar" tied to families like Silvester and Alvarez from Alto Vista near the coast.
The Dutch colonizer recognized red slavery, particularly of Indians captured in wars. In the Guyanas, Indians taken as prisoners in conflicts were traded, even following peace treaties. Though Indians on Aruba were not officially classified as slaves during the West India Company's rule, oral tradition in Aruba mentioned Amerindian slaves in the early 20th century. Father noted their presence in Curaçao as pseudo-slaves. In 1827, Commander Simon Plats found 51 Amerindians treated as pseudo-slaves by Aruban families. Some were brought by shipowners involved in the slave trade. Plats had masters sign a declaration recognizing the freedom of the Amerindians, ensuring proper upbringing, education, and accommodation.
Contrary to common belief, Aruba had a history of slavery, challenging the notion that conditions were considerably better than in other Caribbean regions. Records are limited, with mentions primarily concerning Curaçao in 1750 and 1795. Aruba's circumstances surrounding slavery were comparatively less severe, leading to misconceptions that indigenous people were not enslaved. However, by 1862, 15 percent of Aruba's population were slaves, with 27 percent in Bonaire. A Population Report from 1820 indicates 331 slaves in Aruba—157 indigenous people and 174 of African descent. In 1840, the number increased to 497 slaves, with 269 being indigenous people and 228 of African descent. Approximately, half of Aruba's slaves were of indigenous origin, and the other half were of African descent. Although Dutch law generally prohibited the enslavement of indigenous people, the actual practice varied. |
Aruba | English interregnum and economic development | English interregnum and economic development
thumb|Machinery for the 'cooking' of aloe (1903)
The British Empire took control of the island during the Napoleonic Wars holding it from 1806 to 1816, after which it was returned to Dutch authority in accordance with the Anglo-Dutch Treaty of 1814. Aruba was then integrated into the Colony of Curaçao and Dependencies, along with Bonaire. Throughout the 19th century, the island's economy evolved, centered around gold, phosphate (Aruba Phosphate Company), and the aloe vera industry (Royal Aruba Aloe), However, despite these economic activities, Aruba continued to be a relatively underdeveloped and economically disadvantaged region during this period. |
Aruba | 20th and 21st centuries | 20th and 21st centuries
thumb|Princess Beatrix in Aruba, 1958
The first oil refinery, Lago Oil and Transport Company, in San Nicolas was built in 1924 and a subsidiary of Standard Oil. The refinery on Aruba grew to become one of the largest in the world. In 1927, the Arend Petroleum Company was established to the west of Oranjestad. The refineries processed crude oil from the vast Venezuelan oil fields, bringing greater prosperity to the island.Albert Gastmann, "Suriname and the Dutch in the Caribbean" in Encyclopedia of Latin American History and Culture, vol. 5, p. 189. New York: Charles Scribner's Sons 1996.
During World War II, the Netherlands was occupied by Nazi Germany. In 1940, the oil facilities in Aruba came under the administration of the Dutch government-in-exile in London, causing them to be attacked by the German navy in 1942.Central American and Caribbean Air Forces, Daniel Hagedorn, Air Britain (Historians) Ltd., Tonbridge, 1993, p.135,
In August 1947, Aruba formulated its first staatsreglement (constitution) for Aruba's status aparte as an autonomous state within the Kingdom of the Netherlands, prompted by the efforts of Henny Eman, a noted Aruban politician. By 1954, the Charter of the Kingdom of the Netherlands was established, providing a framework for relations between Aruba and the rest of the kingdom. That created the Netherlands Antilles, which united all of the Dutch colonies in the Caribbean into one administrative structure. Many Arubans were unhappy with the arrangement, however, as the policy was perceived as being dominated by Curaçao.
thumb|right|175px|Betico Croes, a pivotal figure in Aruba's drive for greater autonomy in the 1970s–80s
In 1972, at a conference in Suriname, Aruban politician Betico Croes proposed the creation of a Dutch Commonwealth of four states: Aruba, the Netherlands, Suriname, and the Netherlands Antilles, each to have its own nationality. Backed by his newly created party, the Movimiento Electoral di Pueblo, Croes sought greater autonomy for Aruba, with the long-term goal of independence, adopting the trappings of an independent state in 1976 with the creation of a flag and national anthem. In March 1977, a referendum was held with the support of the United Nations. 82% of the participants voted for complete independence from the Netherlands. Tensions mounted as Croes stepped up the pressure on the Dutch government by organising a general strike in 1977. Croes later met with Dutch Prime Minister Joop den Uyl, with the two sides agreeing to assign the Institute of Social Studies in The Hague to prepare a study for independence, entitled Aruba en Onafhankelijkheid, achtergronden, modaliteiten, en mogelijkheden; een rapport in eerste aanleg (Aruba and independence, backgrounds, modalities, and opportunities; a preliminary report) (1978). |
Aruba | Autonomy | Autonomy
In March 1983 Aruba reached an official agreement within the kingdom for its independence, to be developed in a series of steps as the Crown granted increasing autonomy. In August 1985, Aruba drafted a constitution that was unanimously approved. On 1 January 1986, after the 1985 general election was held for its first parliament, Aruba seceded from the Netherlands Antilles, officially becoming a country of the Kingdom of the Netherlands, with full independence planned for 1996. Croes was seriously injured in a traffic accident in 1985, slipping into a coma. He died in 1986, never seeing the enacting of status aparte for Aruba for which he had worked over many years. After his death, Croes was proclaimed Libertador di Aruba. Croes' successor, Henny Eman of the Aruban People's Party became the first Prime Minister of Aruba.
Meanwhile, in 1985, Aruba's oil refinery closed. It had provided Aruba with 30 percent of its real income and 50 percent of government revenue. The significant blow to the economy led to a push for a dramatic increase in tourism, and that sector has expanded to become the island's largest industry. At a convention in The Hague in 1990, at the request of Prime Minister Nelson Oduber, the governments of Aruba, the Netherlands, and the Netherlands Antilles postponed indefinitely Aruba's transition to full independence. The article scheduling Aruba's complete independence was rescinded in 1995, although it was decided that the process could be revived after another referendum. |
Aruba | Geography | Geography
Aruba is located 77 km (48 mi) west of Curaçao and 29 km (18 mi) north of Paraguaná Peninsula of Venezuela. Aruba showcases three distinct landscapes. The northwestern region is primarily characterized by flat batholith landscapes. Notable landmarks include the conical Hooiberg hill and rock formations like Ayo and Casibari. Moreover, the northeastern part of the island features the oldest formations known as the Aruba Lava Formation. This region is marked by rolling hills, including Jamanota, and is home to Arikok National Park, and limestone terraces surround these two landscapes. The low-lying limestone terrace regions are defined by their white sandy beaches and the high plateaus on the north side of the island, in contrast, are constantly battered by the rough waters of the ocean, featuring caves and small natural bridge formations.
The arid landscape in Aruba is not solely a product of its climate but is also a consequence of extensive deforestation and exploitation during the Spanish colonization of the island. Consequently, certain crops, such as aloe vera, thrive in this environment due to the high calcium-rich soil known as liming. As of 2022, Aruba only has 2.3% of forest-covered land area and only 0.5% of protected natural area. The Aruba Conservation Foundation, established in 2003, oversees the management of the conservation of 16 established protected areas, which encompass a total of nearly 25% of the island's surface, as well as four Marine Protected Areas (MPAs)ACF, Aruba Conservation Foundation. est. 2003. vis. 2025. https://acf.aw/nature-conservation The Arikok National Park, established as formal conservation land in 2000, covers 20% of the island.This Rare Earth. vis. 2025 https://thisrareearth.com/arikok-national-park-aruba/ Forest cover is around 2% of the total land area, equivalent to 420 hectares (ha) of forest in 2020, which was unchanged from 1990. None of the forest was reported to be primary forest (consisting of native tree species with no clearly visible indications of human activity), and no forest area was found within protected areas.
The geography includes naturally formed rooi or gullies that channel rainwater towards dams and ultimately the ocean. Other than Arikok National Park, the Bubali Bird Sanctuary is the only significant body of water on the island that holds the status of protected nature reserve and serves as a brackish water lagoon. |
Aruba | Regions | Regions
Aruba is divided into eight regions for census purposes, with no administrative function. Some correspond to parishes and include several community facilities.
Name Area (km2) Population 1991 census Population 2000 census Population 2010 census Population 2020 census Noord Oranjestad West Oranjestad Oost Paradera San Nicolaas Noord San Nicolaas Zuid Santa Cruz Savaneta Total Aruba |
Aruba | Flora and fauna | Flora and fauna
The landscape is characterized by common xeric scrublands featuring various cacti, thorny shrubs, and evergreen plants. Notably, aloe vera is also found on the island, and its economic significance has led to its inclusion on the coat of arms of Aruba. Cacti include melocactus and opuntia, with opuntia stricta being prominent. Drought-tolerant trees like Caesalpinia coriaria and Vachellia tortuosa are present. The isolation from the South America mainland contributed to the evolution of multiple endemic species. The island provides a habitat for unique wildlife, including the endemic Aruban Whiptail, Aruba Rattlesnake, as well as subspecies of Aruban Burrowing Owl and Brown-throated Parakeet. |
Aruba | Climate and natural hazards | Climate and natural hazards
According to the Köppen climate classification, Aruba is characterized by a hot semi-arid climate (Köppen BSh), characterized by limited rainfall, totaling just annually. Notably, Aruba remains dry even during its supposed rainy season. Rainfall can be highly variable,Dewar, Robert E. and Wallis, James R; 'Geographical patterning in interannual rainfall variability in the tropics and near tropics: An L-moments approach'; in Journal of Climate, 12; pp. 3457–3466 ranging from as little as during strong El Niño years (e.g. 1911/1912, 1930/1931, 1982/1983, 1997/1998) to over in La Niña years, such as 1933/1934, 1970/1971 or 1988/1989.
An exception to the general aridity is observed during the short rainy season from September to January. During this period, the southward retreat of the Intertropical Convergence Zone leads to more frequent moist northeasterly winds. Aruba is positioned south of the Main Development Region for tropical cyclones and generally avoids the direct impact of these storms. However, late in the 2020 Atlantic hurricane season, the island was affected by two hurricanes in their early stages.
In Oranjestad, mean monthly temperatures remain consistently moderate, with little variation (low diurnal temperature variation) ranging from to . This temperature stability is moderated by the constant trade winds originating from the northeast, sweeping in from the Atlantic Ocean. |
Aruba | Demographics | Demographics
In terms of country of birth, the population is estimated to be 66% Aruban, 9.1% Colombian, 4.3% Dutch, 5.1% Dominican, 3.2% Venezuelan, 2.2% Curaçaoan, 1.5% Haitian, 1.2% Surinamese, 1.1% Peruvian, 1.1% Chinese, 6.2% from other backgrounds. In terms of nationality, the population is estimated to be 78.7% Dutch, 6.6% Colombian, 5.5% Venezuelan, 2.8% Dominican; 1.3% Haitian, and 5.1% from other backgrounds (). In 2019, recently arrived Venezuelan refugees were estimated to number around 17,000 on Aruba, accounting for some 15% of the population.
Aruba's population has strong Arawak heritage compared to most Caribbean islands, although there are no full-blooded Aboriginals remaining. The islanders' features clearly reflect their genetic Arawak heritage. The population has diverse origins. The majority of the population of Aruba is of mixed ancestry including European, Amerindian and to a lesser extent African and/or Asian ancestry with minorities of various other groups and nationalities. Arubans are primarily descended from Caquetío Indians, Dutch settlers, Spanish settlers, enslaved Africans and to a lesser extent various other groups who have settled on Aruba over time, including Venezuelans, Colombians, Dominicans, Portuguese, Greeks, Italians, English, French, Germans, West Indians, Indo-Caribbeans, Chinese, Filipinos, Koreans, Javanese, Levantine Arabs and Sephardic Jews.
The population experienced fluctuations between 1972 and 2022, primarily influenced by net migration. While there have been periods of growth, there have also been declines, especially during economic challenges. Notably, between 1988 and 2016, the population nearly doubled. However, in 2017, a decline occurred, breaking almost three decades of continuous growth. The first three years of the ongoing COVID-19 pandemic (2020–2022) also contributed to a population decrease, mainly due to reduced births and emigration.
As of the 3rd quarter in 2024, the population stood at 108,027 people, marking a modest 0.4% growth compared to the previous year. This increase was driven by a significant rise in immigration, which saw a 20.4 percent uptick. |
Aruba | Language | Language
Aruba is a multilingual society. The Official languages are Dutch and Papiamento. While Dutch is the sole language for all administration and legal matters, Papiamento is the predominant language used in Aruba. Papiamento is a Portuguese/Spanish based creole language, spoken on Aruba, Bonaire, and Curaçao that also incorporates words from the Caquetio language, Dutch, various West African languages and English. English and Spanish are also widely spoken on the island, their usage having grown due to tourism and immigration. Other common languages spoken, based on the size of their community, include Portuguese, Cantonese, French and German.
In recent years, the government has shown an increased interest in acknowledging the cultural and historical importance of Papiamento. Although spoken Papiamento is fairly similar among the several Papiamento-speaking islands, the orthography differs per island, with Aruba using etymological spelling (Papiamento), and Curaçao and Bonaire a phonetic spelling (Papiamentu).
The book Buccaneers of America, first published in 1678, states through eyewitness account that the natives on Aruba spoke Spanish already. Spanish became an important language in the 18th century due to the close economic ties with Spanish colonies in what are now Venezuela and Colombia.Dede pikiña ku su bisiña: Papiamentu-Nederlands en de onverwerkt verleden tijd. van Putte, Florimon., 1999. Zutphen: de Walburg Pers Venezuelan TV networks are received on the island, and there are significant communities of Venezuelans and Colombians on Aruba. Around 13% of the population today speaks Spanish natively. Use of English dates to the early 19th century, when the British ruled Curaçao, Aruba, and Bonaire. When Dutch rule resumed in 1815, officials already noted wide use of the language.Dede pikiña ku su bisiña: Papiamentu-Nederlands en de onverwerkt verleden tijd. van Putte, Florimon., 1999. Zutphen: de Walburg Pers There is also a little studied native variety of English Creole spoken in San Nicolaas, known as San Nicolaas English.
Aruba has newspapers published in Papiamento: Diario, Bon Dia, Solo di Pueblo, and Awe Mainta; English: Aruba Daily, Aruba Today, and The News; and Dutch: Amigoe. There are 18 radio stations (two AM and sixteen FM) and two local television stations (Telearuba and Channel 22). |
Aruba | Religion | Religion
Roman Catholicism is the dominant religion, followed by approximately 75% of the population. In addition to Catholicism, there is a diverse range of religions practiced including Protestantism, Islam, Hinduism, Judaism, and African diaspora religions.thumb|Shrine at Sero Preto, San Nicolas (1963)
The Lourdes Grotto, named after the famous French religious pilgrimage site, was constructed in 1958 by a priest named Erkamp and his parishioners. This shrine is nestled into the rocks of Seroe Preto, just off the main road to San Nicolas. Inside the cave, there is a statue of the Virgin Mary, easily visible from the main road. Each year, on February 11 (the feast of Lady Lourdes), a procession departs from St. Theresita Church in San Nicolas and heads to the grotto, where a Mass is held. |
Aruba | Government | Government
thumb|Parliament of Aruba in Oranjestad
Along with the Netherlands, Curaçao, and Sint Maarten, Aruba is a constituent country of the Kingdom of the Netherlands, with internal autonomy. Matters such as foreign affairs and defense are handled by the Netherlands. Aruba's politics take place within a framework of a 21-member Staten (Parliament) and an eight-member Cabinet; the Staten's 21 members are elected by direct, popular vote to serve a four-year term. The governor of Aruba is appointed for a six-year term by the monarch, and the prime minister and deputy prime minister are indirectly elected by the Staten for four-year terms.thumb|Map of the European Union in the world with overseas countries and territories and outermost regions |
Aruba | Politics | Politics
The legal system is based on the Dutch model. Legal jurisdiction lies with the Gerecht in Eerste Aanleg (Court of First Instance), the Gemeenschappelijk Hof van Justitie van Aruba, Curaçao, Sint Maarten, en van Bonaire, Sint Eustatius en Saba (Joint Court of Justice of Aruba, Curaçao, Sint Maarten, and of Bonaire, Sint Eustatius and Saba) and the Hoge Raad der Nederlanden (Supreme Court of Justice of the Netherlands). The Korps Politie Aruba (Aruba Police Force) is the law enforcement agency and operates district precincts in Oranjestad, Noord, San Nicolaas, and Santa Cruz, where it is headquartered.
