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Earth Science- GLACIERS

AB
GLACIERslow moving mass of ice 1000s of feet thick
VALLEY GLACIER VS. CONTINENTAL GLACIERvalley glaciers fill a mountain (alpine) valley; continental glaciers are much larger and round off mountain tops that they cover
ICE SHEETan ice pack covering nearly an entire landmass
ABLATIONloss of ice at the end of a glacier
AUSTRALIAthe only continent without glaciers
ARETEsharp, narrow ridges between cirques
TERMINAL MORAINEunsorted glacial deposits showing the farthest advance; Long Island is one
DRIFTany deposits left behind when a glacier melts
ESKERwinding snakelike deposit of a subglacial stream
U-SHAPED VALLEYalpine glacier erosion
KETTLEdepression left by a melted subterranean ice block
ERRATICboulder deposited by a glacier far from its origin
SNOW LINElowest elevation at which snow remains all year; when moving away from the equator the snow line becomes lower
FIRNsnow that gets compressed and recrystalizes as granular ice
FASTEST MOVING SIDE OF A GLACIERcenter of the surface
GREAT LAKESformed by ice age erosion and melting
CREVASSEhorizontal cracks along the surface of a glacier
CALVINGicebergs break off the teminus of a glacier
ERRATICboulders plucked and moved by a glacier
BASAL SLIPsliding along the base of the glacier
PLASTIC FLOWmovement within the glacier due to pressure


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