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*Earth & Space Science - Ch. 8 "Mass Movements, Wind, and Glaciers" Games

AB
mass movementdownslope movement of Earth materials, due to gravity, that can occur suddenly or very slowly
creepslow, steady downhill movement of loose weathered Earth materials, especially soils, causing objects on a slope to tilt
mudflowrapidly flowing, often destructive mixture of mud and water that can be triggered by an earthquake, intense rainstorm, or volcanic eruption
landsliderapid downslope movement of a mass of loose soil, rock, or debis that has separated from bedrock
slumpmass movement that occurs when Earth materials in a landslide rotate and slide along a curved surface, leaving a crescent-shaped scar on a slope
avalanchelandslide that occurs in a mountainous area when snow falls on an icy crust, becomes heavy, slips off, and slides swiftly down a mountainside
frictionresistance to sliding and rolling between a material and the surface
deflationlowering of land surface as a result of wind erosiion
abrasionsand and other particles rubbing against the surface of rocks
ventifactrocks shaped by wind-blown sediments
dunea pile of wind-blown sand
loesswind-blown silt deposits with a high concentration of nutrients
migrateto move from one location to another
glaciermass of ice that forms at Earth's poles and in mountainous regions at high elevations
valley glaciera glacier that forms in a valley in a mountainous area and widens V-shaped stream valleys into U-shaped glacial valleys as it moves downslope
continental glaciera glacier that forms over broad, contrinent-sized area of land and usually spteads out from its center
cirquea deep depression scooped out by a valley glacier
morainea ridge of mixed debris deposited by a melting glacier
outwash plainarea at the leading edge of a glacier, where outwash is deposited by meltwater streams
drumlinan elongated landform that results when a glacier moves over an older moraine
eskera long, winding ridge of layered sediments deposited by streams that flow beneath a melting glacier
kamea mound of layered sediment similar to an esker in origin but is conical in shape
kettlea lake formed by a hole in the ground left by a melted block of ice

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