Divergent Legal Protections from the rest of the Kingdom of the Netherlands include not being part of the Law Enforcement Council (Raad van de Rechtshandhaving), which is a legal entity based on the Kingdom Act of the July 7, 2010 the Kingdom Act on the Law Enforcement Council. Aruba is the only country in the kingdom that does not have an ombudsman.
Deficit spending has been a staple in Aruba's history, and modestly high inflation has been present as well. By 2006, the government's debt had grown to 1.883 billion Aruban florins. In 2006, the government changed several tax laws to reduce the deficit. Direct taxes have been converted to indirect taxes as proposed by the International Monetary Fund. |
Aruba | Foreign relations | Foreign relations
Aruba is one of the overseas countries and territories (OCT) of the European Union and maintains economic and cultural relations with the European Union and the United States. Aruba is also a member of several international organizations such as the International Monetary Fund and Interpol. Although not officially a part of the European Union, Aruba does receive support from the European Development Fund. |
Aruba | Military | Military
Defence is the responsibility of the Kingdom of the Netherlands. The Dutch Armed Forces that protect the island include the Navy, Marine Corps, and the Coastguard including a platoon sized national guard. All forces are stationed at Marines base in Savaneta. In 1999 the U.S. Department of Defense established a forward operating site the airport. |
Aruba | Education | Education
Historically, Dutch was not widely spoken on the island, except within colonial administration, and its usage increased in the late 19th and early 20th centuries. Students in Curaçao, Aruba, and Bonaire were predominantly taught in Spanish until the late 18th century.Van Putte 1999. Dutch serves as the primary language of instruction, with Papiamento taught as a subject in the lower grades of secondary education.
The educational system mirrors the Dutch education structure, with public national education financed by the government of Aruba. The education landscape includes a mix of public and private institutions, such as the International School of Aruba, the Schakel College, and Colegio Arubano.
The University of Aruba is the national university. Aruba hosts three medical schools, American University School of Medicine Aruba, Aureus University School of Medicine and Xavier University School of Medicine. |
Aruba | Economy | Economy
The economy is dominated by four main industries: tourism, aloe export, petroleum refining, and offshore banking. Aruba has one of the highest standards of living in the Caribbean region. The GDP per capita (PPP) was estimated to be $37,500 in 2017. Its main trading partners are Colombia, the United States, Venezuela, and the Netherlands.
The agriculture and manufacturing sectors are fairly minimal. Gold mining was important in the 19th century. Aloe was introduced in 1840 but did not become a big export until 1890. Cornelius Eman founded Aruba Aloe Balm, and over time the industry became very important to the economy. At one point, two-thirds of the island was covered in aloe vera fields, and Aruba became the largest exporter of aloe in the world. The industry continues today, though on a smaller scale.
Access to biocapacity is much lower than world average. In 2016, Aruba had 0.57 global hectares of biocapacity per person within its territory, much less than the world average of 1.6 global hectares per person. In 2016, Aruba used 6.5 global hectares of biocapacity per person—their ecological footprint of consumption. This means they use almost 12 times the biocapacity that Aruba contains. This is the extent of Aruba's biocapacity deficit.
The official exchange rate of the Aruban florin is pegged to the US dollar at Afl 1.80 to US$1.00. This fact, and the majority of tourists being US, means businesses of hotel and resort districts prefer to bank and trade with the consumer in US dollars. Aruba is a prosperous country. Unemployment is low (although the government has not published statistics since 2013) and per capita income is one of the highest in the Caribbean (approximately $24,087). At the end of 2018, the labor force participation rate was 56.6% for women.
Until the mid-1980s, the main industry was oil refining; the refinery was shut down, and the economy shifted towards tourism. The refinery has been closed and restarted repeatedly during the last decades. In recent years a letter of intent was signed with CITGO (the US subsidiary of the Venezuelan state oil company PDVSA) to explore the possibility of reopening the refinery again.
Until 2009, the Netherlands granted development aid to Aruba. This aid was mainly for law enforcement, education, administrative development, health care and sustainable economic development. This aid was discontinued at Aruba's request in 2009. Since 2015, however, a form of financial supervision has been reintroduced because debt has risen sharply to over 80% of GDP. Aruba has two free trade zones (Barcadera and Bushiri), where import and export and the movement of services are tax-free.thumb|A tourist resort on the island|left |
Aruba | Tourism | Tourism
Aruba has a large and well-developed tourism industry, receiving 1,082,000 tourists who stayed overnight in its territory in 2018. About 75% of the gross national product is earned through tourism and related activities. Most tourists are from North America, with a market-share of 73.3%, followed by Latin America with 15.2% and Europe with 8.3%. In 2018, there were 40,231 visitors from the Netherlands.
For private aircraft passengers bound for the United States, the United States Department of Homeland Security, U.S. Customs and Border Protection has a full pre-clearance facility since 1 February 2001 when Queen Beatrix Airport expanded. Since 2008, Aruba has been the only island to have this service for private flights. |
Aruba | Culture | Culture
Aruba boasts a diverse culture. According to the Bureau Burgelijke Stand en Bevolkingsregister (BBSB, Civil Registry and Population Register), in 2005, the island was home to people from 92 different nationalities. Dutch influence is still evident in traditions like the celebration of Sinterklaas (Saint Nicholas) on December 5 and 6, as well as national holidays like April 27 when Aruba, along with the rest of the Kingdom of the Netherlands, celebrates Koningsdag (King's day) or Dia di Rey (in Papiamento) is celebrated.
On 18 March, Aruba celebrates its National Anthem and Flag Day. Christmas and New Year's Eve are celebrated with the typical music and songs of gaitas for Christmas and the for New Year. Traditional food and drinks like ayaca, ponche crema, ham, and more are also parts of the festive season. January 25 is dedicated to celebrating Betico Croes day, while June 24 is the day for Dia di San Juan. In addition to Christmas, religious holidays such as the Feast of the Ascension and Good Friday are observed.
Aruba's Carnaval is a significant cultural event, akin to celebrations in other Caribbean and Latin American countries. It began in the 1950s, influenced by residents from Venezuela and nearby islands (Curaçao, St. Vincent, Trinidad, Barbados, St. Maarten, and Anguilla) who worked at the oil refinery. The Carnaval Celebrations now spans from early January until Fat Tuesday, featuring a grand parade on the final Sunday of the festivities.
Aruba has seen an increased influence of American culture with rising tourism from the United States. This is evident in the adoption of American celebrations like Halloween in October and Thanksgiving Day in November. |
Aruba | Architecture | Architecture
thumb|Ornate buildings in OranjestadFrom the beginning of the colonization of the Netherlands until the beginning of the 20th century, the architecture in the most inhabited areas was influenced by the Dutch colonial style and also some Spanish elements from the Catholic missionaries. After the boom of the oil industry and the tourist sector in the 20th century, the architectural style of the island incorporated a more American and international influence. In addition, elements of the Art Deco style can still be seen in several buildings in San Nicolas. Therefore, it can be said that the island's architecture is a mixture of Spanish, Dutch, American and Caribbean influences. |
Aruba | Sport | Sport
The most popular sports in Aruba are football, basketball, baseball, and volleyball, as well as beach sports. Aruba has competed at the Olympic Games since 1988. |
Aruba | Infrastructure | Infrastructure
Queen Beatrix International Airport is near Oranjestad. Aruba has four ports: Barcadera, the main cargo port; Paardenbaai, the cruise ship terminal in Oranjestad/Taratata; Commandeurs Baai (Commander's Bay) in Savaneta; and Sint Nicolaas Baai in San Nicolaas. Paardenbaai services all the cruise-ship lines such as Royal Caribbean, Carnival, NCL, Holland America, MSC Cruises, Costa Cruises, P&O Cruises and Disney. Nearly one million tourists enter this port per year. Aruba Ports Authority, owned and operated by the Aruban government, runs these seaports.thumb|The Arrivals building at Queen Beatrix International Airport
Arubus is a government-owned bus company. Its buses operate from 3:30 a.m. until 12:30 a.m., 365 days a year. Private minibuses/people movers service zones such as the Hotel Area, San Nicolaas, Santa Cruz and Noord. A streetcar service runs on rails on the main street of Oranjestad.Street car is up and running The Morning News, 27 February 2013
Water- en Energiebedrijf Aruba, N.V. (W.E.B.) produces and distributes potable water and power. Average daily water consumption in Aruba is about 35,600 m3 (46,500 cu. yd.) per day., and average power generation is 104 MW. W.E.B. produces electricity, which is distributed by N.V. Elmar. Both companies share the same parent holding which is Utilities Aruba N.V. The Sunrise Solar Park was installed and opened in 2018.thumb|Aruba electricity production by source|leftThere are three sewage treatment plants at Zeewijk, Parkietenbos and Bubali. The one in Bubali (near the bird sanctuary) is 4 decades old and is processing over 8,000 m3 (10,000 cu. yd.) per day, around double its original capacity of 4,500 m3 (5900 cu. yd.) per day (due to Aruba's growth). A solid waste landfill (16 hectares; 40 acres) is located at Parkietenbos. The capacity is between 130 and 150 kilotons per year. Sometimes there are huge spontaneous fires creating pollution.
There are two telecommunications providers: government-based Setar, and privately owned Digicel. Digicel is Setar's competitor in wireless technology using the GSM platform. |
Aruba | Places of interest | Places of interest
thumb|right|Hooiberg (hill) |
Aruba | Notable people | Notable people |
Aruba | See also | See also
Central Bank of Aruba
Index of Aruba-related articles
List of monuments of Aruba
Outline of Aruba |
Aruba | Notes | Notes |
Aruba | Sources | Sources
|
Aruba | References | References |
Aruba | Further reading | Further reading
Aymer, Paula L. – Uprooted Women: Migrant Domestics in the Caribbean.
Brown, Enid – Suriname and the Netherlands Antilles: An Annotated English-Language Bibliography.
Gerber, Stanford N. – The Family in the Caribbean: Proceedings of the 2nd Conference on the Family in the Caribbean, Aruba, 1969.
Green, Vera M. – Migrants in Aruba: Interethnic Integration.
Hartert, Ernst – On the Birds of the Islands of Aruba, Curaçao, and Bonaire.
Ridderstaat J., Croes R. and Nijkamp P. (2014), Tourism and Long-run Economic Growth in Aruba, International Journal of Tourism Research, 16, pages 472–487, doi: 10.1002/jtr.1941. |
Aruba | External links | External links
of the Government of Aruba
Category:Island countries
Category:Caribbean countries of the Kingdom of the Netherlands
Category:Countries and territories where Dutch is an official language
Category:Former Dutch colonies
Category:Former Spanish colonies
Category:Former British colonies and protectorates in the Americas
Category:Islands of the Dutch Caribbean
Category:Small Island Developing States
Category:Special territories of the European Union
Category:States and territories established in 1986
Category:Dependent territories in the Caribbean |
Aruba | Table of Content | Short description, Etymology, History, Pre-ceramic age, Early human migration and cultural exchange, Neo-Indian period: the Caquetío, Caquetío chiefdom, Political units and governance, Agriculture, trade, and network, Burial practices, Last indigenous Aruban, Spanish period, Early explorations, Conquistadors, Spanish ranch, Early Dutch period, Dutch conquest: salt, New Netherland, Slavery, English interregnum and economic development, 20th and 21st centuries, Autonomy, Geography, Regions, Flora and fauna, Climate and natural hazards, Demographics, Language, Religion, Government, Politics, Foreign relations, Military, Education, Economy, Tourism, Culture, Architecture, Sport, Infrastructure, Places of interest, Notable people, See also, Notes, Sources, References, Further reading, External links |
Articles of Confederation | Short description | The Articles of Confederation, officially the Articles of Confederation and Perpetual Union, was an agreement and early body of law in the Thirteen Colonies, which served as the nation's first frame of government during the American Revolution. It was debated by the Second Continental Congress at present-day Independence Hall in Philadelphia between July 1776 and November 1777, was finalized by the Congress on November 15, 1777, and came into force on March 1, 1781, after being ratified by all 13 colonial states.
A central and guiding principle of the Articles was the establishment and preservation of the independence and sovereignty of the original 13 states. The Articles consciously established a weak confederal government, affording it only those powers the former colonies recognized as belonging to the British Crown and Parliament during the colonial era. The document provided clearly written rules for how the states' league of friendship, known as the Perpetual Union, was to be organized.
While waiting for all states to ratify the Articles, the Congress observed them as it conducted business during the American Revolution, directing the Revolutionary War effort, conducting diplomacy with foreign states, addressing territorial issues, and dealing with Native American relations. Little changed procedurally once the Articles of Confederation went into effect, since their ratification mostly codified laws already in existence and procedures the Continental Congress had already been following. The body was renamed the Congress of the Confederation, but most Americans continued to call it the Continental Congress, since its organization remained the same.
As the Confederation Congress attempted to govern the continually growing 13 colonial states, its delegates discovered that the limitations on the central government, such as in assembling delegates, raising funds, and regulating commerce, limited its ability to do so. As the government's weaknesses became apparent, especially after Shays's Rebellion, several prominent political thinkers in the fledgling union began asking for changes to the Articles that would strengthen the powers afforded to the central government.
In September 1786, some states met to address interstate protectionist trade barriers between them. Shortly thereafter, as more states became interested in meeting to revise the Articles, a meeting was set in Philadelphia on May 25, 1787. This became the Constitutional Convention. Delegates quickly agreed that the defects of the frame of government could not be remedied by altering the Articles, and so went beyond their mandate by authoring a new constitution and sent it to the states for ratification. After significant ratification debates in each state and across the nation, on March 4, 1789, the government under the Articles was replaced with the federal government under the Constitution. The new Constitution provided for a much stronger federal government by establishing a chief executive (the president), courts, and taxing powers. |
Articles of Confederation | Background and context | Background and context
The political push to increase cooperation among the then-loyal colonies began with the Albany Congress in 1754 and Benjamin Franklin's proposed Albany Plan, an inter-colonial collaboration to help solve mutual local problems. Over the next two decades, some of the basic concepts it addressed would strengthen; others would weaken, especially in the degree of loyalty (or lack thereof) owed the Crown. Colonists' civil disobedience resulted in the British enacting coercive and quelling measures, such as the passage of what colonists called the Intolerable Acts in the British Parliament, and armed skirmishes which resulted in dissidents being proclaimed rebels. These actions eroded the number of colonists continuing to be Loyalists to the Crown. Together with the highly effective propaganda campaign of the Patriot leaders, caused an increasing number of colonists to begin agitating for independence from the mother country. In 1775, with events outpacing communications, the Second Continental Congress began acting as the provisional government for the United Colonies.
