CCHS Glaciers Brown (copy)

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21 Terms

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Alpine / Valley Glacier

A glacier confined to a valley

<p>A glacier confined to a valley</p>
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Ice Cap

a dome shaped mass of ice that covers less than 50,000 square miles

<p>a dome shaped mass of ice that covers less than 50,000 square miles</p>
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Ice Shelf

A thick, floating platform of ice that forms where a glacier or ice sheet flows down to a coastline and onto the ocean surface.

<p>A thick, floating platform of ice that forms where a glacier or ice sheet flows down to a coastline and onto the ocean surface.</p>
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Snow line

The elevation above which snow remains all year long

<p>The elevation above which snow remains all year long</p>
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axial precession (wobble)

The direction Earth's axis of rotation is pointed

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Obliquity

The angle Earth's axis is tilted with respect to Earth's orbital plane

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eccentricity

The shape of Earth's orbit

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continental glacier

Dome shaped glacier of at least 50,000 square miles

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Firn

partially compacted granular snow that is the intermediate stage between snow and glacial ice.

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glacial advance

when a mountain glacier's terminus extends farther down valley than before. usually associated with glacial periods (ice ages).

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glacial retreat

a glacier that loses more water than it gains. usually associated with interglacial periods (warm periods).

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glacier

A large, dense body of ice that is constantly moving due to its own weight

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Ice Age

A period of time lasting tens of thousands of years, where Earth's temperature drops very low and the polar ice caps and glaciers grow toward the equator.

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glacial period (ice age)

times with large ice sheets

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interglacial period

times without large ice sheets

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Louis Agassiz

the father of glaciology

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Milankovitch cycles

changes in Earth's position relative to the Sun that are believed to be a strong driver of Earth's long-term climate, and are responsible for triggering the beginning and end of glaciation periods (Ice Ages).

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rigid zone

the upper brittle zone (top 130 ft) of a glacier where the ice cracks into crevasses

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zone of plastic flow

the lower section (deeper than 130 ft) of a glacier that behaves like a plastic

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zone of accumulation

the part of a glacier that receives more mass by accumulation than loses by melting (above the snow line)

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zone of wastage

The area on a glacier where there is a net loss of snow and ice (below the snow line)