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L_0105 | cenozoic plate tectonics | T_0974 | FIGURE 1.2 | image | textbook_images/cenozoic_plate_tectonics_20648.png |
L_0108 | chemical weathering | T_0983 | FIGURE 1.1 | image | textbook_images/chemical_weathering_20655.png |
L_0108 | chemical weathering | T_0984 | FIGURE 1.2 | image | textbook_images/chemical_weathering_20656.png |
L_0108 | chemical weathering | T_0985 | FIGURE 1.3 | image | textbook_images/chemical_weathering_20657.png |
L_0108 | chemical weathering | T_0986 | FIGURE 1.4 When iron-rich minerals oxidize, they pro- duce the familiar red color found in rust. | image | textbook_images/chemical_weathering_20658.png |
L_0108 | chemical weathering | T_0988 | FIGURE 1.5 | image | textbook_images/chemical_weathering_20659.png |
L_0112 | clouds | T_1006 | FIGURE 1.1 | image | textbook_images/clouds_20664.png |
L_0112 | clouds | T_1010 | FIGURE 1.2 | image | textbook_images/clouds_20665.png |
L_0112 | clouds | T_1011 | FIGURE 1.3 | image | textbook_images/clouds_20666.png |
L_0112 | clouds | DD_0076 | This diagram shows the common types of clouds in the troposphere. The three main types of clouds are cirrus, stratus and cumulus. The types of clouds varies according to how high it is above the ground from 5,000 feet up to 20,000 feet. Because of the cold temperature at high altitudes, clouds are made up of ice crystals. Cloud types can be easily identified by their appearance. Stratus and Cumulus clouds usually form at lower altitudes, clumpy and usually causes rain and precipitation. While Cirrus clouds form at higher altitudes where the temperature is fairly constant and is usually evenly scattered. Clouds play a big role in maintaining the balance of the earth's temperature and has a big impact on the weather. Shown also are Aerosols that stay in the lower atmosphere. Aerosols are produced naturally but recent concerns have been raised since these are largely man-made and Aerosols have significant impacts on cloud and weather system. | image | teaching_images/types_clouds_7649.png |
L_0112 | clouds | DD_0077 | Below the stratus, there is steady precipitation whereas below the cumulus, there is showery precipitation. Right below 6,500 ft, there are low clouds and between 6,500 ft and 23,000 ft, there are the middle clouds. It is higher than 23,000 ft where there is the cirrus, cirrostratus, and cirrocumulus. There is also a halo around the sun. | image | teaching_images/types_clouds_7645.png |
L_0117 | composition of the atmosphere | T_1028 | FIGURE 1.1 | image | textbook_images/composition_of_the_atmosphere_20677.png |
L_0117 | composition of the atmosphere | T_1031 | FIGURE 1.2 Mean winter atmospheric water vapor in the Northern Hemisphere when temperature and humidity are lower than they would be in summer. | image | textbook_images/composition_of_the_atmosphere_20678.png |
L_0122 | dark matter | T_1041 | FIGURE 1.1 The arc around the galaxies at the center of this image is caused by gravitational lensing. The addition of gravitational pull from dark matter is required to explain this phenomenon. | image | textbook_images/dark_matter_20685.png |
L_0122 | dark matter | T_1042 | FIGURE 1.2 | image | textbook_images/dark_matter_20686.png |
L_0129 | divergent plate boundaries | T_1058 | FIGURE 1.1 This map shows the three major plate boundaries in or near California. | image | textbook_images/divergent_plate_boundaries_20693.png |
L_0130 | divergent plate boundaries in the oceans | T_1060 | FIGURE 1.1 Iceland is the one location where the ridge is located on land: the Mid-Atlantic Ridge separates the North American and Eurasian plates | image | textbook_images/divergent_plate_boundaries_in_the_oceans_20695.png |
L_0134 | earthquake characteristics | T_1081 | FIGURE 1.1 | image | textbook_images/earthquake_characteristics_20701.png |