It was an era of constitution writing—most states were busy at the task—and leaders felt the new nation must have a written constitution; a "rulebook" for how the new nation should function. During the war, Congress exercised an unprecedented level of political, diplomatic, military and economic authority. It adopted trade restrictions, established and maintained an army, issued fiat money, created a military code and negotiated with foreign governments.
To transform themselves from outlaws into a legitimate nation, the colonists needed international recognition for their cause and foreign allies to support it. In early 1776, Thomas Paine argued in the closing pages of the first edition of Common Sense that the "custom of nations" demanded a formal declaration of American independence if any European power were to mediate a peace between the Americans and Great Britain. The monarchies of France and Spain, in particular, could not be expected to aid those they considered rebels against another legitimate monarch. Foreign courts needed to have American grievances laid before them persuasively in a "manifesto" which could also reassure them that the Americans would be reliable trading partners. Without such a declaration, Paine concluded, "[t]he custom of all courts is against us, and will be so, until, by an independence, we take rank with other nations."
Beyond improving their existing association, the records of the Second Continental Congress show that the need for a declaration of independence was intimately linked with the demands of international relations. On June 7, 1776, Richard Henry Lee introduced a resolution before the Continental Congress declaring the colonies independent; at the same time, he also urged Congress to resolve "to take the most effectual measures for forming foreign Alliances" and to prepare a plan of confederation for the newly independent states. Congress then created three overlapping committees to draft the Declaration, a model treaty, and the Articles of Confederation. The Declaration announced the states' entry into the international system; the model treaty was designed to establish amity and commerce with other states; and the Articles of Confederation, which established "a firm league" among the thirteen free and independent states, constituted an international agreement to set up central institutions for the conduct of vital domestic and foreign affairs. |
Articles of Confederation | Drafting | Drafting
thumb|right|upright=.90|alt=Historical 13-cent postage stamp commemorating the Articles of Confederation 200th anniversary|1977 13-cent U.S. Postage stamp commemorating the Articles of Confederation bicentennial; the draft was completed on November 15, 1777
On June 12, 1776, a day after appointing the Committee of Five to prepare a draft of the Declaration of Independence, the Second Continental Congress resolved to appoint a committee of 13 with one representative from each colony to prepare a draft of a constitution for a union of the states. The committee was made up of the following individuals:
John Dickinson (Pennsylvania, chairman of the committee)
Samuel Adams (Massachusetts)
Josiah Bartlett (New Hampshire)
Button Gwinnett (Georgia)
Joseph Hewes (North Carolina)
Stephen Hopkins (Rhode Island)
Robert R. Livingston (New York)
Thomas McKean (Delaware)
Thomas Nelson (Virginia)
Edward Rutledge (South Carolina)
Roger Sherman (Connecticut)
Thomas Stone (Maryland)
Francis Hopkinson (New Jersey, added to the committee last)
The committee met frequently, and chairman John Dickinson presented their results to the Congress on July 12, 1776. Afterward, there were long debates on such issues as state sovereignty, the exact powers to be given to Congress, whether to have a judiciary, western land claims, and voting procedures. To further complicate work on the constitution, Congress was forced to leave Philadelphia twice, for Baltimore, Maryland, in the winter of 1776, and later for Lancaster then York, Pennsylvania, in the fall of 1777, to evade advancing British troops. Even so, the committee continued with its work.
The final draft of the Articles of Confederation and Perpetual Union was completed on November 15, 1777. Consensus was achieved by including language guaranteeing that each state retained its sovereignty, leaving the matter of western land claims in the hands of the individual states, including language stating that votes in Congress would be en bloc by state, and establishing a unicameral legislature with limited and clearly delineated powers. |
Articles of Confederation | Ratification | Ratification
The Articles of Confederation was submitted to the states for ratification in late November 1777. The first state to ratify was Virginia on December 16, 1777; 12 states had ratified the Articles by February 1779, 14 months into the process. The lone holdout, Maryland, refused to go along until the landed states, especially Virginia, had indicated they were prepared to cede their claims west of the Ohio River to the Union. It would be two years before the Maryland General Assembly became satisfied that the various states would follow through, and voted to ratify. During this time, Congress observed the Articles as its de facto frame of government. Maryland finally ratified the Articles on February 2, 1781. Congress was informed of Maryland's assent on March 1, and officially proclaimed the Articles of Confederation to be the law of the land.
The several states ratified the Articles of Confederation on the following dates: References to a 1778 Virginia ratification are based on an error in the Journals of Congress: "The published Journals of Congress print this enabling act of the Virginia assembly under date of Dec. 15, 1778. This error has come from the MS. vol. 9 (History of Confederation), p. 123, Papers of the Continental Congress, Library of Congress."
State Date 30px Virginia 30px South Carolina 30px New York 30px Rhode Island 26px Connecticut 30px Georgia 30px New Hampshire 30px Pennsylvania 30px Massachusetts 30px North Carolina 30px New Jersey 30px Delaware 30px Maryland |
Articles of Confederation | Article summaries | Article summaries
The Articles of Confederation contain a preamble, thirteen articles, a conclusion, and a signatory section. The individual articles set the rules for current and future operations of the confederation's central government. Under the Articles, the states retained sovereignty over all governmental functions not specifically relinquished to the national Congress, which was empowered to make war and peace, negotiate diplomatic and commercial agreements with foreign countries, and to resolve disputes between the states. The document also stipulates that its provisions "shall be inviolably observed by every state" and that "the Union shall be perpetual".
Summary of the purpose and content of each of the 13 articles:
Establishes the name of the confederation with these words: "The stile of this confederacy shall be 'The United States of America.
Asserts the sovereignty of each state, except for the specific powers delegated to the confederation government: "Each state retains its sovereignty, freedom, and independence, and every power, jurisdiction, and right, which is not by this Confederation expressly delegated."
Declares the purpose of the confederation: "The said States hereby severally enter into a firm league of friendship with each other, for their common defense, the security of their liberties, and their mutual and general welfare, binding themselves to assist each other, against all force offered to, or attacks made upon them, or any of them, on account of religion, sovereignty, trade, or any other pretense whatever."
Elaborates upon the intent "to secure and perpetuate mutual friendship and intercourse among the people of the different States in this union," and to establish equal treatment and freedom of movement for the free inhabitants of each state to pass unhindered between the states, excluding "paupers, vagabonds, and fugitives from justice." All these people are entitled to equal rights established by the state into which they travel. If a crime is committed in one state and the perpetrator flees to another state, if caught they will be extradited to and tried in the state in which the crime was committed.
Allocates one vote in the Congress of the Confederation (the "United States in Congress Assembled") to each state, which is entitled to a delegation of between two and seven members. Members of Congress are to be appointed by state legislatures. No congressman may serve more than three out of any six years.
Only the central government may declare war, or conduct foreign political or commercial relations. No state or official may accept foreign gifts or titles, and granting any title of nobility is forbidden to all. No states may form any sub-national groups. No state may tax or interfere with treaty stipulations already proposed. No state may wage war without permission of Congress, unless invaded or under imminent attack on the frontier; no state may maintain a peacetime standing army or navy, unless infested by pirates, but every State is required to keep ready, a well-trained, disciplined, and equipped militia.
Whenever an army is raised for common defense, the state legislatures shall assign military ranks of colonel and below.
Expenditures by the United States of America will be paid with funds raised by state legislatures, and apportioned to the states in proportion to the real property values of each.
Powers and functions of the United States in Congress Assembled.
Grants to the United States in Congress assembled the sole and exclusive right and power to determine peace and war; to exchange ambassadors; to enter into treaties and alliances, with some provisos; to establish rules for deciding all cases of captures or prizes on land or water; to grant letters of marque and reprisal (documents authorizing privateers) in times of peace; to appoint courts for the trial of pirates and crimes committed on the high seas; to establish courts for appeals in all cases of captures, but no member of Congress may be appointed a judge; to set weights and measures (including coins), and for Congress to serve as a final court for disputes between states.
The court will be composed of jointly appointed commissioners or Congress shall appoint them. Each commissioner is bound by oath to be impartial. The court's decision is final.
Congress shall regulate the post offices; appoint officers in the military; and regulate the armed forces.
The United States in Congress assembled may appoint a president who shall not serve longer than one year per three-year term of the Congress.
Congress may request requisitions (demands for payments or supplies) from the states in proportion with their population, or take credit.
Congress may not declare war, enter into treaties and alliances, appropriate money, or appoint a commander in chief without nine states assenting. Congress shall keep a journal of proceedings and adjourn for periods not to exceed six months.
When Congress is in recess, any of the powers of Congress may be executed by "The committee of the states, or any nine of them", except for those powers of Congress which require nine states in Congress to execute.
If Canada [referring to the British Province of Quebec] accedes to this confederation, it will be admitted. No other colony could be admitted without the consent of nine states.
Affirms that the Confederation will honor all bills of credit incurred, monies borrowed, and debts contracted by Congress before the existence of the Articles.
Declares that the Articles shall be perpetual, and may be altered only with the approval of Congress and the ratification of all the state legislatures. |
Articles of Confederation | Congress under the Articles | Congress under the Articles |
Articles of Confederation | Army | Army
Under the Articles, Congress had the authority to regulate and fund the Continental Army, but it lacked the power to compel the States to comply with requests for either troops or funding. This left the military vulnerable to inadequate funding, supplies, and even food. Further, although the Articles enabled the states to present a unified front when dealing with the European powers, as a tool to build a centralized war-making government, they were largely a failure; Historian Bruce Chadwick wrote:
Phelps wrote:
The Continental Congress, before the Articles were approved, had promised soldiers a pension of half pay for life. However Congress had no power to compel the states to fund this obligation, and as the war wound down after the victory at Yorktown the sense of urgency to support the military was no longer a factor. No progress was made in Congress during the winter of 1783–84. General Henry Knox, who would later become the first Secretary of War under the Constitution, blamed the weaknesses of the Articles for the inability of the government to fund the army. The army had long been supportive of a strong union.
Knox wrote:
As Congress failed to act on the petitions, Knox wrote to Gouverneur Morris, four years before the Philadelphia Convention was convened, "As the present Constitution is so defective, why do not you great men call the people together and tell them so; that is, to have a convention of the States to form a better Constitution."
Once the war had been won, the Continental Army was largely disbanded. A very small national force was maintained to man the frontier forts and to protect against Native American attacks. Meanwhile, each of the states had an army (or militia), and 11 of them had navies. The wartime promises of bounties and land grants to be paid for service were not being met. In 1783, George Washington defused the Newburgh conspiracy, but riots by unpaid Pennsylvania veterans forced Congress to leave Philadelphia temporarily.
The Congress from time to time during the Revolutionary War requisitioned troops from the states. Any contributions were voluntary, and in the debates of 1788, the Federalists (who supported the proposed new Constitution) claimed that state politicians acted unilaterally, and contributed when the Continental army protected their state's interests. The Anti-Federalists claimed that state politicians understood their duty to the Union and contributed to advance its needs. Dougherty (2009) concludes that generally the States' behavior validated the Federalist analysis. This helps explain why the Articles of Confederation needed reforms. |
Articles of Confederation | Foreign policy | Foreign policy
The 1783 Treaty of Paris, which ended hostilities with Great Britain, languished in Congress for several months because too few delegates were present at any one time to constitute a quorum so that it could be ratified. Afterward, the problem only got worse as Congress had no power to enforce attendance. Rarely did more than half of the roughly sixty delegates attend a session of Congress at the time, causing difficulties in raising a quorum. The resulting paralysis embarrassed and frustrated many American nationalists, including George Washington. Many of the most prominent national leaders, such as Washington, John Adams, John Hancock, and Benjamin Franklin, retired from public life, served as foreign delegates, or held office in state governments; and for the general public, local government and self-rule seemed quite satisfactory. This served to exacerbate Congress's impotence.
Inherent weaknesses in the confederation's frame of government also frustrated the ability of the government to conduct foreign policy. In 1786, Thomas Jefferson, concerned over the failure of Congress to fund an American naval force to confront the Barbary pirates, wrote in a diplomatic correspondence to James Monroe that, "It will be said there is no money in the treasury. There never will be money in the treasury till the Confederacy shows its teeth." [Original source: The Papers of Thomas Jefferson, vol. 10, June 22–December 31, 1786, ed. Julian P. Boyd. Princeton: Princeton University Press, 1954, pp. 560–566]
Furthermore, the 1786 Jay–Gardoqui Treaty with Spain also showed weakness in foreign policy. In this treaty, which was never ratified, the United States was to give up rights to use the Mississippi River for 25 years, which would have economically strangled the settlers west of the Appalachian Mountains. Finally, due to the Confederation's military weakness, it could not compel the British army to leave frontier forts which were on American soil—and which, in 1783, the British promised to leave, but which they delayed leaving pending U.S. implementation of other provisions such as ending action against Loyalists and allowing them to seek compensation. This incomplete British implementation of the Treaty of Paris would later be resolved by the implementation of Jay's Treaty in 1795 after the federal Constitution came into force. |
Articles of Confederation | Taxation and commerce | Taxation and commerce
Under the Articles of Confederation, the central government's power was kept quite limited. The Confederation Congress could make decisions but lacked enforcement powers. Implementation of most decisions, including modifications to the Articles, required unanimous approval of all thirteen state legislatures.
Congress was denied any powers of taxation: it could only request money from the states. The states often failed to meet these requests in full, leaving both Congress and the Continental Army chronically short of money. As more money was printed by Congress, the continental dollars depreciated. In 1779, George Washington wrote to John Jay, who was serving as the president of the Continental Congress, "that a wagon load of money will scarcely purchase a wagon load of provisions." Mr. Jay and the Congress responded in May by requesting $45 million from the States. In an appeal to the States to comply, Jay wrote that the taxes were "the price of liberty, the peace, and the safety of yourselves and posterity." He argued that Americans should avoid having it said "that America had no sooner become independent than she became insolvent" or that "her infant glories and growing fame were obscured and tarnished by broken contracts and violated faith." The States did not respond with any of the money requested from them.
Congress had also been denied the power to regulate either foreign trade or interstate commerce and, as a result, all of the States maintained control over their own trade policies. The states and the Confederation Congress both incurred large debts during the Revolutionary War, and how to repay those debts became a major issue of debate following the War. Some States paid off their war debts and others did not. Federal assumption of the states' war debts became a major issue in the deliberations of the Constitutional Convention. |
Articles of Confederation | Accomplishments | Accomplishments
Nevertheless, the Confederation Congress did take two actions with long-lasting impact. The Land Ordinance of 1785 and Northwest Ordinance created territorial government, set up protocols for the admission of new states and the division of land into useful units, and set aside land in each township for public use. This system represented a sharp break from imperial colonization, as in Europe, and it established the precedent by which the national (later, federal) government would be sovereign and expand westward—as opposed to the existing states doing so under their sovereignty.
The Land Ordinance of 1785 established both the general practices of land surveying in the west and northwest and the land ownership provisions used throughout the later westward expansion beyond the Mississippi River. Frontier lands were surveyed into the now-familiar squares of land called the township (36 square miles), the section (one square mile), and the quarter section (160 acres). This system was carried forward to most of the States west of the Mississippi (excluding areas of Texas and California that had already been surveyed and divided up by the Spanish Empire). Then, when the Homestead Act was enacted in 1867, the quarter section became the basic unit of land that was granted to new settler-farmers.
