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| moving away from each other |
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| mountains formed by magma from Earth's interior |
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| currently erupting or have erupted in recorded history |
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| plates move away from each other |
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| plates collide and slide over each other |
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| found at areas where magma rises to surface, Hawaiian islands |
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| sediments build up and compress, limestone |
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| pressure and heat applied to rock inside Earth's mantle, slate |
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| rock melts and resolidifies, magma comes to surface, emerges as lava, cools to make rock, basalt |
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| greenhouse effect from ozone |
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| aka ionosphere, absorbs solar wind from Sun |
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| day to day temperature, pressure, sunlight, wind speed, humidity |
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| constant patterns of an area |
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| vertical currents that rise from warm gases expanding and becoming less dense |
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| temperature water vapor condenses into liquid |
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| fallen condensation (frozen or liquid) |
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| air from body of water moves inland and runs into mountain, rises and on other side, no moisture left |
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| intense tropical storms (typhoon or cyclone in Pacific Ocean) |
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| where water from a particular stream collects and drains into |
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| where rivers meet ocean, made of deposited sediments |
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| freshwater and saltwater mix, rich with species |
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| marshes, swamps, bogs, prairie potholes, flood plains, ecologically diverse |
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| water below ground, can be from wells or aquifers (layers of Earth or gravel with water) |
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| shallow water at shoreline |
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| open water, sunlight can penetrate |
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| between shore and end of continental shelf |
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| no photosynthesis, middle region |
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| deep ocean, very cold, little dissolved oxygen, high nutrients |
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| surface and plant litter, lots organic matter, fungi, freshly fallen |
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| topsoil, lots of organic matter, mineral material, humus, partially decomposed |
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| regolith, partially broken down inorganic materials, parent material |
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| bedrock, unaltered parent material |
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| thin layer taken off land surface |
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| capacity to supply nutrients (nitrogen, phosphorus, potassium) for plant growth |
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| mineral salts accumulate in soil, saline irrigation |
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Less than 25 cm rain per year, sandy soil Lots of cacti b/c water-adapted 30 degrees north and south of equator |
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50-75 cm rain, shallow infertile soil Small trees w/ big leaves, shrubs Western North America, Mediterranean |
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Less than 25 cm rain, permafrost for soil Small herbaceous plants Northern parts of North America, Europe, and Russia |
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10-60 cm rain, rich soil Many types of grasses N. America prairies, S. African velds, Russian steppes, Argentinean pampas |
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75-250 cm, high rainfall, rich soil Hardwood trees N. America, E. Asia, Europe, Australia |
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200-400 cm, high rainfall, poor soil Tall trees, vines S. America, W. Africa, Southeast Asia |
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| Taiga (Coniferous Forest) |
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20-60 cm rainfall, acidic soil Coniferous trees Northern parts of N. America and Eurasia |
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| Convert sun energy or chemical energy into carbohydrates, photosynthesis or chemosynthesis |
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| lichens grow in lifeless area |
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| grasses, existing community has been cleared with soil leftover |
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| species in first stages of primary or secondary succession |
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| final stage of succession |
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| (K) is max population size that can be supported with resources available in particular region |
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| conversion of productive land to desert |
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| Causes of desertification |
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| overgrazing, deforestation, adverse soil erosion, poor drainage of irrigated land, overuse of water supplies |
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| repeated irrigation forces soil salts to the top |
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| removing trees for agri. or selling as lumber |
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| never cut, growing for hundreds of years |
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| trees and crops planted together |
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| animals eat grass faster than it grows |
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| not regenerated during human existence |
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