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ES Chapter 07 Vocabulary Review

Glaciers, Deserts, & Wind
Prentice Hall Earth Science

AB
alluvial fana fan-shaped deposit of sediment formed when a stream’s slope is abruptly reduced
deflationthe lifting and removal of loose material by wind
desert pavementa layer of coarse pebbles and gravel created when wind removed the finer material
dunea hill or ridge of wind-deposited sand
glaciera thick mass of ice originating on land from the compaction and recrystallization of snow that shows evidence of past or present flow
ice agea period of time when much of Earth’s land is covered by glaciers
loessdeposits of windblown silt, lacking visible layers, generally light yellow, and capable of maintaining a nearly vertical cliff
morainea ridge of unsorted sediment left by a glacier
playa lakea flat area on the floor of an undrained desert basin (playa that fills and becomes a lake after heavy rain)
snowlinelowest elevation in a particular area that remains covered in snow all year
tillsediment of different sizes deposited directly by a glacier
valley glaciera glacier confined to a mountain valley, which in most instances had previously been a stream valley; also known as an alpine glacier
cirquean amphitheater-shaped basin at the head of a glaciated valley produced by frost wedging and plucking
continental glaciera very large, thick mass of glacial ice that covers a large region and flows outward in all directions from one or more accumulation centers; also called a continental ice sheet
crevassea deep crack in the brittle surface of a glacier
drumlina streamlined asymmetrical hill composed of glacial till; The steep side of the hill faces the direction from which the ice advanced.
eskersinuous ridge composed largely of sand and gravel deposited by a stream flowing in a tunnel beneath a glacier near its terminus
glacial erratican ice-transported boulder that was not derived from bedrock near its present site
kettledepression created when a block of ice became lodged in glacial deposits and subsequently melted
outwash plaina relatively flat, gently sloping plain consisting of materials deposited by meltwater streams in front of the margin of an ice sheet
firncoarse grains of ice resulting from recrystallization of compressed snow
ventifacta cobble or pebble polished and shaped by the sandblasting effect of wind


Chemistry & Physics
Lumberton High School
Lumberton, NC

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