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L_0119 | continental drift | T_1035 | FIGURE 1.2 | image | textbook_images/continental_drift_20681.png |
L_0120 | coriolis effect | T_1036 | FIGURE 1.1 | image | textbook_images/coriolis_effect_20682.png |
L_0121 | correlation using relative ages | T_1039 | FIGURE 1.1 | image | textbook_images/correlation_using_relative_ages_20683.png |
L_0121 | correlation using relative ages | T_1040 | FIGURE 1.2 The white clay is a key bed that marks the Cretaceous-Tertiary Boundary. | image | textbook_images/correlation_using_relative_ages_20684.png |
L_0123 | deep ocean currents | T_1045 | FIGURE 1.1 | image | textbook_images/deep_ocean_currents_20687.png |
L_0123 | deep ocean currents | T_1046 | FIGURE 1.2 | image | textbook_images/deep_ocean_currents_20688.png |
L_0124 | determining relative ages | T_1047 | FIGURE 1.1 | image | textbook_images/determining_relative_ages_20689.png |
L_0127 | distance between stars | T_1054 | FIGURE 1.1 Parallax is used to measure the distance to stars that are relatively nearby. | image | textbook_images/distance_between_stars_20691.png |
L_0128 | distribution of water on earth | T_1056 | FIGURE 1.1 | image | textbook_images/distribution_of_water_on_earth_20692.png |
L_0131 | dwarf planets | T_1064 | FIGURE 1.1 In 1992, Plutos orbit was recognized to be part of the Kuiper belt. With more than 200 million Kuiper belt objects, Pluto has failed the test of clearing other bodies out its orbit. | image | textbook_images/dwarf_planets_20696.png |
L_0131 | dwarf planets | T_1065 | FIGURE 1.2 This composite image compares the size of the dwarf planet Ceres to Earth and the Moon. | image | textbook_images/dwarf_planets_20697.png |
L_0131 | dwarf planets | T_1066 | FIGURE 1.3 | image | textbook_images/dwarf_planets_20698.png |
L_0132 | early atmosphere and oceans | T_1068 | FIGURE 1.1 The gases that create a comets tail can become part of the atmosphere of a planet. | image | textbook_images/early_atmosphere_and_oceans_20699.png |
L_0132 | early atmosphere and oceans | T_1073 | FIGURE 1.2 | image | textbook_images/early_atmosphere_and_oceans_20700.png |
L_0140 | earths core | T_1099 | FIGURE 1.1 An iron meteorite is the closest thing to the Earths core that we can hold in our hands. | image | textbook_images/earths_core_20715.png |
L_0144 | earths magnetic field | T_1115 | FIGURE 1.1 | image | textbook_images/earths_magnetic_field_20720.png |
L_0148 | eclipses | T_1123 | FIGURE 1.1 A solar eclipse, not to scale. | image | textbook_images/eclipses_20727.png |
L_0148 | eclipses | T_1123 | FIGURE 1.2 | image | textbook_images/eclipses_20728.png |
L_0148 | eclipses | T_1124 | FIGURE 1.3 The Moons shadow in a solar eclipse covers a very small area. | image | textbook_images/eclipses_20729.png |
L_0148 | eclipses | T_1124 | FIGURE 1.4 A lunar eclipse. | image | textbook_images/eclipses_20730.png |
L_0150 | effect of latitude on climate | T_1128 | FIGURE 1.1 | image | textbook_images/effect_of_latitude_on_climate_20733.png |
L_0151 | effects of air pollution on human health | T_1131 | FIGURE 1.1 A lung tumor is highlighted in this illustra- tion. | image | textbook_images/effects_of_air_pollution_on_human_health_20734.png |
L_0154 | electromagnetic energy in the atmosphere | T_1139 | FIGURE 1.1 The electromagnetic spectrum; short wavelengths are the fastest with the high- est energy. | image | textbook_images/electromagnetic_energy_in_the_atmosphere_20740.png |
L_0154 | electromagnetic energy in the atmosphere | T_1139 | FIGURE 1.2 A prism breaks apart white light. | image | textbook_images/electromagnetic_energy_in_the_atmosphere_20741.png |
