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is a large mass of ice, resting on land or floating in the sea: – Cover ~11% of Earth’s land area today |
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Alpine Glaciers Continental Glaciers |
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Glaciers in mountain ranges are termed ‘alpine glaciers’ |
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A valley glacier is confined within a valley: |
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– Range in length from 100m to over 100 km – Erodes bedrock while flowing slowly downhill – Transports and deposits debris – A cirque is a bowl-shaped recess at the head of the valley |
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A continental glacier is a continuous mass of ice on continents |
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A continental glacier is a continuous mass of ice on continents |
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– Blankets 80% of Greenland and 90% of Antarctica |
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Underlying crust is isostatically depressed due to the enormous weight of the ice: |
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Crust depressed more than 2,000 m below sea level in Greenland and Antarctica |
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Continuous ice cover also associated with mountains: |
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– Ice cap is roughly circular and covers less than 50,000 km2 – Ice field has elongated pattern with ridges and peaks visible above the buried terrain |
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Glacier is an open system: – Inputs: |
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Ice, meltwater and water vapor |
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On the lower end below the firn line, glacier is wasted via ablation by several processes: |
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– Melting on the surface, internally and at the base – Ice removal by deflation (wind) – Calving of ice blocks – Sublimation |
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is where accumulation gain balances ablation loss |
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Rates of glacial flow ranges from almost nothing to 1-2 km/yr: |
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– Depends on rate of snow accumulation – Flowing glacier can develop crevasses |
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Glacier can lurch forward in a surge |
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Possible cause is build-up of water pressure underneath |
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Passing glacier can pluck and remove rock material via erosion: |
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Embedded rock can scour the landscape through abrasion as the glacier moves |
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Glacial erosion can convert |
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a V-shaped stream valley into a U-shaped valley |
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Two eroding cirques can create a |
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saddlelike depression in between called a ‘col’ |
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results from several cirques gouging a mountain summit from all sides |
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are a series of circular lakes |
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forms when a glacial trough intersects an ocean and seawater flows inland |
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Glacial drift consists of |
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unsorted and sorted glacial deposits (rocks & sediment): |
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Glacial drift consists of unsorted and sorted glacial deposits (rocks & sediment): |
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unstratified (non-layered) and unsorted |
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(layered) drift deposited by glacial meltwater |
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Moraines are specific landforms produced by deposition of glacial sediment |
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Lateral moraine forms on either side of glacier – Lateral moraines may merge to form medial moraine – Terminal moraine marks the glacier’s furthest extent |
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Continental glaciers form |
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across broad, open landscapes |
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Most erosional and depositional features are |
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associated with glacial retreat: |
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Outwash plains of stratified drift deposited by |
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Other features associated with Continental Glaciation: |
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Sinuous, narrow ridge of coarse sand and gravel that formed by meltwater stream that flowed beneath glacier |
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Hole left behind after large block of ice melts |
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Small hill or knob of poorly-sorted sand and gravel |
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Elongated deposit of till streamlined in the direction of continental ice movement |
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Located in subarctic and polar climates (tundra) |
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Landscapes consists of frost weathering and freeze-thaw shattering of rock: |
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Some associated with near-permanent ice – Others at high elevation and seasonally snowfree |
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soil or rock remain below freezing for at least two years but is not covered by glaciers |
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The freezing of water in soil and rock initiates frost action |
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– Expansion of water as it freezes fractures rock and disrupts soil |
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Saturated soil and rocks are subjected to large displacements when freezing: |
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– Vertical movement called frost heaving – Horizontal motions called frost thrusting |
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Proper construction in periglacial environments requires |
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raising of buildings and pipes above ground |
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The Last 1.6 Million Years |
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During the early 20th century, four major glacial advances were recognized and mapped in North America: |
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Wisconsin (maximum ~18,000 years ago) – Illinoian (ended ~130,000 years ago) – Kansan – Nebraskan (~2 m. |
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Three to five were recognized in |
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Recent studies of deep-sea cores indicate many |
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more glacial episodes than were recognized on land |
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Diverse Effects of Last Ice Age |
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Changes in oceanic circulation patterns |
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Glaciers locked up abundant water on continents, lowering sea level: |
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Coral reefs high and dry – Continental shelves and land bridges exposed – Rivers crossed exposed shelves, cutting canyons – On land, downcutting by rivers formed terraces |
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Sea Level Drop Lowered Base Level |
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Causing Streams On Land To Downcut And Form Terraces |
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Pleistocene Glaciation (~18,000 years ago |
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• Several major ice centers in Canada • Low-stand of sea level • Bering Land Bridge |
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Following retreat of glaciers after the last ice age, crustal rebound occurred around Hudson Bay, Canada, and the northern Baltic Sea over the last 10,000 years |
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Ice dam first broke ~ 15,000 years ago |
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Derived from outwash plains of glacial meltwater |
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Derived from outwash plains of glacial meltwater |
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– Meltwater carried large volumes of sediments from melting ice sheets; sediments deposited in outwash plain |
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During the fall and winter, melting of ice sheets ceased |
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– Flow of meltwater either ceased or was greatly reduced – Unvegetated floodplains dried out and were exposed to the wind – Glacially ground flour-like silt and clay winnowed by the wind – Particles blown downwind and deposited as loess deposits |
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Western U.S. was dotted with large lakes 12,000 – 30,000 years ago: |
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A time of wetter conditions during glaciation |
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Lacustrine Deposits: Lake sediment that form terraces along former shorelines |
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