L_0134 | earthquake characteristics | T_1082 | FIGURE 1.2 In about 75% of earthquakes, the focus is in the top 10 to 15 kilometers (6 to 9 miles) of the crust. Shallow earthquakes cause the most damage because the focus is near where people live. However, it is the epicenter of an earthquake that is reported by scientists and the media. | image | textbook_images/earthquake_characteristics_20702.png |
L_0135 | earthquake damage | T_1084 | FIGURE 1.1 A landslide in a neighborhood in Anchor- age, Alaska, after the 1964 Great Alaska earthquake. | image | textbook_images/earthquake_damage_20703.png |
L_0135 | earthquake damage | T_1084 | FIGURE 1.2 | image | textbook_images/earthquake_damage_20704.png |
L_0135 | earthquake damage | T_1085 | FIGURE 1.3 | image | textbook_images/earthquake_damage_20705.png |
L_0136 | earthquake safe structures | T_1086 | FIGURE 1.1 | image | textbook_images/earthquake_safe_structures_20706.png |
L_0136 | earthquake safe structures | T_1087 | FIGURE 1.2 | image | textbook_images/earthquake_safe_structures_20707.png |
L_0136 | earthquake safe structures | T_1089 | FIGURE 1.3 | image | textbook_images/earthquake_safe_structures_20708.png |
L_0137 | earthquake zones | T_1090 | FIGURE 1.1 | image | textbook_images/earthquake_zones_20709.png |
L_0137 | earthquake zones | T_1091 | FIGURE 1.2 Click image to the left or use the URL below. URL: https://www.ck12.org/flx/render/embeddedobject/186182 | image | textbook_images/earthquake_zones_20710.png |
L_0138 | earthquakes at convergent plate boundaries | T_1093 | FIGURE 1.1 | image | textbook_images/earthquakes_at_convergent_plate_boundaries_20711.png |
L_0138 | earthquakes at convergent plate boundaries | T_1093 | FIGURE 1.2 | image | textbook_images/earthquakes_at_convergent_plate_boundaries_20712.png |
L_0138 | earthquakes at convergent plate boundaries | T_1095 | FIGURE 1.3 | image | textbook_images/earthquakes_at_convergent_plate_boundaries_20713.png |
L_0139 | earthquakes at transform plate boundaries | T_1097 | FIGURE 1.1 | image | textbook_images/earthquakes_at_transform_plate_boundaries_20714.png |
L_0141 | earths crust | T_1101 | FIGURE 1.1 | image | textbook_images/earths_crust_20716.png |
L_0141 | earths crust | T_1102 | FIGURE 1.2 | image | textbook_images/earths_crust_20717.png |
L_0143 | earths layers | T_1113 | FIGURE 1.1 | image | textbook_images/earths_layers_20719.png |
L_0145 | earths mantle | T_1118 | FIGURE 1.1 | image | textbook_images/earths_mantle_20721.png |
L_0145 | earths mantle | T_1118 | FIGURE 1.2 | image | textbook_images/earths_mantle_20722.png |
L_0147 | earths tectonic plates | T_1120 | FIGURE 1.1 Earthquakes outline the plates. | image | textbook_images/earths_tectonic_plates_20724.png |
L_0147 | earths tectonic plates | T_1121 | FIGURE 1.2 Mantle convection drives plate tectonics. Hot material rises at mid-ocean ridges and sinks at deep sea trenches, which keeps the plates moving along the Earths surface. | image | textbook_images/earths_tectonic_plates_20725.png |
L_0153 | effusive eruptions | T_1136 | FIGURE 1.1 | image | textbook_images/effusive_eruptions_20737.png |
L_0153 | effusive eruptions | T_1137 | FIGURE 1.2 | image | textbook_images/effusive_eruptions_20738.png |
L_0153 | effusive eruptions | T_1138 | FIGURE 1.3 A road is overrun by an eruption at Ki- lauea volcano in Hawaii. | image | textbook_images/effusive_eruptions_20739.png |
L_0159 | evolution of simple cells | T_1149 | FIGURE 1.1 | image | textbook_images/evolution_of_simple_cells_20749.png |
L_0159 | evolution of simple cells | T_1151 | FIGURE 1.2 | image | textbook_images/evolution_of_simple_cells_20750.png |
L_0159 | evolution of simple cells | T_1151 | FIGURE 1.3 | image | textbook_images/evolution_of_simple_cells_20751.png |