L_0155 | energy conservation | T_1141 | FIGURE 1.1 | image | textbook_images/energy_conservation_20742.png |
L_0155 | energy conservation | T_1142 | FIGURE 1.2 A: One way is to look for this ENERGY STAR logo (Figure 1.3). | image | textbook_images/energy_conservation_20743.png |
L_0155 | energy conservation | T_1142 | FIGURE 1.3 | image | textbook_images/energy_conservation_20744.png |
L_0156 | energy from biomass | T_1143 | FIGURE 1.1 | image | textbook_images/energy_from_biomass_20745.png |
L_0157 | energy use | T_1147 | FIGURE 1.1 | image | textbook_images/energy_use_20746.png |
L_0157 | energy use | T_1147 | FIGURE 1.2 | image | textbook_images/energy_use_20747.png |
L_0158 | environmental impacts of mining | T_1148 | FIGURE 1.1 | image | textbook_images/environmental_impacts_of_mining_20748.png |
L_0161 | exoplanets | T_1158 | FIGURE 1.1 The extrasolar planet Fomalhaut is sur- rounded by a large disk of gas. The disk is not centered on the planet, suggesting that another planet may be pulling on the gas as well. | image | textbook_images/exoplanets_20755.png |
L_0162 | expansion of the universe | T_1160 | FIGURE 1.1 | image | textbook_images/expansion_of_the_universe_20756.png |
L_0162 | expansion of the universe | T_1161 | FIGURE 1.2 | image | textbook_images/expansion_of_the_universe_20757.png |
L_0165 | faults | T_1170 | FIGURE 1.1 Joints in rocks at Joshua Tree National Park, in California. | image | textbook_images/faults_20764.png |
L_0165 | faults | T_1171 | FIGURE 1.2 Faults are easy to recognize as they cut across bedded rocks. | image | textbook_images/faults_20765.png |
L_0165 | faults | T_1172 | FIGURE 1.3 | image | textbook_images/faults_20766.png |
L_0165 | faults | T_1172 | FIGURE 1.4 | image | textbook_images/faults_20767.png |
L_0165 | faults | T_1173 | FIGURE 1.5 | image | textbook_images/faults_20768.png |
L_0167 | flooding | T_1179 | FIGURE 1.1 | image | textbook_images/flooding_20774.png |
L_0167 | flooding | T_1179 | FIGURE 1.2 | image | textbook_images/flooding_20775.png |
L_0167 | flooding | T_1180 | FIGURE 1.3 | image | textbook_images/flooding_20776.png |
L_0167 | flooding | T_1183 | FIGURE 1.4 | image | textbook_images/flooding_20777.png |
L_0169 | folds | T_1187 | FIGURE 1.1 | image | textbook_images/folds_20779.png |
L_0169 | folds | T_1189 | FIGURE 1.2 | image | textbook_images/folds_20780.png |
L_0169 | folds | T_1189 | FIGURE 1.3 | image | textbook_images/folds_20781.png |
L_0169 | folds | T_1189 | FIGURE 1.4 Basins can be enormous. This is a ge- ologic map of the Michigan Basin, which is centered in the state of Michigan but extends into four other states and a Cana- dian province. | image | textbook_images/folds_20782.png |
L_0169 | folds | T_1189 | FIGURE 1.5 | image | textbook_images/folds_20783.png |
L_0170 | formation of earth | T_1193 | FIGURE 1.1 Earths interior: Inner core, outer core, mantle, and crust. | image | textbook_images/formation_of_earth_20784.png |
L_0170 | formation of earth | T_1195 | FIGURE 1.2 The Allende Meteorite is a carbona- ceous chondrite that struck Earth in 1969. The calcium-aluminum-rich inclusions are fragments of the earliest solar system. | image | textbook_images/formation_of_earth_20785.png |
L_0171 | formation of the moon | T_1198 | FIGURE 1.1 | image | textbook_images/formation_of_the_moon_20786.png |
L_0172 | formation of the sun and planets | T_1201 | FIGURE 1.1 | image | textbook_images/formation_of_the_sun_and_planets_20787.png |
L_0173 | fossil fuel formation | T_1202 | FIGURE 1.1 This wetland may look something like an ancient coal-forming swamp. | image | textbook_images/fossil_fuel_formation_20788.png |