The Northwest Ordinance of 1787 noted the agreement of the original states to give up northwestern land claims, organized the Northwest Territory and laid the groundwork for the eventual creation of new states. Although it did not happen under the articles, the land north of the Ohio River and west of the (present) western border of Pennsylvania ceded by Massachusetts, Connecticut, New York, Pennsylvania, and Virginia, eventually became the states of Ohio, Indiana, Illinois, Michigan, and Wisconsin, and the part of Minnesota that is east of the Mississippi River. The Northwest Ordinance of 1787 also made great advances in the abolition of slavery. New states admitted to the union in this territory would never be slave states.
No new states were admitted to the Union under the Articles of Confederation. The Articles provided for a blanket acceptance of the Province of Quebec (referred to as "Canada" in the Articles) into the United States if it chose to do so. It did not, and the subsequent Constitution carried no such special provision of admission. Additionally, ordinances to admit Frankland (later modified to Franklin), Kentucky, and Vermont to the Union were considered, but none were approved. |
Articles of Confederation | Presidents of Congress | Presidents of Congress
Under the Articles of Confederation, the presiding officer of Congress—referred to in many official records as President of the United States in Congress Assembled—chaired the Committee of the States when Congress was in recess, and performed other administrative functions. He was not, however, an executive in the way the later president of the United States is a chief executive, since all of the functions he executed were under the direct control of Congress.
There were 10 presidents of Congress under the Articles. The first, Samuel Huntington, had been serving as president of the Continental Congress since September 28, 1779.
President TermSamuel Huntington July 10, 1781Thomas McKean November 5, 1781John Hanson November 4, 1782Elias Boudinot November 3, 1783Thomas Mifflin June 3, 1784 Richard Henry Lee November 4, 1785John Hancock June 5, 1786Nathaniel Gorham November 3, 1786Arthur St. Clair November 4, 1787Cyrus Griffin November 15, 1788 |
Articles of Confederation | U.S. under the Articles | U.S. under the Articles
The peace treaty left the United States independent and at peace but with an unsettled governmental structure. The Articles envisioned a permanent confederation but granted to the Congress—the only federal institution—little power to finance itself or to ensure that its resolutions were enforced. There was no president, no executive agencies, no judiciary, and no tax base. The absence of a tax base meant that there was no way to pay off state and national debts from the war years except by requesting money from the states, which seldom arrived. Although historians generally agree that the Articles were too weak to hold the fast-growing nation together, they do give credit to the settlement of the western issue, as the states voluntarily turned over their lands to national control.
By 1783, with the end of the British blockade, the new nation was regaining its prosperity. However, trade opportunities were restricted by the mercantilism of the British and French empires. The ports of the British West Indies were closed to all staple products which were not carried in British ships. France and Spain established similar policies. Simultaneously, new manufacturers faced sharp competition from British products which were suddenly available again. Political unrest in several states and efforts by debtors to use popular government to erase their debts increased the anxiety of the political and economic elites which had led the Revolution. The apparent inability of the Congress to redeem the public obligations (debts) incurred during the war, or to become a forum for productive cooperation among the states to encourage commerce and economic development, only aggravated a gloomy situation. In 1786–87, Shays's Rebellion, an uprising of dissidents in western Massachusetts against the state court system, threatened the stability of state government.
The Continental Congress printed paper money which was so depreciated that it ceased to pass as currency, spawning the expression "not worth a continental". Congress could not levy taxes and could only make requisitions upon the States. Less than a million and a half dollars came into the treasury between 1781 and 1784, although the governors had been asked for two million in 1783 alone.
When John Adams went to London in 1785 as the first representative of the United States, he found it impossible to secure a treaty for unrestricted commerce. Demands were made for favors and there was no assurance that individual states would agree to a treaty. Adams stated it was necessary for the States to confer the power of passing navigation laws to Congress, or that the States themselves pass retaliatory acts against Great Britain. Congress had already requested and failed to get power over navigation laws. Meanwhile, each State acted individually against Great Britain to little effect. When other New England states closed their ports to British shipping, Connecticut hastened to profit by opening its ports.
By 1787, Congress was unable to protect manufacturing and shipping. State legislatures were unable or unwilling to resist attacks upon private contracts and public credit. Land speculators expected no rise in values when the government could not defend its borders nor protect its frontier population.
The idea of a convention to revise the Articles of Confederation grew in favor. Alexander Hamilton realized while serving as Washington's top aide that a strong central government was necessary to avoid foreign intervention and allay the frustrations due to an ineffectual Congress. Hamilton led a group of like-minded nationalists, won Washington's endorsement, and convened the Annapolis Convention in 1786 to petition Congress to call a constitutional convention to meet in Philadelphia to remedy the long-term crisis. |
Articles of Confederation | Signatures | Signatures
The Second Continental Congress approved the Articles for distribution to the states on November 15, 1777. A copy was made for each state and one was kept by the Congress. On November 28, the copies sent to the states for ratification were unsigned, and the cover letter, dated November 17, had only the signatures of Henry Laurens and Charles Thomson, who were the President and Secretary to the Congress.
The Articles, however, were unsigned, and the date was blank. Congress began the signing process by examining their copy of the Articles on June 27, 1778. They ordered a final copy prepared (the one in the National Archives), and that delegates should inform the secretary of their authority for ratification.
On July 9, 1778, the prepared copy was ready. They dated it and began to sign. They also requested each of the remaining states to notify its delegation when ratification was completed. On that date, delegates present from New Hampshire, Massachusetts, Rhode Island, Connecticut, New York, Pennsylvania, Virginia and South Carolina signed the Articles to indicate that their states had ratified. New Jersey, Delaware and Maryland could not, since their states had not ratified. North Carolina and Georgia also were unable to sign that day, since their delegations were absent.
After the first signing, some delegates signed at the next meeting they attended. For example, John Wentworth of New Hampshire added his name on August 8. John Penn was the first of North Carolina's delegates to arrive (on July 10), and the delegation signed the Articles on July 21, 1778.
The other states had to wait until they ratified the Articles and notified their Congressional delegation. Georgia signed on July 24, New Jersey on November 26, and Delaware on February 12, 1779. Maryland refused to ratify the Articles until every state had ceded its western land claims. Chevalier de La Luzerne, French Minister to the United States, felt that the Articles would help strengthen the American government. In 1780, when Maryland requested France provide naval forces in the Chesapeake Bay for protection from the British (who were conducting raids in the lower part of the bay), he indicated that French Admiral Destouches would do what he could but La Luzerne also "sharply pressed" Maryland to ratify the Articles, thus suggesting the two issues were related.
thumb|upright=.90|The Act of the Maryland legislature to ratify the Articles of Confederation, February 2, 1781
On February 2, 1781, the much-awaited decision was taken by the Maryland General Assembly in Annapolis. As the last piece of business during the afternoon Session, "among engrossed Bills" was "signed and sealed by Governor Thomas Sim Lee in the Senate Chamber, in the presence of the members of both Houses ... an Act to empower the delegates of this state in Congress to subscribe and ratify the articles of confederation" and perpetual union among the states. The Senate then adjourned "to the first Monday in August next." The decision of Maryland to ratify the Articles was reported to the Continental Congress on February 12. The confirmation signing of the Articles by the two Maryland delegates took place in Philadelphia at noon time on March 1, 1781, and was celebrated in the afternoon. With these events, the Articles were entered into force and the United States of America came into being as a sovereign federal state.
Congress had debated the Articles for over a year and a half, and the ratification process had taken nearly three and a half years. Many participants in the original debates were no longer delegates, and some of the signers had only recently arrived. The Articles of Confederation and Perpetual Union were signed by a group of men who were never present in the Congress at the same time. |
Articles of Confederation | Signers | Signers
The signers and the states they represented were:
Connecticut
Roger Sherman
Samuel Huntington
Oliver Wolcott
Titus Hosmer
Andrew Adams
Delaware
Thomas McKean
John Dickinson
Nicholas Van Dyke
Georgia
John Walton
Edward Telfair
Edward Langworthy
Maryland
John Hanson
Daniel Carroll
Massachusetts Bay
John Hancock
Samuel Adams
Elbridge Gerry
Francis Dana
James Lovell
Samuel Holten
New Hampshire
Josiah Bartlett
John Wentworth Jr.
New Jersey
John Witherspoon
Nathaniel Scudder
New York
James Duane
Francis Lewis
William Duer
Gouverneur Morris
North Carolina
John Penn
Cornelius Harnett
John Williams
Pennsylvania
Robert Morris
Daniel Roberdeau
Jonathan Bayard Smith
William Clingan
Joseph Reed
Rhode Island and Providence Plantations
William Ellery
Henry Marchant
John Collins
South Carolina
Henry Laurens
William Henry Drayton
John Mathews
Richard Hutson
Thomas Heyward Jr.
Virginia
Richard Henry Lee
John Banister
Thomas Adams
John Harvie
Francis Lightfoot Lee
Roger Sherman (Connecticut) was the only person to sign all four great state papers of the United States: the Continental Association, the United States Declaration of Independence, the Articles of Confederation and the United States Constitution.
Robert Morris (Pennsylvania) signed three of the great state papers of the United States: the United States Declaration of Independence, the Articles of Confederation and the United States Constitution.
John Dickinson (Delaware), Daniel Carroll (Maryland) and Gouverneur Morris (New York), along with Sherman and Robert Morris, were the only five people to sign both the Articles of Confederation and the United States Constitution (Gouverneur Morris represented Pennsylvania when signing the Constitution). |
Articles of Confederation | Parchment pages | Parchment pages
Original parchment pages of the Articles of Confederation, National Archives and Records Administration. |
Articles of Confederation | Revision and replacement | Revision and replacement
In September 1786, delegates from five states met at what became known as the Annapolis Convention to discuss the need for reversing the protectionist interstate trade barriers that each state had erected. At its conclusion, delegates voted to invite all states to a larger convention to be held in Philadelphia in 1787. The Confederation Congress later endorsed this convention "for the sole and express purpose of revising the Articles of Confederation". Although the states' representatives to the Constitutional Convention in Philadelphia were only authorized to amend the Articles, delegates held secret, closed-door sessions and wrote a new constitution. The new frame of government gave much more power to the central government, but characterization of the result is disputed. The general goal of the authors was to get close to a republic as defined by the philosophers of the Age of Enlightenment, while trying to address the many difficulties of the interstate relationships. Historian Forrest McDonald, using the ideas of James Madison from Federalist 39, described the change this way:
In May 1786, Charles Pinckney of South Carolina proposed that Congress revise the Articles of Confederation. Recommended changes included granting Congress power over foreign and domestic commerce, and providing means for Congress to collect money from state treasuries. Unanimous approval was necessary to make the alterations, however, and Congress failed to reach a consensus. The weakness of the Articles in establishing an effective unifying government was underscored by the threat of internal conflict both within and between the states, especially after Shays's Rebellion threatened to topple the state government of Massachusetts.
Historian Ralph Ketcham commented on the opinions of Patrick Henry, George Mason, and other Anti-Federalists who were not so eager to give up the local autonomy won by the revolution:
Historians have given many reasons for the perceived need to replace the articles in 1787. Jillson and Wilson (1994) point to the financial weakness as well as the norms, rules and institutional structures of the Congress, and the propensity to divide along sectional lines.
Rakove identifies several factors that explain the collapse of the Confederation. The lack of compulsory direct taxation power was objectionable to those wanting a strong centralized state or expecting to benefit from such power. It could not collect customs after the war because tariffs were vetoed by Rhode Island. Rakove concludes that their failure to implement national measures "stemmed not from a heady sense of independence but rather from the enormous difficulties that all the states encountered in collecting taxes, mustering men, and gathering supplies from a war-weary populace." The second group of factors Rakove identified derived from the substantive nature of the problems the Continental Congress confronted after 1783, especially the inability to create a strong foreign policy. Finally, the Confederation's lack of coercive power reduced the likelihood for profit to be made by political means, thus potential rulers were uninspired to seek power.
When the war ended in 1783, certain special interests had incentives to create a new "merchant state", much like the British state people had rebelled against. In particular, holders of war scrip and land speculators wanted a central government to pay off scrip at face value and to legalize western land holdings with disputed claims. Also, manufacturers wanted a high tariff as a barrier to foreign goods, but competition among states made this impossible without a central government. |
Articles of Confederation | Legitimacy of closing down | Legitimacy of closing down
Two prominent political leaders in the Confederation, John Jay of New York and Thomas Burke of North Carolina believed that "the authority of the congress rested on the prior acts of the several states, to which the states gave their voluntary consent, and until those obligations were fulfilled, neither nullification of the authority of congress, exercising its due powers, nor secession from the compact itself was consistent with the terms of their original pledges."
According to Article XIII of the Confederation, any alteration had to be approved unanimously:
[T]he Articles of this Confederation shall be inviolably observed by every State, and the Union shall be perpetual; nor shall any alteration at any time hereafter be made in any of them; unless such alteration be agreed to in a Congress of the United States, and be afterwards confirmed by the legislatures of every State.
On the other hand, Article VII of the proposed Constitution stated that it would become effective after ratification by a mere nine states, without unanimity:
The Ratification of the Conventions of nine States, shall be sufficient for the Establishment of this Constitution between the States so ratifying the Same.
The apparent tension between these two provisions was addressed at the time, and remains a topic of scholarly discussion. In 1788, James Madison remarked (in Federalist No. 40) that the issue had become moot: "As this objection ... has been in a manner waived by those who have criticised the powers of the convention, I dismiss it without further observation." Nevertheless, it is a historical and legal question whether opponents of the Constitution could have plausibly attacked the Constitution on that ground. At the time, there were state legislators who argued that the Constitution was not an alteration of the Articles of Confederation, but rather would be a complete replacement so the unanimity rule did not apply. Moreover, the Confederation had proven woefully inadequate and therefore was supposedly no longer binding.
Modern scholars such as Francisco Forrest Martin agree that the Articles of Confederation had lost its binding force because many states had violated it, and thus "other states-parties did not have to comply with the Articles' unanimous consent rule". In contrast, law professor Akhil Amar suggests that there may not have really been any conflict between the Articles of Confederation and the Constitution on this point; Article VI of the Confederation specifically allowed side deals among states, and the Constitution could be viewed as a side deal until all states ratified it. |
Articles of Confederation | Final months | Final months
On July 3, 1788, the Congress received New Hampshire's all-important ninth ratification of the proposed Constitution, thus, according to its terms, establishing it as the new framework of governance for the ratifying states. The following day delegates considered a bill to admit Kentucky into the Union as a sovereign state. The discussion ended with Congress making the determination that, in light of this development, it would be "unadvisable" to admit Kentucky into the Union, as it could do so "under the Articles of Confederation" only, but not "under the Constitution".
By the end of July 1788, 11 of the 13 states had ratified the new Constitution. Congress continued to convene under the Articles with a quorum until October. On Saturday, September 13, 1788, the Confederation Congress voted the resolve to implement the new Constitution, and on Monday, September 15 published an announcement that the new Constitution had been ratified by the necessary nine states, set the first Wednesday in January 1789 for appointing electors, set the first Wednesday in February 1789 for the presidential electors to meet and vote for a new president, and set the first Wednesday of March 1789 as the day "for commencing proceedings" under the new Constitution. On that same September 13, it determined that New York would remain the national capital. |
Articles of Confederation | See also | See also
Court of Appeals in Cases of Capture
Founding Fathers of the United States
Journals of the Continental Congress
History of the United States (1776–1789)
Libertarianism
Perpetual Union
Vetocracy |
Articles of Confederation | Citations | Citations |
Articles of Confederation | General and cited references | General and cited references
(Collection published 1995.)