L_0159 | evolution of simple cells | T_1153 | FIGURE 1.4 | image | textbook_images/evolution_of_simple_cells_20752.png |
L_0159 | evolution of simple cells | T_1153 | FIGURE 1.5 | image | textbook_images/evolution_of_simple_cells_20753.png |
L_0163 | explosive eruptions | T_1163 | FIGURE 1.1 Ash and gases create a mushroom cloud above Mt. Redoubt in Alaska, 1989. The cloud reached 45,000 feet and caught a Boeing 747 in its plume. | image | textbook_images/explosive_eruptions_20758.png |
L_0163 | explosive eruptions | T_1164 | FIGURE 1.2 | image | textbook_images/explosive_eruptions_20759.png |
L_0163 | explosive eruptions | T_1164 | FIGURE 1.3 | image | textbook_images/explosive_eruptions_20760.png |
L_0163 | explosive eruptions | T_1165 | FIGURE 1.4 | image | textbook_images/explosive_eruptions_20761.png |
L_0163 | explosive eruptions | T_1166 | FIGURE 1.5 | image | textbook_images/explosive_eruptions_20762.png |
L_0166 | finding and mining ores | T_1175 | FIGURE 1.1 | image | textbook_images/finding_and_mining_ores_20769.png |
L_0166 | finding and mining ores | T_1176 | FIGURE 1.2 gold traveled down rivers and then settled in gravel deposits. Currently, California has active mines for gold and silver and for non-metal minerals such as sand and gravel, which are used for construction. | image | textbook_images/finding_and_mining_ores_20770.png |
L_0166 | finding and mining ores | T_1177 | FIGURE 1.3 Underground mine. | image | textbook_images/finding_and_mining_ores_20771.png |
L_0209 | intraplate activity | T_1334 | FIGURE 1.1 | image | textbook_images/intraplate_activity_20866.png |
L_0209 | intraplate activity | T_1334 | FIGURE 1.2 The Hawaiian-Emperor chain can be traced from Hawaii in the central Pacific north of the Equator into the Aleutian trench, where the oldest of the volcanoes is being subducted. It looks like a skewed "L". | image | textbook_images/intraplate_activity_20867.png |
L_0209 | intraplate activity | T_1335 | FIGURE 1.3 | image | textbook_images/intraplate_activity_20868.png |
L_0214 | landforms from erosion and deposition by gravity | T_1351 | FIGURE 1.1 | image | textbook_images/landforms_from_erosion_and_deposition_by_gravity_20881.png |
L_0214 | landforms from erosion and deposition by gravity | T_1353 | FIGURE 1.2 | image | textbook_images/landforms_from_erosion_and_deposition_by_gravity_20882.png |
L_0214 | landforms from erosion and deposition by gravity | T_1353 | FIGURE 1.3 | image | textbook_images/landforms_from_erosion_and_deposition_by_gravity_20883.png |
L_0214 | landforms from erosion and deposition by gravity | T_1353 | FIGURE 1.4 Creep is the extremely gradual movement of soil downhill. Curves in tree trunks indicate creep because the base of the tree is moving downslope while the top is trying to grow straight up (Figure 1.5). Tilted telephone or power company poles are also signs of creep. | image | textbook_images/landforms_from_erosion_and_deposition_by_gravity_20884.png |
L_0214 | landforms from erosion and deposition by gravity | T_1353 | FIGURE 1.5 | image | textbook_images/landforms_from_erosion_and_deposition_by_gravity_20885.png |
L_0214 | landforms from erosion and deposition by gravity | T_1357 | FIGURE 1.6 A rock wall stabilizes a slope that has been cut away to make a road. | image | textbook_images/landforms_from_erosion_and_deposition_by_gravity_20886.png |
L_0220 | locating earthquake epicenters | T_1380 | FIGURE 1.1 | image | textbook_images/locating_earthquake_epicenters_20906.png |
L_0234 | mesozoic plate tectonics | T_1426 | FIGURE 1.1 | image | textbook_images/mesozoic_plate_tectonics_20937.png |
L_0234 | mesozoic plate tectonics | T_1426 | FIGURE 1.2 | image | textbook_images/mesozoic_plate_tectonics_20938.png |
L_0241 | mineral formation | T_1442 | FIGURE 1.1 | image | textbook_images/mineral_formation_20946.png |