L_0173 | fossil fuel formation | T_1202 | FIGURE 1.2 | image | textbook_images/fossil_fuel_formation_20789.png |
L_0174 | fossil fuel reserves | T_1204 | FIGURE 1.1 Worldwide oil reserves. | image | textbook_images/fossil_fuel_reserves_20790.png |
L_0174 | fossil fuel reserves | T_1204 | FIGURE 1.2 | image | textbook_images/fossil_fuel_reserves_20791.png |
L_0175 | fresh water ecosystems | T_1206 | FIGURE 1.1 | image | textbook_images/fresh_water_ecosystems_20792.png |
L_0175 | fresh water ecosystems | T_1208 | FIGURE 1.2 | image | textbook_images/fresh_water_ecosystems_20793.png |
L_0175 | fresh water ecosystems | T_1210 | FIGURE 1.3 A swamp is characterized by trees in still water. | image | textbook_images/fresh_water_ecosystems_20794.png |
L_0176 | galaxies | T_1212 | FIGURE 1.1 | image | textbook_images/galaxies_20795.png |
L_0176 | galaxies | T_1212 | FIGURE 1.2 | image | textbook_images/galaxies_20796.png |
L_0176 | galaxies | T_1213 | FIGURE 1.3 The large, reddish-yellow object in the middle of this figure is a typical elliptical galaxy. What other types of galaxies can you find in the figure? | image | textbook_images/galaxies_20797.png |
L_0176 | galaxies | T_1213 | FIGURE 1.4 Astronomers believe that these dusty el- liptical galaxies form when two galaxies of similar size collide. | image | textbook_images/galaxies_20798.png |
L_0176 | galaxies | T_1214 | FIGURE 1.5 | image | textbook_images/galaxies_20799.png |
L_0177 | geologic time scale | T_1216 | FIGURE 1.1 The geologic time scale is based on rela- tive ages. No actual ages were placed on the original time scale. Click image to the left or use the URL below. URL: https://www.ck12.org/flx/render/embeddedobject/186648 | image | textbook_images/geologic_time_scale_20800.png |
L_0178 | geological stresses | T_1218 | FIGURE 1.1 | image | textbook_images/geological_stresses_20801.png |
L_0178 | geological stresses | T_1218 | FIGURE 1.2 | image | textbook_images/geological_stresses_20802.png |
L_0178 | geological stresses | T_1219 | FIGURE 1.3 With increasing stress, the rock under- goes: (1) elastic deformation, (2) plastic deformation, and (3) fracture. | image | textbook_images/geological_stresses_20803.png |
L_0179 | geothermal power | T_1220 | FIGURE 1.1 A geothermal energy plant in Iceland. Ice- land gets about one fourth of its electricity from geothermal sources. | image | textbook_images/geothermal_power_20804.png |
L_0180 | glaciers | T_1222 | FIGURE 1.1 | image | textbook_images/glaciers_20805.png |
L_0180 | glaciers | T_1225 | FIGURE 1.2 | image | textbook_images/glaciers_20806.png |
L_0180 | glaciers | T_1227 | FIGURE 1.3 | image | textbook_images/glaciers_20807.png |
L_0181 | global warming | T_1230 | FIGURE 1.1 Recent temperature increases show how much temperature has risen since the Industrial Revolution began. | image | textbook_images/global_warming_20808.png |
L_0181 | global warming | T_1232 | FIGURE 1.2 | image | textbook_images/global_warming_20809.png |
L_0181 | global warming | T_1232 | FIGURE 1.3 | image | textbook_images/global_warming_20810.png |
L_0181 | global warming | T_1232 | FIGURE 1.4 | image | textbook_images/global_warming_20811.png |
L_0183 | gravity in the solar system | T_1238 | FIGURE 1.1 | image | textbook_images/gravity_in_the_solar_system_20814.png |
L_0184 | greenhouse effect | T_1240 | FIGURE 1.1 The Earths heat budget shows the amount of energy coming into and going out of the Earths system and the im- portance of the greenhouse effect. The numbers are the amount of energy that is found in one square meter of that location. | image | textbook_images/greenhouse_effect_20815.png |
