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Chapter 1.3 Vocabulary
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weatheringthe chemical or mechanical process by which a rock is gradually broken down, eventually becoming soil
chemical weatheringthe process by which the actual chemical structure of a rock is changed, usually when water and carbon dioxide cause a breakdown of a rock
agents of erosionwind, water and glaciers
dust bowlwhen great dust storms covered the mid-western states
morainesa ridgelike mass of rock, gravel, sand and clay carried and deposited by a glacier
ice agethe period of time when the ewarth was really cold
mechanical weatheringwhen a rock is actually broken down physically
acid rainchemicals in the pollted air combine with water vapor and fall back to earth
sedimentsmall particles of soil, sand and gravel
loessthe windblown deposits of mineral-rich dust and silt
"U" shaped valleysvalleys formed by glaciers
continental glaciers/ice sheetsbroad, flat glaciers found in Greenland and Antarctica
frost wedgingwhen water freezes into a crack in a rock; because water expands when it freezes,the ice widens the cracka nd eventually splits the rock
erosionthe movement of weathered materials such as gravel, soil and sand
deltatriangular shaped deposits of sediment at the mouth of ariver
glaciershuge, slow moving sheets of ice
"V" shaped valleysvalleys formed by water
valley/alpine glaciersfound throughout the world on mountain valleys where the weather is not warm enough to melt ice