Rakove, Jack N. (1991) "The Articles of Confederation, 1775–1783. In Jack P. Green and J.R. Pole, eds. The Blackwell Encyclopedia of the American Revolution. Oxford: Blackwell pp. 280–95.
|
Articles of Confederation | External links | External links
Text version of the Articles of Confederation
Articles of Confederation and Perpetual Union
Articles of Confederation and related resources, Library of Congress
Today in History: November 15, Library of Congress
United States Constitution Online—The Articles of Confederation
Free Download of Articles of Confederation Audio
Mobile friendly version of the Articles of Confederation
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Articles of Confederation | Table of Content | Short description, Background and context, Drafting, Ratification, Article summaries, Congress under the Articles, Army, Foreign policy, Taxation and commerce, Accomplishments, Presidents of Congress, U.S. under the Articles, Signatures, Signers, Parchment pages, Revision and replacement, Legitimacy of closing down, Final months, See also, Citations, General and cited references, External links |
Asia Minor (disambiguation) | Wiktionary | Asia Minor is an alternative name for Anatolia, the westernmost protrusion of Asia, comprising the majority of the Republic of Turkey.
Asia Minor may also refer to:
Asia Minor (album), an album by Jamaican-born jazz trumpeter Dizzy Reece
"Asia Minor" (instrumental), a 1961 instrumental recording by Jimmy Wisner (operating under the name Kokomo) |
Asia Minor (disambiguation) | See also | See also
Asia Major (disambiguation) |
Asia Minor (disambiguation) | Table of Content | Wiktionary, See also |
Atlantic Ocean | Short description | thumb|This video was taken by the crew of Expedition 29 on board the ISS. The pass starts from just northeast of the island of Newfoundland over the North Atlantic Ocean to central Africa, over South Sudan.
The Atlantic Ocean is the second largest of the world's five oceanic divisions, with an area of about . It covers approximately 17% of Earth's surface and about 24% of its water surface area. During the Age of Discovery, it was known for separating the New World of the Americas (North America and South America) from the Old World of Afro-Eurasia (Africa, Asia, and Europe).
Through its separation of Afro-Eurasia from the Americas, the Atlantic Ocean has played a central role in the development of human society, globalization, and the histories of many nations. While the Norse were the first known humans to cross the Atlantic, it was the expedition of Christopher Columbus in 1492 that proved to be the most consequential. Columbus' expedition ushered in an age of exploration and colonization of the Americas by European powers, most notably Portugal, Spain, France, and the United Kingdom. From the 16th to 19th centuries, the Atlantic Ocean was the center of both an eponymous slave trade and the Columbian exchange while occasionally hosting naval battles. Such naval battles, as well as growing trade from regional American powers like the United States and Brazil, both increased in degree during the early 20th century, and while no major military conflicts have taken place in the Atlantic recently, the ocean remains a core component of trade around the world.
The Atlantic Ocean occupies an elongated, S-shaped basin extending longitudinally between Europe and Africa to the east, and the Americas to the west. As one component of the interconnected World Ocean, it is connected in the north to the Arctic Ocean, to the Pacific Ocean in the southwest, the Indian Ocean in the southeast, and the Southern Ocean in the south. Other definitions describe the Atlantic as extending southward to Antarctica. The Atlantic Ocean is divided in two parts, the northern and southern Atlantic, by the Equator.International Hydrographic Organization, Limits of Oceans and Seas, 3rd ed. (1953) , pages 4 and 13. |
Atlantic Ocean | Toponymy | Toponymy
thumb|The Aethiopian Ocean depicted in a 1710 French map of Africa
The oldest known mentions of an "Atlantic" sea come from Stesichorus around mid-sixth century BC (Sch. A. R. 1. 211): (, , . ) and in The Histories of Herodotus around 450 BC (Hdt. 1.202.4): (, or ) where the name refers to "the sea beyond the pillars of Hercules" which is said to be part of the sea that surrounds all land. In these uses, the name refers to Atlas, the Titan in Greek mythology, who supported the heavens and who later appeared as a frontispiece in medieval maps and also lent his name to modern atlases. On the other hand, to early Greek sailors and in ancient Greek mythological literature such as the Iliad and the Odyssey, this all-encompassing ocean was instead known as Oceanus, the gigantic river that encircled the world; in contrast to the enclosed seas well known to the Greeks: the Mediterranean and the Black Sea. In contrast, the term "Atlantic" originally referred specifically to the Atlas Mountains in Morocco and the sea off the Strait of Gibraltar and the West African coast.
The term "Aethiopian Ocean", derived from Ancient Ethiopia, was applied to the southern Atlantic as late as the mid-19th century. During the Age of Discovery, the Atlantic was also known to English cartographers as the Great Western Ocean.
thumb|The Atlantic as seen from the shores of Clare Island, Ireland in 1981.
The pond is a term often used by British and American speakers in reference to the northern Atlantic Ocean, as a form of meiosis, or ironic understatement. It is used mostly when referring to events or circumstances "on this side of the pond" or "on the other side of the pond" or "across the pond", rather than to discuss the ocean itself. The term dates to 1640, first appearing in print in a pamphlet released during the reign of Charles I, and reproduced in 1869 in Nehemiah Wallington's Historical Notices of Events Occurring Chiefly in The Reign of Charles I, where "great Pond" is used in reference to the Atlantic Ocean by Francis Windebank, Charles I's Secretary of State. |
Atlantic Ocean | Extent and data | Extent and data
The International Hydrographic Organization (IHO) defined the limits of the oceans and seas in 1953, but some of these definitions have been revised since then and some are not recognized by various authorities, institutions, and countries, for example the CIA World Factbook. Correspondingly, the extent and number of oceans and seas vary.
The Atlantic Ocean is bounded on the west by North and South America. It connects to the Arctic Ocean through the Labrador Sea, Denmark Strait, Greenland Sea, Norwegian Sea and Barents Sea with the northern divider passing through Iceland and Svalbard. To the east, the boundaries of the ocean proper are Europe and Africa: the Strait of Gibraltar (where it connects with the Mediterranean Seaone of its marginal seasand, in turn, the Black Sea, both of which also touch upon Asia).
In the southeast, the Atlantic merges into the Indian Ocean. The 20° East meridian, running south from Cape Agulhas to Antarctica defines its border. In the 1953 definition it extends south to Antarctica, while in later maps it is bounded at the 60° parallel by the Southern Ocean.
The Atlantic has irregular coasts indented by numerous bays, gulfs and seas. These include the Baltic Sea, Black Sea, Caribbean Sea, Davis Strait, Denmark Strait, part of the Drake Passage, Gulf of Mexico, Labrador Sea, Mediterranean Sea, North Sea, Norwegian Sea, almost all of the Scotia Sea, and other tributary water bodies. Including these marginal seas the coast line of the Atlantic measures compared to for the Pacific.
Including its marginal seas, the Atlantic covers an area of or 23.5% of the global ocean and has a volume of or 23.3% of the total volume of the Earth's oceans. Excluding its marginal seas, the Atlantic covers and has a volume of . The North Atlantic covers (11.5%) and the South Atlantic (11.1%). The average depth is and the maximum depth, the Milwaukee Deep in the Puerto Rico Trench, is . |
Atlantic Ocean | Biggest seas in Atlantic Ocean | Biggest seas in Atlantic Ocean
Top large seas:
Sargasso Sea3.5 million km2
Caribbean Sea2.754 million km2
Mediterranean Sea2.510 million km2
Gulf of Guinea2.35 million km2
Gulf of Mexico1.550 million km2
Norwegian Sea1.383 million km2
Greenland Sea1.205 million km2
Argentine Sea1 million km2
Labrador Sea841,000 km2
Irminger Sea780,000 km2
Baffin Bay689,000 km2
North Sea575,000 km2
Black Sea436,000 km2
Baltic Sea377,000 km2
Libyan Sea350,000 km2
Levantine Sea320,000 km2
Celtic Sea300,000 km2
Tyrrhenian Sea275,000 km2
Gulf of Saint Lawrence226,000 km2
Bay of Biscay223,000 km2
Aegean Sea214,000 km2
Ionian Sea169,000 km2
Balearic Sea150,000 km2
Adriatic Sea138,000 km2
Gulf of Bothnia116,300 km2
Sea of Crete95,000 km2
Gulf of Maine93,000 km2
Ligurian Sea80,000 km2
English Channel75,000 km2
James Bay68,300 km2
Bothnian Sea66,000 km2
Gulf of Sidra57,000 km2
Sea of the Hebrides47,000 km2
Irish Sea46,000 km2
Sea of Azov39,000 km2
Bothnian Bay36,800 km2
Gulf of Venezuela17,840 km2
Bay of Campeche16,000 km2
Gulf of Lion15,000 km2
Sea of Marmara11,350 km2
Wadden Sea10,000 km2
Archipelago Sea8,300 km2 |
Atlantic Ocean | Bathymetry | Bathymetry
thumb|False color map of ocean depth in the Atlantic basin
The bathymetry of the Atlantic is dominated by a submarine mountain range called the Mid-Atlantic Ridge (MAR). It runs from 87°N or south of the North Pole to the subantarctic Bouvet Island at 54°S. Expeditions to explore the bathymertry of the Atlantic include the Challenger expedition and the German Meteor expedition; , Columbia University's Lamont–Doherty Earth Observatory and the United States Navy Hydrographic Office conduct research on the ocean. |
Atlantic Ocean | Mid-Atlantic Ridge | Mid-Atlantic Ridge
The MAR divides the Atlantic longitudinally into two halves, in each of which a series of basins are delimited by secondary, transverse ridges. The MAR reaches above along most of its length, but is interrupted by larger transform faults at two places: the Romanche Trench near the Equator and the Gibbs fracture zone at 53°N. The MAR is a barrier for bottom water, but at these two transform faults deep water currents can pass from one side to the other.
The MAR rises above the surrounding ocean floor and its rift valley is the divergent boundary between the North American and Eurasian plates in the North Atlantic and the South American and African plates in the South Atlantic. The MAR produces basaltic volcanoes in Eyjafjallajökull, Iceland, and pillow lava on the ocean floor. The depth of water at the apex of the ridge is less than in most places, while the bottom of the ridge is three times as deep.
The MAR is intersected by two perpendicular ridges: the Azores–Gibraltar transform fault, the boundary between the Nubian and Eurasian plates, intersects the MAR at the Azores triple junction, on either side of the Azores microplate, near the 40°N. A much vaguer, nameless boundary, between the North American and South American plates, intersects the MAR near or just north of the Fifteen-Twenty fracture zone, approximately at 16°N.
In the 1870s, the Challenger expedition discovered parts of what is now known as the Mid-Atlantic Ridge, or:
The remainder of the ridge was discovered in the 1920s by the German Meteor expedition using echo-sounding equipment. The exploration of the MAR in the 1950s led to the general acceptance of seafloor spreading and plate tectonics.
Most of the MAR runs under water but where it reaches the surfaces it has produced volcanic islands. While nine of these have collectively been nominated a World Heritage Site for their geological value, four of them are considered of "Outstanding Universal Value" based on their cultural and natural criteria: Þingvellir, Iceland; Landscape of the Pico Island Vineyard Culture, Portugal; Gough and Inaccessible Islands, United Kingdom; and Brazilian Atlantic Islands: Fernando de Noronha and Atol das Rocas Reserves, Brazil. |
Atlantic Ocean | Ocean floor | Ocean floor
Continental shelves in the Atlantic are wide off Newfoundland, southernmost South America, and northeastern Europe.
In the western Atlantic carbonate platforms dominate large areas, for example, the Blake Plateau and Bermuda Rise.
The Atlantic is surrounded by passive margins except at a few locations where active margins form deep trenches: the Puerto Rico Trench ( maximum depth) in the western Atlantic and South Sandwich Trench () in the South Atlantic. There are numerous submarine canyons off northeastern North America, western Europe, and northwestern Africa. Some of these canyons extend along the continental rises and farther into the abyssal plains as deep-sea channels.
In 1922, a historic moment in cartography and oceanography occurred. The USS Stewart used a Navy Sonic Depth Finder to draw a continuous map across the bed of the Atlantic. This involved little guesswork because the idea of sonar is straightforward with pulses being sent from the vessel, which bounce off the ocean floor, then return to the vessel. The deep ocean floor is thought to be fairly flat with occasional deeps, abyssal plains, trenches, seamounts, basins, plateaus, canyons, and some guyots. Various shelves along the margins of the continents constitute about 11% of the bottom topography with few deep channels cut across the continental rise.
The mean depth between 60°N and 60°S is , or close to the average for the global ocean, with a modal depth between .
In the South Atlantic the Walvis Ridge and Rio Grande Rise form barriers to ocean currents.
The Laurentian Abyss is found off the eastern coast of Canada. |
Atlantic Ocean | Water characteristics | Water characteristics
thumb|upright=1.8|As the Gulf Stream meanders across the North Atlantic from the North American east coast to Western Europe its temperature drops by .|alt=Visualisation of the Gulf Stream stretching from the Gulf of Mexico to Western Europe
Path of the thermohaline circulation. Purple paths represent deep-water currents, while blue paths represent surface currents.|thumb|alt=Map displaying a looping line with arrows indicating that water flows eastward in the far Southern Ocean, angling northeast of Australia, turning sough-after passing Alaska, then crossing the mid-Pacific to flow north of Australia, continuing west below Africa, then turning northwest until reaching eastern Canada, then angling east to southern Europe, then finally turning south just below Greenland and flowing down the Americas' eastern coast, and resuming its flow eastward to complete the circle
Surface water temperatures, which vary with latitude, current systems, and season and reflect the latitudinal distribution of solar energy, range from below to over . Maximum temperatures occur north of the equator, and minimum values are found in the polar regions. In the middle latitudes, the area of maximum temperature variations, values may vary by .
From October to June the surface is usually covered with sea ice in the Labrador Sea, Denmark Strait, and Baltic Sea.
The Coriolis effect circulates North Atlantic water in a clockwise direction, whereas South Atlantic water circulates counter-clockwise. The south tides in the Atlantic Ocean are semi-diurnal; that is, two high tides occur every 24 lunar hours. In latitudes above 40° North some east–west oscillation, known as the North Atlantic oscillation, occurs. |
Atlantic Ocean | Salinity | Salinity
On average, the Atlantic is the saltiest major ocean; surface water salinity in the open ocean ranges from 33 to 37 parts per thousand (3.3–3.7%) by mass and varies with latitude and season. Evaporation, precipitation, river inflow and sea ice melting influence surface salinity values. Although the lowest salinity values are just north of the equator (because of heavy tropical rainfall), in general, the lowest values are in the high latitudes and along coasts where large rivers enter. Maximum salinity values occur at about 25° north and south, in subtropical regions with low rainfall and high evaporation.