L_0185 | groundwater aquifers | T_1242 | FIGURE 1.1 | image | textbook_images/groundwater_aquifers_20816.png |
L_0185 | groundwater aquifers | T_1245 | FIGURE 1.2 | image | textbook_images/groundwater_aquifers_20817.png |
L_0185 | groundwater aquifers | T_1245 | FIGURE 1.3 | image | textbook_images/groundwater_aquifers_20818.png |
L_0185 | groundwater aquifers | T_1245 | FIGURE 1.4 | image | textbook_images/groundwater_aquifers_20819.png |
L_0186 | groundwater depletion | T_1247 | FIGURE 1.1 | image | textbook_images/groundwater_depletion_20820.png |
L_0187 | groundwater pollution | T_1251 | FIGURE 1.1 Tanks may break and leak whatever tox- ins they contain into the ground. | image | textbook_images/groundwater_pollution_20824.png |
L_0188 | growth of human populations | T_1254 | FIGURE 1.1 | image | textbook_images/growth_of_human_populations_20825.png |
L_0188 | growth of human populations | T_1254 | FIGURE 1.2 Click image to the left or use the URL below. URL: https://www.ck12.org/flx/render/embeddedobject/186839 | image | textbook_images/growth_of_human_populations_20826.png |
L_0191 | heat transfer in the atmosphere | T_1258 | FIGURE 1.1 Thermal convection where the heat source is at the bottom and there is a ceiling at the top. | image | textbook_images/heat_transfer_in_the_atmosphere_20827.png |
L_0192 | heat waves and droughts | T_1261 | FIGURE 1.1 | image | textbook_images/heat_waves_and_droughts_20828.png |
L_0196 | hot springs and geysers | T_1278 | FIGURE 1.1 Even in winter, the water in this hot spring in Yellowstone doesnt freeze. | image | textbook_images/hot_springs_and_geysers_20837.png |
L_0196 | hot springs and geysers | T_1279 | FIGURE 1.2 | image | textbook_images/hot_springs_and_geysers_20838.png |
L_0197 | how fossilization creates fossils | T_1280 | FIGURE 1.1 | image | textbook_images/how_fossilization_creates_fossils_20839.png |
L_0197 | how fossilization creates fossils | T_1282 | FIGURE 1.2 Hyenas eating an antelope. Will the ante- lope in this photo become a fossil? | image | textbook_images/how_fossilization_creates_fossils_20840.png |
L_0197 | how fossilization creates fossils | T_1282 | FIGURE 1.3 Fossil shell that has been attacked by a boring sponge. | image | textbook_images/how_fossilization_creates_fossils_20841.png |
L_0197 | how fossilization creates fossils | T_1283 | FIGURE 1.4 | image | textbook_images/how_fossilization_creates_fossils_20842.png |
L_0197 | how fossilization creates fossils | T_1285 | FIGURE 1.5 organisms can be buried by mudslides, volcanic ash, or covered by sand in a sandstorm (Figure 1.6). Skeletons can be covered by mud in lakes, swamps, or bogs. | image | textbook_images/how_fossilization_creates_fossils_20843.png |
L_0197 | how fossilization creates fossils | T_1285 | FIGURE 1.6 | image | textbook_images/how_fossilization_creates_fossils_20844.png |
L_0197 | how fossilization creates fossils | T_1286 | FIGURE 1.7 of past climates and geological conditions as well. | image | textbook_images/how_fossilization_creates_fossils_20845.png |
L_0197 | how fossilization creates fossils | T_1287 | FIGURE 1.8 | image | textbook_images/how_fossilization_creates_fossils_20846.png |
L_0198 | how ocean currents moderate climate | T_1288 | FIGURE 1.1 London, England in winter. | image | textbook_images/how_ocean_currents_moderate_climate_20847.png |
L_0198 | how ocean currents moderate climate | T_1288 | FIGURE 1.2 | image | textbook_images/how_ocean_currents_moderate_climate_20848.png |
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