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Ch 4 Landforms

AB
hydrologic cyclethe continous circulation of water between the atmosphere, oceans, and Earth
drainage basinan area drained by a major river and its tributaries
ground waterthe water held in the pores of rock
water tablethe level at which the rock is saturated
landformsnaturally formed features on the surface of the earth
deltaa triangular area of land formed from deposits at the mouth of a river
islanda body of land completely surrounded by water
oasisa spot of fertile land in a desert, fed by water from wells or underground springs
valleylow land between hills or mountains
glaciera large ice mass that moves slowly down a mountain or over land
canyona narrow, deep valley with steep sides
plateaua broad, flat area of the land higher than the surrounding land
continental shelfThe earth’s surface from the edge of a continent to the deep part of the ocean
topographythe combination of the surface shape and composition of the landforms and their distribution in a region
isthmusnarrow piece of land connecting two larger pieces of land
peninsulaland surrounded by water on three sides
crustthe outermost layer of earth
magmaliquid rock inside of Earth
plate tectonicstheory that explains how forces within the planet create landforms
erosionthe movement of surface material from one location to another
wind, rain, & icecauses of erosion
desalinizationremoval of salt from ocean water
tributarya smaller stream that flows into a larger river
irrigationartifically suppling water to the land
soil exhaustionoveruse of soil making it useless for farming
deforestationdestruction or loss of forests
reforestationreplanting of trees
aqueductsartificial chanels for suppling water
aquiferslayers of rock where groundwater is found
fossil fuelsenergy resources formed from ancient plants
hydroelectric powerelectricity produced by moving water
geothermal energyheat from Eatrh's interior used to make electricity

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