The high surface salinity in the Atlantic, on which the Atlantic thermohaline circulation is dependent, is maintained by two processes: the Agulhas Leakage/Rings, which brings salty Indian Ocean waters into the South Atlantic, and the "Atmospheric Bridge", which evaporates subtropical Atlantic waters and exports it to the Pacific. |
Atlantic Ocean | Water masses | Water masses
+ Temperature-salinity characteristics for Atlantic water masses Water mass Temperature Salinity Upper waters () Atlantic SubarcticUpper Water (ASUW) 0.0–4.0 °C 34.0–35.0 Western North AtlanticCentral Water (WNACW) 7.0–20 °C 35.0–36.7 Eastern North AtlanticCentral Water (ENACW) 8.0–18.0 °C 35.2–36.7 South AtlanticCentral Water (SACW) 5.0–18.0 °C 34.3–35.8 Intermediate waters () Western Atlantic SubarcticIntermediate Water (WASIW) 3.0–9.0 °C 34.0–35.1 Eastern Atlantic SubarcticIntermediate Water (EASIW) 3.0–9.0 °C 34.4–35.3 Mediterranean Water (MW) 2.6–11.0 °C 35.0–36.2 Arctic Intermediate Water (AIW) −1.5–3.0 °C 34.7–34.9 Deep and abyssal waters (1,500 m–bottom or 4,900 ft–bottom) North AtlanticDeep Water (NADW) 1.5–4.0 °C 34.8–35.0 Antarctic Bottom Water (AABW) −0.9–1.7 °C 34.6–34.7 Arctic Bottom Water (ABW) −1.8 to −0.5 °C 34.9–34.9
The Atlantic Ocean consists of four major, upper water masses with distinct temperature and salinity. The Atlantic subarctic upper water in the northernmost North Atlantic is the source for subarctic intermediate water and North Atlantic intermediate water. North Atlantic central water can be divided into the eastern and western North Atlantic central water since the western part is strongly affected by the Gulf Stream and therefore the upper layer is closer to underlying fresher subpolar intermediate water. The eastern water is saltier because of its proximity to Mediterranean water. North Atlantic central water flows into South Atlantic central water at 15°N.
There are five intermediate waters: four low-salinity waters formed at subpolar latitudes and one high-salinity formed through evaporation. Arctic intermediate water flows from the north to become the source for North Atlantic deep water, south of the Greenland-Scotland sill. These two intermediate waters have different salinity in the western and eastern basins. The wide range of salinities in the North Atlantic is caused by the asymmetry of the northern subtropical gyre and a large number of contributions from a wide range of sources: Labrador Sea, Norwegian-Greenland Sea, Mediterranean, and South Atlantic Intermediate Water.
The North Atlantic deep water (NADW) is a complex of four water masses, two that form by deep convection in the open oceanclassical and upper Labrador sea waterand two that form from the inflow of dense water across the Greenland-Iceland-Scotland sillDenmark Strait and Iceland-Scotland overflow water. Along its path across Earth the composition of the NADW is affected by other water masses, especially Antarctic bottom water and Mediterranean overflow water.
The NADW is fed by a flow of warm shallow water into the northern North Atlantic which is responsible for the anomalous warm climate in Europe. Changes in the formation of NADW have been linked to global climate changes in the past. Since human-made substances were introduced into the environment, the path of the NADW can be traced throughout its course by measuring tritium and radiocarbon from nuclear weapon tests in the 1960s and CFCs. |
Atlantic Ocean | Gyres | Gyres
The clockwise warm-water North Atlantic Gyre occupies the northern Atlantic, and the counter-clockwise warm-water South Atlantic Gyre appears in the southern Atlantic.
In the North Atlantic, surface circulation is dominated by three inter-connected currents: the Gulf Stream which flows north-east from the North American coast at Cape Hatteras; the North Atlantic Current, a branch of the Gulf Stream which flows northward from the Grand Banks; and the Subpolar Front, an extension of the North Atlantic Current, a wide, vaguely defined region separating the subtropical gyre from the subpolar gyre. This system of currents transports warm water into the North Atlantic, without which temperatures in the North Atlantic and Europe would plunge dramatically.
thumb|In the subpolar gyre of the North Atlantic warm subtropical waters are transformed into colder subpolar and polar waters. In the Labrador Sea this water flows back to the subtropical gyre.
North of the North Atlantic Gyre, the cyclonic North Atlantic Subpolar Gyre plays a key role in climate variability. It is governed by ocean currents from marginal seas and regional topography, rather than being steered by wind, both in the deep ocean and at sea level.
The subpolar gyre forms an important part of the global thermohaline circulation. Its eastern portion includes eddying branches of the North Atlantic Current which transport warm, saline waters from the subtropics to the northeastern Atlantic. There this water is cooled during winter and forms return currents that merge along the eastern continental slope of Greenland where they form an intense (40–50 Sv) current which flows around the continental margins of the Labrador Sea. A third of this water becomes part of the deep portion of the North Atlantic Deep Water (NADW). The NADW, in turn, feeds the meridional overturning circulation (MOC), the northward heat transport of which is threatened by anthropogenic climate change. Large variations in the subpolar gyre on a decade-century scale, associated with the North Atlantic oscillation, are especially pronounced in Labrador Sea Water, the upper layers of the MOC.
The South Atlantic is dominated by the anti-cyclonic southern subtropical gyre. The South Atlantic Central Water originates in this gyre, while Antarctic Intermediate Water originates in the upper layers of the circumpolar region, near the Drake Passage and the Falkland Islands. Both these currents receive some contribution from the Indian Ocean. On the African east coast, the small cyclonic Angola Gyre lies embedded in the large subtropical gyre.
The southern subtropical gyre is partly masked by a wind-induced Ekman layer. The residence time of the gyre is 4.4–8.5 years. North Atlantic Deep Water flows southward below the thermocline of the subtropical gyre. |
Atlantic Ocean | Sargasso Sea | Sargasso Sea
The Sargasso Sea in the western North Atlantic can be defined as the area where two species of Sargassum (S. fluitans and natans) float, an area wide and encircled by the Gulf Stream, North Atlantic Drift, and North Equatorial Current. This population of seaweed probably originated from Tertiary ancestors on the European shores of the former Tethys Ocean and has, if so, maintained itself by vegetative growth, floating in the ocean for millions of years.
Other species endemic to the Sargasso Sea include the sargassum fish, a predator with algae-like appendages which hovers motionless among the Sargassum. Fossils of similar fishes have been found in fossil bays of the former Tethys Ocean, in what is now the Carpathian region, that were similar to the Sargasso Sea. It is possible that the population in the Sargasso Sea migrated to the Atlantic as the Tethys closed at the end of the Miocene around 17 Ma. The origin of the Sargasso fauna and flora remained enigmatic for centuries. The fossils found in the Carpathians in the mid-20th century often called the "quasi-Sargasso assemblage", finally showed that this assemblage originated in the Carpathian Basin from where it migrated over Sicily to the central Atlantic where it evolved into modern species of the Sargasso Sea.
The location of the spawning ground for European eels remained unknown for decades. In the early 19th century it was discovered that the southern Sargasso Sea is the spawning ground for both the European and American eel and that the former migrate more than and the latter . Ocean currents such as the Gulf Stream transport eel larvae from the Sargasso Sea to foraging areas in North America, Europe, and northern Africa. Recent but disputed research suggests that eels possibly use Earth's magnetic field to navigate through the ocean both as larvae and as adults. |
Atlantic Ocean | Climate | Climate
thumb|Waves in the trade winds in the Atlantic Oceanareas of converging winds that move along the same track as the prevailing windcreate instabilities in the atmosphere that may lead to the formation of hurricanes.|alt=Map of Caribbean showing seven approximately parallel westward-pointing arrows that extend from east of the Virgin Islands to Cuba. The southern arrows bend northward just east of the Dominican Republic before straightening out again.
The climate is influenced by the temperatures of the surface waters and water currents as well as winds. Because of the ocean's great capacity to store and release heat, maritime climates are more moderate and have less extreme seasonal variations than inland climates. Precipitation can be approximated from coastal weather data and air temperature from water temperatures.
The oceans are the major source of atmospheric moisture that is obtained through evaporation. Climatic zones vary with latitude; the warmest zones stretch across the Atlantic north of the equator. The coldest zones are in high latitudes, with the coldest regions corresponding to the areas covered by sea ice. Ocean currents influence the climate by transporting warm and cold waters to other regions. The winds that are cooled or warmed when blowing over these currents influence adjacent land areas.
The Gulf Stream and its northern extension towards Europe, the North Atlantic Drift is thought to have at least some influence on climate. For example, the Gulf Stream helps moderate winter temperatures along the coastline of southeastern North America, keeping it warmer in winter along the coast than inland areas. The Gulf Stream also keeps extreme temperatures from occurring on the Florida Peninsula. In the higher latitudes, the North Atlantic Drift, warms the atmosphere over the oceans, keeping the British Isles and northwestern Europe mild and cloudy, and not severely cold in winter, like other locations at the same high latitude. The cold water currents contribute to heavy fog off the coast of eastern Canada (the Grand Banks of Newfoundland area) and Africa's northwestern coast. In general, winds transport moisture and air over land areas. |
Atlantic Ocean | Natural hazards | Natural hazards
thumb|Iceberg A22A in the South Atlantic Ocean
Every winter, the Icelandic Low produces frequent storms. Icebergs are common from early February to the end of July across the shipping lanes near the Grand Banks of Newfoundland. The ice season is longer in the polar regions, but there is little shipping in those areas.
Hurricanes are a hazard in the western parts of the North Atlantic during the summer and autumn. Due to a consistently strong wind shear and a weak Intertropical Convergence Zone, South Atlantic tropical cyclones are rare. |
Atlantic Ocean | Geology and plate tectonics | Geology and plate tectonics
The Atlantic Ocean is underlain mostly by dense mafic oceanic crust made up of basalt and gabbro and overlain by fine clay, silt and siliceous ooze on the abyssal plain. The continental margins and continental shelf mark lower density, but greater thickness felsic continental rock that is often much older than that of the seafloor. The oldest oceanic crust in the Atlantic is up to 145 million years and is situated off the west coast of Africa and the east coast of North America, or on either side of the South Atlantic.
In many places, the continental shelf and continental slope are covered in thick sedimentary layers. For instance, on the North American side of the ocean, large carbonate deposits formed in warm shallow waters such as Florida and the Bahamas, while coarse river outwash sands and silt are common in shallow shelf areas like the Georges Bank. Coarse sand, boulders, and rocks were transported into some areas, such as off the coast of Nova Scotia or the Gulf of Maine during the Pleistocene ice ages. |
Atlantic Ocean | Central Atlantic | Central Atlantic
The break-up of Pangaea began in the central Atlantic, between North America and Northwest Africa, where rift basins opened during the Late Triassic and Early Jurassic. This period also saw the first stages of the uplift of the Atlas Mountains. The exact timing is controversial with estimates ranging from 200 to 170 Ma.
The opening of the Atlantic Ocean coincided with the initial break-up of the supercontinent Pangaea, both of which were initiated by the eruption of the Central Atlantic Magmatic Province (CAMP), one of the most extensive and voluminous large igneous provinces in Earth's history associated with the Triassic–Jurassic extinction event, one of Earth's major extinction events.
Theoliitic dikes, sills, and lava flows from the CAMP eruption at 200 Ma have been found in West Africa, eastern North America, and northern South America. The extent of the volcanism has been estimated to of which covered what is now northern and central Brazil.
The formation of the Central American Isthmus closed the Central American Seaway at the end of the Pliocene 2.8 Ma ago. The formation of the isthmus resulted in the migration and extinction of many land-living animals, known as the Great American Interchange, but the closure of the seaway resulted in a "Great American Schism" as it affected ocean currents, salinity, and temperatures in both the Atlantic and Pacific. Marine organisms on both sides of the isthmus became isolated and either diverged or went extinct. |
Atlantic Ocean | North Atlantic | North Atlantic
Geologically, the North Atlantic is the area delimited to the south by two conjugate margins, Newfoundland and Iberia, and to the north by the Arctic Eurasian Basin. The opening of the North Atlantic closely followed the margins of its predecessor, the Iapetus Ocean, and spread from the central Atlantic in six stages: Iberia–Newfoundland, Porcupine–North America, Eurasia–Greenland, Eurasia–North America. Active and inactive spreading systems in this area are marked by the interaction with the Iceland hotspot.
Seafloor spreading led to the extension of the crust and the formation of troughs and sedimentary basins. The Rockall Trough opened between 105 and 84 million years ago although the rift failed along with one leading into the Bay of Biscay.
Spreading began opening the Labrador Sea around 61 million years ago, continuing until 36 million years ago. Geologists distinguish two magmatic phases. One from 62 to 58 million years ago predates the separation of Greenland from northern Europe while the second from 56 to 52 million years ago happened as the separation occurred.
Iceland began to form 62 million years ago due to a particularly concentrated mantle plume. Large quantities of basalt erupted at this time period are found on Baffin Island, Greenland, the Faroe Islands, and Scotland, with ash falls in Western Europe acting as a stratigraphic marker. The opening of the North Atlantic caused a significant uplift of continental crust along the coast. For instance, despite 7 km thick basalt, Gunnbjorn Field in East Greenland is the highest point on the island, elevated enough that it exposes older Mesozoic sedimentary rocks at its base, similar to old lava fields above sedimentary rocks in the uplifted Hebrides of western Scotland.
The North Atlantic Ocean contains about 810 seamounts, most of them situated along the Mid-Atlantic Ridge.Gubbay S. 2003. Seamounts of the northeast Atlantic. OASIS (Oceanic Seamounts: an Integrated Study). Hamburg & WWF, Frankfurt am Main, Germany The OSPAR database (Convention for the Protection of the Marine Environment of the North-East Atlantic) mentions 104 seamounts: 74 within national exclusive economic zones. Of these seamounts, 46 are located close to the Iberian Peninsula. |
Atlantic Ocean | South Atlantic | South Atlantic
West Gondwana (South America and Africa) broke up in the Early Cretaceous to form the South Atlantic. The apparent fit between the coastlines of the two continents was noted on the first maps that included the South Atlantic and it was also the subject of the first computer-assisted plate tectonic reconstructions in 1965. This magnificent fit, however, has since then proven problematic and later reconstructions have introduced various deformation zones along the shorelines to accommodate the northward-propagating break-up. Intra-continental rifts and deformations have also been introduced to subdivide both continental plates into sub-plates.
Geologically, the South Atlantic can be divided into four segments: equatorial segment, from 10°N to the Romanche fracture zone (RFZ); central segment, from RFZ to Florianopolis fracture zone (FFZ, north of Walvis Ridge and Rio Grande Rise); southern segment, from FFZ to the Agulhas–Falkland fracture zone (AFFZ); and Falkland segment, south of AFFZ.
In the southern segment the Early Cretaceous (133–130 Ma) intensive magmatism of the Paraná–Etendeka Large Igneous Province produced by the Tristan hotspot resulted in an estimated volume of . It covered an area of in Brazil, Paraguay, and Uruguay and in Africa. Dyke swarms in Brazil, Angola, eastern Paraguay, and Namibia, however, suggest the LIP originally covered a much larger area and also indicate failed rifts in all these areas. Associated offshore basaltic flows reach as far south as the Falkland Islands and South Africa. Traces of magmatism in both offshore and onshore basins in the central and southern segments have been dated to 147–49 Ma with two peaks between 143 and 121 Ma and 90–60 Ma.
In the Falkland segment rifting began with dextral movements between the Patagonia and Colorado sub-plates between the Early Jurassic (190 Ma) and the Early Cretaceous (126.7 Ma). Around 150 Ma sea-floor spreading propagated northward into the southern segment. No later than 130 Ma rifting had reached the Walvis Ridge–Rio Grande Rise.