L_0241 | mineral formation | T_1444 | FIGURE 1.2 | image | textbook_images/mineral_formation_20947.png |
L_0241 | mineral formation | T_1444 | FIGURE 1.3 | image | textbook_images/mineral_formation_20948.png |
L_0241 | mineral formation | T_1445 | FIGURE 1.4 | image | textbook_images/mineral_formation_20949.png |
L_0241 | mineral formation | T_1445 | FIGURE 1.5 | image | textbook_images/mineral_formation_20950.png |
L_0241 | mineral formation | T_1446 | FIGURE 1.6 | image | textbook_images/mineral_formation_20951.png |
L_0242 | mineral groups | T_1448 | FIGURE 1.1 | image | textbook_images/mineral_groups_20952.png |
L_0242 | mineral groups | T_1448 | FIGURE 1.2 | image | textbook_images/mineral_groups_20953.png |
L_0242 | mineral groups | T_1449 | FIGURE 1.3 A gold nugget. | image | textbook_images/mineral_groups_20954.png |
L_0242 | mineral groups | T_1450 | FIGURE 1.4 | image | textbook_images/mineral_groups_20955.png |
L_0242 | mineral groups | T_1451 | FIGURE 1.5 | image | textbook_images/mineral_groups_20956.png |
L_0242 | mineral groups | T_1451 | FIGURE 1.6 | image | textbook_images/mineral_groups_20957.png |
L_0242 | mineral groups | T_1452 | FIGURE 1.7 | image | textbook_images/mineral_groups_20958.png |
L_0242 | mineral groups | T_1453 | FIGURE 1.8 Apatite. | image | textbook_images/mineral_groups_20959.png |
L_0242 | mineral groups | T_1454 | FIGURE 1.9 | image | textbook_images/mineral_groups_20960.png |
L_0242 | mineral groups | T_1455 | FIGURE 1.10 This mineral has shiny, gold, cubic crys- tals with striations, so it is pyrite. | image | textbook_images/mineral_groups_20961.png |
L_0243 | mineral identification | T_1458 | FIGURE 1.1 Purple quartz, known as amethyst, and clear quartz are the same mineral despite the different colors. | image | textbook_images/mineral_identification_20962.png |
L_0243 | mineral identification | T_1460 | FIGURE 1.2 | image | textbook_images/mineral_identification_20963.png |
L_0243 | mineral identification | T_1463 | FIGURE 1.3 Halite has cubic cleavage. | image | textbook_images/mineral_identification_20964.png |
L_0243 | mineral identification | T_1463 | FIGURE 1.4 | image | textbook_images/mineral_identification_20965.png |
L_0243 | mineral identification | T_1463 | FIGURE 1.5 Fluorite has octahedral cleavage. | image | textbook_images/mineral_identification_20966.png |
L_0243 | mineral identification | T_1464 | FIGURE 1.6 | image | textbook_images/mineral_identification_20967.png |
L_0244 | minerals | T_1466 | FIGURE 1.1 | image | textbook_images/minerals_20968.png |
L_0244 | minerals | T_1469 | FIGURE 1.2 | image | textbook_images/minerals_20969.png |
L_0247 | mountain building | T_1477 | FIGURE 1.1 | image | textbook_images/mountain_building_20977.png |
L_0247 | mountain building | T_1478 | FIGURE 1.2 | image | textbook_images/mountain_building_20978.png |
L_0247 | mountain building | T_1479 | FIGURE 1.3 | image | textbook_images/mountain_building_20979.png |
L_0267 | plate tectonics through earth history | T_1551 | FIGURE 1.1 The Appalachian Mountains in New Hampshire. | image | textbook_images/plate_tectonics_through_earth_history_21027.png |
L_0267 | plate tectonics through earth history | T_1551 | FIGURE 1.2 | image | textbook_images/plate_tectonics_through_earth_history_21028.png |
L_0272 | precipitation | T_1565 | FIGURE 1.1 | image | textbook_images/precipitation_21038.png |
L_0272 | precipitation | T_1565 | FIGURE 1.2 | image | textbook_images/precipitation_21039.png |
L_0272 | precipitation | T_1565 | FIGURE 1.3 | image | textbook_images/precipitation_21040.png |
L_0273 | predicting earthquakes | T_1567 | FIGURE 1.1 | image | textbook_images/predicting_earthquakes_21041.png |
L_0273 | predicting earthquakes | T_1568 | FIGURE 1.2 | image | textbook_images/predicting_earthquakes_21042.png |
Subsets and Splits