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A nifty little presentation naming the types of glaciers... *An ice sheet is also called a continental glacier. MADE FOR SCIENCE OLYMPIAD (Dynamic Planet) 2012-2013
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Dynamic PlanetGlaciers
Abby Rooney
http://nsidc.org/cryosphere/glaciers/questions/types.htmlThanks to Rachel Richards for sharing this link!
Ice SheetsLarge sheets of ice expanding over 50,000 kilometers
Antarctica & Greenland
Antarctica- 4,200 meters thick ice sheet
Ice sheets cover everything but Transantarctic Mountains (Antarctica)
Ice ShelvesHappens when ice sheets float on water
Few hundred meters – 1,000 meters
Surround Antarctic continent
When retreating, may show climate change
Ice CapsMiniature ice sheets
< than 50,000 kilometers
Polar & sub-polar regions
Greenland- ice sheet
Iceland- ice cap
Ice StreamsChannelized glaciers that flow rapidly
Many Ice streams in Antarctica
Ice FieldsSmaller than ice caps
Flow: underlying topography
Mountain GlaciersFlow out of ice fields
Span several peaks or a whole mountain range
Places: Arctic Canada, Alaska, Andes, Himalayas, Antarctica
Valley GlaciersCome from mountain glaciers or ice fields
Slide down valleys
Look like giant tongues
Long; flow beyond snow line
May reach sea level
Piedmont GlaciersHappen when steep valley glaciers spill into flat plains
Spread into bulb-like lobes
Malaspina Glacier, Alaska: 5,000 square kilometers
Cirque GlaciersNamed for bowl-like hollows (they live there)
High mountainsides
Wide
Hanging GlaciersIce aprons
Cling to steep mountainsides
Wide
Common in Alps- cause Avalanches
Tidewater GlaciersFlow far enough to reach out into the sea
Responsible for splitting small icebergs
May cause problems for shipping lanes
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