In the central segment, rifting started to break Africa in two by opening the Benue Trough around 118 Ma. Rifting in the central segment, however, coincided with the Cretaceous Normal Superchron (also known as the Cretaceous quiet period), a 40 Ma period without magnetic reversals, which makes it difficult to date sea-floor spreading in this segment.
The equatorial segment is the last phase of the break-up, but, because it is located on the Equator, magnetic anomalies cannot be used for dating. Various estimates date the propagation of seafloor spreading in this segment and consequent opening of the Equatorial Atlantic Gateway (EAG) to the period 120–96 Ma. This final stage, nevertheless, coincided with or resulted in the end of continental extension in Africa.
About 50 Ma the opening of the Drake Passage resulted from a change in the motions and separation rate of the South American and Antarctic plates. First, small ocean basins opened and a shallow gateway appeared during the Middle Eocene. 34–30 Ma a deeper seaway developed, followed by an Eocene–Oligocene climatic deterioration and the growth of the Antarctic ice sheet. |
Atlantic Ocean | Closure of the Atlantic | Closure of the Atlantic
An embryonic subduction margin is potentially developing west of Gibraltar. The Gibraltar Arc in the western Mediterranean is migrating westward into the central Atlantic where it joins the converging African and Eurasian plates. Together these three tectonic forces are slowly developing into a new subduction system in the eastern Atlantic Basin. Meanwhile, the Scotia Arc and Caribbean plate in the western Atlantic Basin are eastward-propagating subduction systems that might, together with the Gibraltar system, represent the beginning of the closure of the Atlantic Ocean and the final stage of the Atlantic Wilson cycle. |
Atlantic Ocean | History | History |
Atlantic Ocean | Old World | Old World
Mitochondrial DNA (mtDNA) studies indicate that 80–60,000 years ago a major demographic expansion within Africa, derived from a single, small population, coincided with the emergence of behavioral complexity and the rapid MIS 5–4 environmental changes. This group of people not only expanded over the whole of Africa, but also started to disperse out of Africa into Asia, Europe, and Australasia around 65,000 years ago and quickly replaced the archaic humans in these regions. During the Last Glacial Maximum (LGM) 20,000 years ago humans had to abandon their initial settlements along the European North Atlantic coast and retreat to the Mediterranean. Following rapid climate changes at the end of the LGM this region was repopulated by Magdalenian culture. Other hunter-gatherers followed in waves interrupted by large-scale hazards such as the Laacher See volcanic eruption, the inundation of Doggerland (now the North Sea), and the formation of the Baltic Sea. The European coasts of the North Atlantic were permanently populated about 9–8.5 thousand years ago.
This human dispersal left abundant traces along the coasts of the Atlantic Ocean. 50 kya-old, deeply stratified shell middens found in Ysterfontein on the western coast of South Africa are associated with the Middle Stone Age (MSA). The MSA population was small and dispersed and the rate of their reproduction and exploitation was less intense than those of later generations. While their middens resemble 12–11 kya-old Late Stone Age (LSA) middens found on every inhabited continent, the 50–45 kya-old Enkapune Ya Muto in Kenya probably represents the oldest traces of the first modern humans to disperse out of Africa.
thumb|Excavation of the Ertebølle middens in 1880
The same development can be seen in Europe. In La Riera Cave (23–13 kya) in Asturias, Spain, only some 26,600 molluscs were deposited over 10 kya. In contrast, 8–7 kya-old shell middens in Portugal, Denmark, and Brazil generated thousands of tons of debris and artefacts. The Ertebølle middens in Denmark, for example, accumulated of shell deposits representing some 50 million molluscs over only a thousand years. This intensification in the exploitation of marine resources has been described as accompanied by new technologiessuch as boats, harpoons, and fish hooks because many caves found in the Mediterranean and on the European Atlantic coast have increased quantities of marine shells in their upper levels and reduced quantities in their lower. The earliest exploitation, however, took place on the now submerged shelves, and most settlements now excavated were then located several kilometers from these shelves. The reduced quantities of shells in the lower levels can represent the few shells that were exported inland. |
Atlantic Ocean | New World | New World
During the LGM the Laurentide Ice Sheet covered most of northern North America while Beringia connected Siberia to Alaska. In 1973, late American geoscientist Paul S. Martin proposed a "blitzkrieg" colonization of the Americas by which Clovis hunters migrated into North America around 13,000 years ago in a single wave through an ice-free corridor in the ice sheet and "spread southward explosively, briefly attaining a density sufficiently large to overkill much of their prey." Others later proposed a "three-wave" migration over the Bering Land Bridge. These hypotheses remained the long-held view regarding the settlement of the Americas, a view challenged by more recent archaeological discoveries: the oldest archaeological sites in the Americas have been found in South America; sites in northeast Siberia report virtually no human presence there during the LGM; and most Clovis artefacts have been found in eastern North America along the Atlantic coast. Furthermore, colonisation models based on mtDNA, yDNA, and atDNA data respectively support neither the "blitzkrieg" nor the "three-wave" hypotheses but they also deliver mutually ambiguous results. Contradictory data from archaeology and genetics will most likely deliver future hypotheses that will, eventually, confirm each other. A proposed route across the Pacific to South America could explain early South American finds and another hypothesis proposes a northern path, through the Canadian Arctic and down the North American Atlantic coast.
Early settlements across the Atlantic have been suggested by alternative theories, ranging from purely hypothetical to mostly disputed, including the Solutrean hypothesis and some of the Pre-Columbian trans-oceanic contact theories.
thumb|Based on the medieval sagas, including the Grœnlendinga saga, this interpretative map of the "Norse World" shows that Norse knowledge of the Americas and the Atlantic remained limited.
The Norse settlement of the Faroe Islands and Iceland began during the 9th and 10th centuries. A settlement on Greenland was established before 1000 CE, but contact with it was lost in 1409 and it was finally abandoned during the early Little Ice Age. This setback was caused by a range of factors: an unsustainable economy resulted in erosion and denudation, while conflicts with the local Inuit resulted in the failure to adapt their Arctic technologies; a colder climate resulted in starvation, and the colony got economically marginalized as the Great Plague harvested its victims on Iceland in the 15th century.
Iceland was initially settled 865–930 CE following a warm period when winter temperatures hovered around which made farming favorable at high latitudes. This did not last, however, and temperatures quickly dropped; at 1080 CE summer temperatures had reached a maximum of . The (Book of Settlement) records disastrous famines during the first century of settlement"men ate foxes and ravens" and "the old and helpless were killed and thrown over cliffs"and by the early 1200s hay had to be abandoned for short-season crops such as barley. |
Atlantic Ocean | Atlantic World | Atlantic World
thumb|left|The Atlantic Gyres influenced the Portuguese discoveries and trading port routes, here shown in the India Run ("Carreira da Índia"), which would be developed in subsequent years.
Christopher Columbus reached the Americas in 1492, sailing under the Spanish flag. Six years later Vasco da Gama reached India under the Portuguese flag, by navigating south around the Cape of Good Hope, thus proving that the Atlantic and Indian Oceans are connected. In 1500, in his voyage to India following Vasco da Gama, Pedro Álvares Cabral reached Brazil, taken by the currents of the South Atlantic Gyre. Following these explorations, Spain and Portugal quickly conquered and colonized large territories in the New World and forced the Amerindian population into slavery in order to exploit the vast quantities of silver and gold they found. Spain and Portugal monopolized this trade in order to keep other European nations out, but conflicting interests nevertheless led to a series of Spanish-Portuguese wars. A peace treaty mediated by the Pope divided the conquered territories into Spanish and Portuguese sectors while keeping other colonial powers away. England, France, and the Dutch Republic enviously watched the Spanish and Portuguese wealth grow and allied themselves with pirates such as Henry Mainwaring and Alexandre Exquemelin. They could explore the convoys leaving the Americas because prevailing winds and currents made the transport of heavy metals slow and predictable.
thumb|Embarked and disembarked slaves in the Atlantic slave trade 1525–1863 (first and last slave voyages)
In the colonies of the Americas, depredation, smallpox and other diseases, and slavery quickly reduced the indigenous population of the Americas to the extent that the Atlantic slave trade was introduced by colonists to replace thema trade that became the norm and an integral part of the colonization. Between the 15th century and 1888, when Brazil became the last part of the Americas to end the slave trade, an estimated 9.5 million enslaved Africans were shipped into the New World, most of them destined for agricultural labor. The slave trade was officially abolished in the British Empire and the United States in 1808, and slavery itself was abolished in the British Empire in 1838 and in the United States in 1865 after the Civil War.
From Columbus to the Industrial Revolution trans-Atlantic trade, including colonialism and slavery, became crucial for Western Europe. For European countries with direct access to the Atlantic (including Britain, France, the Netherlands, Portugal, and Spain) 1500–1800 was a period of sustained growth during which these countries grew richer than those in Eastern Europe and Asia. Colonialism evolved as part of the trans-Atlantic trade, but this trade also strengthened the position of merchant groups at the expense of monarchs. Growth was more rapid in non-absolutist countries, such as Britain and the Netherlands, and more limited in absolutist monarchies, such as Portugal, Spain, and France, where profit mostly or exclusively benefited the monarchy and its allies.
Trans-Atlantic trade also resulted in increasing urbanization: in European countries facing the Atlantic, urbanization grew from 8% in 1300, 10.1% in 1500, to 24.5% in 1850; in other European countries from 10% in 1300, 11.4% in 1500, to 17% in 1850. Likewise, GDP doubled in Atlantic countries but rose by only 30% in the rest of Europe. By the end of the 17th century, the volume of the Trans-Atlantic trade had surpassed that of the Mediterranean trade. |
Atlantic Ocean | Economy | Economy
The Atlantic has contributed significantly to the development and economy of surrounding countries. Besides major transatlantic transportation and communication routes, the Atlantic offers abundant petroleum deposits in the sedimentary rocks of the continental shelves.
thumb|right|Cod fishery in Norway
The Atlantic harbors petroleum and gas fields, fish, marine mammals (seals and whales), sand and gravel aggregates, placer deposits, polymetallic nodules, and precious stones.
Gold deposits are a mile or two underwater on the ocean floor, however, the deposits are also encased in rock that must be mined through. Currently, there is no cost-effective way to mine or extract gold from the ocean to make a profit.
Various international treaties attempt to reduce pollution caused by environmental threats such as oil spills, marine debris, and the incineration of toxic wastes at sea. |
Atlantic Ocean | Fisheries | Fisheries
The shelves of the Atlantic hosts one of the world's richest fishing resources. The most productive areas include the Grand Banks of Newfoundland, the Scotian Shelf, Georges Bank off Cape Cod, the Bahama Banks, the waters around Iceland, the Irish Sea, the Bay of Fundy, the Dogger Bank of the North Sea, and the Falkland Banks.
Fisheries have, however, undergone significant changes since the 1950s and global catches can now be divided into three groups of which only two are observed in the Atlantic: fisheries in the eastern-central and southwest Atlantic oscillate around a globally stable value, the rest of the Atlantic is in overall decline following historical peaks. The third group, "continuously increasing trend since 1950", is only found in the Indian Ocean and western Pacific.
UN FAO partitioned the Atlantic into major fishing areas:
thumb|Banks of the northeast Atlantic
Northeast Atlantic
Northeast Atlantic is schematically limited to the 40°00' west longitude (except around Greenland), south to the 36°00' north latitude, and to the 68°30' east longitude, with both the west and east longitude limits reaching to the north pole. The Atlantic's subareas include: Barents Sea; Norwegian Sea, Spitzbergen, and Bear Island; Skagerrak, Kattegat, Sound, Belt Sea, and Baltic Sea; North Sea; Iceland and Faroes Grounds; Rockall, Northwest Coast of Scotland, and North Ireland; Irish Sea, West of Ireland, Porcupine Bank, and eastern and western English Channel; Bay of Biscay; Portuguese Waters; Azores Grounds and Northeast Atlantic South; North of Azores; and East Greenland. There are also two defunct subareas.
In the Northeast Atlantic total catches decreased between the mid-1970s and the 1990s and reached 8.7 million tons in 2013. Blue whiting reached a 2.4 million tons peak in 2004 but was down to 628,000 tons in 2013. Recovery plans for cod, sole, and plaice have reduced mortality in these species. Arctic cod reached its lowest levels in the 1960s–1980s but is now recovered. Arctic saithe and haddock are considered fully fished; Sand eel is overfished as was capelin which has now recovered to fully fished. Limited data makes the state of redfishes and deep-water species difficult to assess but most likely they remain vulnerable to overfishing. Stocks of northern shrimp and Norwegian lobster are in good condition. In the Northeast Atlantic, 21% of stocks are considered overfished.
This zone makes almost three-quarters (72.8%) of European Union fishing catches in 2020. Main fishing EU countries are Denmark, France, the Netherlands and Spain. Most common species include herring, mackerel, and sprats.
thumb|Banks of the northwest Atlantic
Northwest Atlantic In the Northwest Atlantic landings have decreased from 4.2 million tons in the early 1970s to 1.9 million tons in 2013. During the 21st century, some species have shown weak signs of recovery, including Greenland halibut, yellowtail flounder, Atlantic halibut, haddock, spiny dogfish, while other stocks shown no such signs, including cod, witch flounder, and redfish. Stocks of invertebrates, in contrast, remain at record levels of abundance. 31% of stocks are overfished in the northwest Atlantic.
thumb|left|Capture of Atlantic northwest cod in million tons
In 1497, John Cabot became the first Western European since the Vikings to explore mainland North America and one of his major discoveries was the abundant resources of Atlantic cod off Newfoundland. Referred to as "Newfoundland Currency" this discovery yielded some 200 million tons of fish over five centuries. In the late 19th and early 20th centuries, new fisheries started to exploit haddock, mackerel, and lobster. From the 1950s to the 1970s, the introduction of European and Asian distant-water fleets in the area dramatically increased the fishing capacity and the number of exploited species. It also expanded the exploited areas from near-shore to the open sea and to great depths to include deep-water species such as redfish, Greenland halibut, witch flounder, and grenadiers. Overfishing in the area was recognized as early as the 1960s but, because this was occurring on international waters, it took until the late 1970s before any attempts to regulate was made. In the early 1990s, this finally resulted in the collapse of the Atlantic northwest cod fishery. The population of a number of deep-sea fishes also collapsed in the process, including American plaice, redfish, and Greenland halibut, together with flounder and grenadier.
Eastern central-Atlantic In the eastern central-Atlantic small pelagic fishes constitute about 50% of landings with sardine reaching 0.6–1.0 million tons per year. Pelagic fish stocks are considered fully fished or overfished, with sardines south of Cape Bojador the notable exception. Almost half of the stocks are fished at biologically unsustainable levels. Total catches have been fluctuating since the 1970s; reaching 3.9 million tons in 2013 or slightly less than the peak production in 2010.
thumb|upright|Bahama Banks
Western central-Atlantic In the western central-Atlantic, catches have been decreasing since 2000 and reached 1.3 million tons in 2013. The most important species in the area, Gulf menhaden, reached a million tons in the mid-1980s but only half a million tons in 2013 and is now considered fully fished. Round sardinella was an important species in the 1990s but is now considered overfished. Groupers and snappers are overfished and northern brown shrimp and American cupped oyster are considered fully fished approaching overfished. 44% of stocks are being fished at unsustainable levels.
thumb|left|Agulhas Bank
Southeast Atlantic In the southeast Atlantic catches have decreased from 3.3 million tons in the early 1970s to 1.3 million tons in 2013. Horse mackerel and hake are the most important species, together representing almost half of the landings. Off South Africa and Namibia deep-water hake and shallow-water Cape hake have recovered to sustainable levels since regulations were introduced in 2006 and the states of southern African pilchard and anchovy have improved to fully fished in 2013.
