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Glacial Landscapes
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Erosional Land- scapes Areal scour vs. Selective linear erosion
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Cirques
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Arêtes and Horns Jointing and mass wasting (two cirques) Coalescence of three or more cirques
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Troughs “U” shaped –Like a stream, but slower! –X-section area = f(Q) –Elevation = f(Q) at common surface
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Trough Erosion Scour @ bed Mass wasting @ sides (transport)
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Paternoster Lakes Local overdeepenings –Rel. erodibility? –Extension/ compression? Some evidence of cyclicity
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Grinnell Creek
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Landforms of Areal Scour Typically streamlined –Erosional or depositional? –Glacial or glaciofluvial? Discrete or continuous distribution? [after Rose, 1987]
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Outwash Streams and Sediment
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Subglacial Channels Eroded into bedrock (e.g., Antarctica) –Pressure –Tools
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Note: –Escarpment –Notches –Channels
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Eskers Subglacial streams –Deposits –Pressure- driven (may trend uphill!) Copyright © Daryl Dagesse 2002
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Moraines Lateral (Stripped) Terminal (single, massive, sharp-crested) (multiple, subtle, hummocky)
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Pleistocene Moraines
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Moraines (map) Below ELA Lastglacial (older?) Effects on streams: –Moraine- dammed –Glacier- dammed –Outwash
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Till Plains/Outwash “Glacier foreland”
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Clark Fork of the Yellowstone
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Paradise Valley
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Kame Terrace Interaction between valley wall and glacier wall. Example: Blackfoot River valley – till/kame Terminal moraine Kame terrace
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Ice sheet “ground moraine” Kame and kettle topography
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Outburst Floods (Jökulhlaup) Sudden drainage of a glacial lake -Breaching of moraines or floating of ice dams. -Calving of icebergs -Typically cyclic -Massive geomorphic work but potentially devastating http://www.sfu.ca~qgrc/people/john/floods.htm [Clague, 1997]
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Missoula/Spokane floods
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Pluvial Lakes Closed basins –Bonneville –Lahontan –Owens+
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Glaciation and Earth Systems Oscillating glacial/non-glacial climates Changing ice/wind/water/coasts… (yr x 10 3 )
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