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All 34 terms

TermDefinition
Glaciermoving body of ice on land that flows downslope or outward from an area of accumulation
Little Ice Agean interval from about 1500 to the mid-to-late- 1800 during which glaciers expanded to their greatest historical extent
Valley Glaciera glacier confined to a mountain valley or an interconnected system of mountain valleys
Continental Glaciersa glacier that covers a vast area (at least 50,00km2) and is not confined by topography: also called ice sheet
Ice Capa dome-shaped mass of glacial ice that covers less than 50,000km2
Glaciationrefers to all aspects of glaciers, including their origin, expansion, and retreat, and their impact on the earth's surface
Glacial Icewater in the solid state within a glacier: forms as snow partially melts and refreezes and compacts so that it is transforms first to firn and then to glacial ice
Plastic Flowthe flow that takes place in response to pressure and causes deformation with no fracturing
Basal Slipmovement involving a glacier sliding over its underlying surface
Glacial Budgetthe balance between expansion and contraction of a glacier in response to accumulation versus wastage
Zone of Accumulationthe part of a glacier where additions exceeds losses and the glacier's surface is perennially covered with snow.
Zone of Wastagethe part of a glacier where losses from melting, sublimation, and calving of icebergs exceed the rate of acculmation
Glacial Surgea time of greatly accelerated flow in a glacier. commonly results in displacement of the glacier's terminus by several km
Abrasionthe process whereby rock is worn smooth by the impact of sediment transported by running water, glaciers, waves, and winds
Glacial Polisha smooth, glistening rock surface formed by the movement of sediment-laden ice over bedrock
Glacial Striationsa straight scratch rarely more than a few millimeters deep on a rock caused by the movement of sediment-laden glacial ice
U-Shaped glacial trougha valley with steep or vertical walls and a broad, rather flat floor formed by the movement of a glacier through a stream valley
fiordan arm of the sea extending into a glacial trough eroded below sea level
hanging valleya tributary glacial valley whose floor is at a higher level that than of the main glacial valley
Glacial drifta collective term for all sediment deposited directly by glacial ice (till) and by meltwater streams (outwash).
glacial erraticsa rock fragment carried some distance from its source by a glacier and usually deposited on bedrock of a different compostion
stratified driftglacial deposits that show both stratification and sorting
end morainesa pile or ridge of rubble deposited at the terminus of a glacier
ground morainesthe layer of sediment released from melting ice as a glacier's terminus retreats
recessional morainesan end moraine that forms when a glacier;s terminus retreats, the stabilizes, and a ridge or mound of till is deposited
lateral morainesridge of sediment deposited along the margin of a valley glacier
medial morainea moraine carried on the central surface of a glacier; formed where two lateral moraines merge
drumlinsan elongate hill of till formed by the movement of a continental glacier or by floods
valley trainsa long, narrow deposit of stratified drift confined within a glacial valley
outwash plainthe sediment deposited by meltwater discharging from a continental glacier's terminus
kamesconical hill if stratified drift originally deposited in a depression on a glacier's surface
eskersa long, sinuous ridge of stratified drift deposited by running water in a tunnel beneath stagnant ice.
Milankovitch theoryan explanation for the cyclic variations in climate and the onset ice ages as a result of irregularities in earth's rotation and orbit
firngranular snow formed by partial melting and refreezing of snow; transitional material between snow and glacial ice
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Set Information

Terms 34
Creator PearlCrest
Created September 22, 2009
Groups None
Subject Geology
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