Southwest Atlantic In the southwest Atlantic, a peak was reached in the mid-1980s and catches now fluctuate between 1.7 and 2.6 million tons. The most important species, the Argentine shortfin squid, which reached half a million tons in 2013 or half the peak value, is considered fully fished to overfished. Another important species was the Brazilian sardinella, with a production of 100,000 tons in 2013 it is now considered overfished. Half the stocks in this area are being fished at unsustainable levels: Whitehead's round herring has not yet reached fully fished but Cunene horse mackerel is overfished. The sea snail perlemoen abalone is targeted by illegal fishing and remains overfished. |
Atlantic Ocean | Environmental issues | Environmental issues |
Atlantic Ocean | Endangered species | Endangered species
Endangered marine species include the manatee, seals, sea lions, turtles, and whales. Drift net fishing can kill dolphins, albatrosses and other seabirds (petrels, auks), hastening the fish stock decline and contributing to international disputes. |
Atlantic Ocean | Waste and pollution | Waste and pollution
Marine pollution is a generic term for the entry into the ocean of potentially hazardous chemicals or particles. The biggest culprits are rivers and with them many agriculture fertilizer chemicals as well as livestock and human waste. The excess of oxygen-depleting chemicals leads to hypoxia and the creation of a dead zone.Sebastian A. Gerlach "Marine Pollution", Springer, Berlin (1975)
thumb|Marine debris strewn over the beaches of the South Atlantic Inaccessible Island
Marine debris, which is also known as marine litter, describes human-created waste floating in a body of water. Oceanic debris tends to accumulate at the center of gyres and coastlines, frequently washing aground where it is known as beach litter. The North Atlantic garbage patch is estimated to be hundreds of kilometers across in size.
Other pollution concerns include agricultural and municipal waste. Municipal pollution comes from the eastern United States, southern Brazil, and eastern Argentina; oil pollution in the Caribbean Sea, Gulf of Mexico, Lake Maracaibo, Mediterranean Sea, and North Sea; and industrial waste and municipal sewage pollution in the Baltic Sea, North Sea, and Mediterranean Sea.
A USAF C-124 aircraft from Dover Air Force Base, Delaware was carrying three nuclear bombs over the Atlantic Ocean when it experienced a loss of power. For their own safety, the crew jettisoned two nuclear bombs, which were never recovered. |
Atlantic Ocean | Climate change | Climate change
North Atlantic hurricane activity has increased over past decades because of increased sea surface temperature (SST) at tropical latitudes, changes that can be attributed to either the natural Atlantic Multidecadal Oscillation (AMO) or to anthropogenic climate change.
A 2005 report indicated that the Atlantic meridional overturning circulation (AMOC) slowed down by 30% between 1957 and 2004. In 2024, the research highlighted a significant weakening of the AMOC by approximately 12% over the past two decades. If the AMO were responsible for SST variability, the AMOC would have increased in strength, which is apparently not the case. Furthermore, it is clear from statistical analyses of annual tropical cyclones that these changes do not display multidecadal cyclicity. Therefore, these changes in SST must be caused by human activities.
The ocean mixed layer plays an important role in heat storage over seasonal and decadal time scales, whereas deeper layers are affected over millennia and have a heat capacity about 50 times that of the mixed layer. This heat uptake provides a time-lag for climate change but it also results in thermal expansion of the oceans which contributes to sea level rise. 21st-century global warming will probably result in an equilibrium sea-level rise five times greater than today, whilst melting of glaciers, including that of the Greenland ice sheet, expected to have virtually no effect during the 21st century, will likely result in a sea-level rise of over a millennium. |
Atlantic Ocean | Theories of natural delimitation between the Atlantic and Pacific oceans | Theories of natural delimitation between the Atlantic and Pacific oceans
thumb|300px|right|Map showing the proposal presented by the thesis entitled "Natural delimitation between the Pacific and South Atlantic oceans by the Shackleton Fracture Zone"
Scientific researchers have proposed delimiting the boundary between the Atlantic and Pacific oceans by two different natural boundaries, by the Shackleton fracture zone and by the Scotia Arc the former being more current than the latter. |
Atlantic Ocean | See also | See also
Atlantic Revolutions
List of countries and territories bordering the Atlantic Ocean
Seven Seas
Shipwrecks in the Atlantic Ocean
Atlantic hurricanes
Piracy in the Atlantic World
Transatlantic crossing
South Atlantic Peace and Cooperation Zone
Natural delimitation between the Pacific and South Atlantic oceans by the Scotia Arc |
Atlantic Ocean | References | References |
Atlantic Ocean | Sources | Sources
map
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Atlantic Ocean | Further reading | Further reading
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Atlantic Ocean | External links | External links
Atlantic Ocean. Cartage.org.lb (archived)
"Map of Atlantic Coast of North America from the Chesapeake Bay to Florida" from 1639 via the Library of Congress
Category:Oceans
Category:Articles containing video clips
Category:Oceans surrounding Antarctica |
Atlantic Ocean | Table of Content | Short description, Toponymy, Extent and data, Biggest seas in Atlantic Ocean, Bathymetry, Mid-Atlantic Ridge, Ocean floor, Water characteristics, Salinity, Water masses, Gyres, Sargasso Sea, Climate, Natural hazards, Geology and plate tectonics, Central Atlantic, North Atlantic, South Atlantic, Closure of the Atlantic, History, Old World, New World, Atlantic World, Economy, Fisheries, Environmental issues, Endangered species, Waste and pollution, Climate change, Theories of natural delimitation between the Atlantic and Pacific oceans, See also, References, Sources, Further reading, External links |
Arthur Schopenhauer | Short description | Arthur Schopenhauer ( ; ; 22 February 1788 – 21 September 1860) was a German philosopher. He is known for his 1818 work The World as Will and Representation (expanded in 1844), which characterizes the phenomenal world as the manifestation of a blind and irrational noumenal will. Building on the transcendental idealism of Immanuel Kant, Schopenhauer developed an atheistic metaphysical and ethical system that rejected the contemporaneous ideas of German idealism.
Schopenhauer was among the first philosophers in the Western tradition to share and affirm significant tenets of Indian philosophy, such as asceticism, denial of the self, and the notion of the world-as-appearance.See the book-length study about oriental influences on the genesis of Schopenhauer's philosophy by Urs App: Schopenhauer's Compass. An Introduction to Schopenhauer's Philosophy and its Origins. Wil: UniversityMedia, 2014 ()
His work has been described as an exemplary manifestation of philosophical pessimism. Studies in Pessimism – audiobook from LibriVox.
Though his work failed to garner substantial attention during his lifetime, he had a posthumous impact across various disciplines, including philosophy, literature, and science. His writing on aesthetics, morality, and psychology has influenced many thinkers and artists. |
Arthur Schopenhauer | Early life | Early life
thumb|upright|Schopenhauer's birthplace house, Świętego Ducha street
Arthur Schopenhauer was born on 22 February 1788 in Gdańsk (then part of the Polish–Lithuanian Commonwealth; later in the Kingdom of Prussia Danzig) on Św. Ducha 47 (in Prussia Heiliggeistgasse), the son of and his wife Johanna Schopenhauer (née Trosiener), both descendants of wealthy German patrician families. While they came from a Protestant background, neither of them was very religious; both supported the French Revolution, were republicans, cosmopolitans, and Anglophiles. When Gdańsk became part of Prussia in 1793, Heinrich moved to Hamburg—a free city with a republican constitution. His firm continued trading in Danzig, where most of their extended families remained. Adele, Arthur's only sibling, was born on 12 July 1797.
In 1797, Arthur was sent to Le Havre to live with the family of his father's business associate, Grégoire de Blésimaire. He seemed to enjoy his two-year stay there, learning to speak French and fostering a life-long friendship with Jean Anthime Grégoire de Blésimaire. As early as 1799, Arthur started playing the flute.
In 1803, he accompanied his parents on a European tour of Holland, Britain, France, Switzerland, Austria, and Prussia. Viewed as primarily a pleasure tour, Heinrich used the opportunity to visit some of his business associates abroad.
Heinrich presented Arthur with a choice: he could either stay at home to begin preparations for university or travel with them to further his merchant education. Arthur chose to travel with them. He deeply regretted his choice later because the merchant training was very tedious. He spent twelve weeks of the tour attending school in Wimbledon, where he was confused by strict and intellectual Anglicans, who he described as shallow. He continued to sharply criticize Anglican religiosity later in life despite his general Anglophilia. He was also under pressure from his father, who became very critical of his educational results.
In 1805, Heinrich drowned in a canal near their home in Hamburg. Although it was possible that his death was accidental, his wife and son believed that it was suicide. He was prone to anxiety and depression, each becoming more pronounced later in his life.Safranski (1990), p. 12 Heinrich had become so fussy that even his wife started to doubt his mental health. "There was, in the father's life, some dark and vague source of fear which later made him hurl himself to his death from the attic of his house in Hamburg."
Arthur showed similar moodiness during his youth and often acknowledged that he inherited it from his father. There were other instances of serious mental health problems on his father's side of the family. Despite his hardship, Schopenhauer liked his father and later referred to him in a positive light. Heinrich Schopenhauer left the family with a significant inheritance split in three among Johanna and the children. Arthur Schopenhauer was entitled to control of his part when he reached the age of majority. He invested it conservatively in government bonds and earned annual interest that was more than double the salary of a university professor. After quitting his merchant apprenticeship, with encouragement from his mother, he dedicated himself to studies at the Ernestine Gymnasium, Gotha, in Saxe-Gotha-Altenburg. While there, he also enjoyed a social life among the local nobility, spending large amounts of money, which deeply concerned his frugal mother. He left the Gymnasium after writing a satirical poem about one of the schoolmasters. Although Arthur claimed he left voluntarily, his mother's letter indicates that he may have been expelled.
thumb|left|Schopenhauer in his youth
Arthur spent two years as a merchant in honor of his dead father. During this time, he had doubts about being able to start a new life as a scholar. Most of his prior education was as a practical merchant and he had trouble learning Latin; a prerequisite for an academic career.
His mother moved away, with her daughter Adele, to Weimar—then the centre of German literature—to enjoy social life among writers and artists. Arthur and his mother did not part on good terms. In one letter, she wrote: "You are unbearable and burdensome, and very hard to live with; all your good qualities are overshadowed by your conceit, and made useless to the world simply because you cannot restrain your propensity to pick holes in other people." His mother, Johanna, was generally described as vivacious and sociable. She died 24 years later. Some of Arthur's negative opinions about women may be rooted in his troubled relationship with his mother.Durant, Will, The Story of Philosophy, Garden City Publishing Co., Inc., New York, p. 350
Arthur moved to Hamburg to live with his friend Jean Anthime, who was also studying to become a merchant. |
Arthur Schopenhauer | Education | Education
He moved to Weimar but did not live with his mother, who even tried to discourage him from coming by explaining that they would not get along very well. Their relationship deteriorated even further due to their temperamental differences. He accused his mother of being financially irresponsible, flirtatious and seeking to remarry, which he considered an insult to his father's memory. His mother, while professing her love to him, criticized him sharply for being moody, tactless, and argumentative, and urged him to improve his behavior so that he would not alienate people. Arthur concentrated on his studies, which were now going very well, and he also enjoyed the usual social life such as balls, parties and theater. By that time Johanna's famous salon was well established among local intellectuals and dignitaries, the most celebrated of them being Goethe. Arthur attended her parties, usually when he knew that Goethe would be there—although the famous writer and statesman seemed not even to notice the young and unknown student. It is possible that Goethe kept a distance because Johanna warned him about her son's depressive and combative nature, or because Goethe was then on bad terms with Arthur's language instructor and roommate, Franz Passow. Schopenhauer was also captivated by the beautiful Karoline Jagemann, mistress of Karl August, Grand Duke of Saxe-Weimar-Eisenach, and he wrote to her his only known love poem. Despite his later celebration of asceticism and negative views of sexuality, Schopenhauer occasionally had sexual affairs—usually with women of lower social status, such as servants, actresses, and sometimes even paid prostitutes. In a letter to his friend Anthime he claims that such affairs continued even in his mature age and admits that he had two out-of-wedlock daughters (born in 1819 and 1836), both of whom died in infancy. In their youthful correspondence Arthur and Anthime were somewhat boastful and competitive about their sexual exploits—but Schopenhauer seemed aware that women usually did not find him very charming or physically attractive, and his desires often remained unfulfilled.
He left Weimar to become a student at the University of Göttingen in 1809. There are no written reasons about why Schopenhauer chose that university instead of the then more famous University of Jena, but Göttingen was known as more modern and scientifically oriented, with less attention given to theology. Law or medicine were usual choices for young men of Schopenhauer's status who also needed career and income; he chose medicine due to his scientific interests. Among his notable professors were Bernhard Friedrich Thibaut, Arnold Hermann Ludwig Heeren, Johann Friedrich Blumenbach, Friedrich Stromeyer, Heinrich Adolf Schrader, Johann Tobias Mayer and Konrad Johann Martin Langenbeck. He studied metaphysics, psychology and logic under Gottlob Ernst Schulze, the author of Aenesidemus, who made a strong impression and advised him to concentrate on Plato and Immanuel Kant. He decided to switch from medicine to philosophy around 1810–11 and he left Göttingen, which did not have a strong philosophy program: besides Schulze, the only other philosophy professor was Friedrich Bouterwek, whom Schopenhauer disliked. He did not regret his medicinal and scientific studies; he claimed that they were necessary for a philosopher, and even in Berlin he attended more lectures in sciences than in philosophy. During his days at Göttingen, he spent considerable time studying, but also continued his flute playing and social life. His friends included Friedrich Gotthilf Osann, Karl Witte, Christian Charles Josias von Bunsen, and William Backhouse Astor Sr.
He arrived at the newly founded University of Berlin for the winter semester of 1811–12. At the same time, his mother had just begun her literary career; she published her first book in 1810, a biography of her friend Karl Ludwig Fernow, which was a critical success. Arthur attended lectures by the prominent post-Kantian philosopher Johann Gottlieb Fichte, but quickly found many points of disagreement with his epistemology; he also found Fichte's lectures tedious and hard to understand. He later mentioned Fichte only in critical, negative terms—seeing his philosophy as a lower-quality version of Kant's and considering it useful only because Fichte's poor arguments unintentionally highlighted some failings of Kantianism. He also attended the lectures of the famous Protestant theologian Friedrich Schleiermacher, whom he also quickly came to dislike. His notes and comments on Schleiermacher's lectures show that Schopenhauer was becoming very critical of religion and moving towards atheism. He learned by self-directed reading; besides Plato, Kant and Fichte he also read the works of Schelling, Fries, Jacobi, Bacon, Locke, and much current scientific literature. He attended philological courses by August Böckh and Friedrich August Wolf and continued his naturalistic interests with courses by Martin Heinrich Klaproth, Paul Erman, Johann Elert Bode, Ernst Gottfried Fischer, Johann Horkel, Friedrich Christian Rosenthal and Hinrich Lichtenstein (Lichtenstein was also a friend whom he met at one of his mother's parties in Weimar). |
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