16 - Glaciers as Landforms 2% of all water 88% of FW Covers Antarctica and Greenland avg 2.5 km...
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Transcript of 16 - Glaciers as Landforms 2% of all water 88% of FW Covers Antarctica and Greenland avg 2.5 km...
16 - Glaciers as Landforms16 - Glaciers as Landforms• 2% of all water• 88% of FW• Covers
Antarctica and Greenland avg 2.5 km thick
• Max 4 km thick• During
Pleistocene 20% of water on land
AccumulationAccumulation and Ablation
Unconfined Ice Sheet
Geomorphology of Alpine GlaciersGeomorphology of Alpine Glaciers
• http://www2.wwnorton.com/college/geo/egeo/animations/ch18.htm
Equilibrium line ~snow line, maximum flow in x-sec. Glaciers much higher average surface gradient than streams
Valley Glaciers
A Cirque Glacier
End of Glacier Debris Flow
Importance of glaciersImportance of glaciers• Influence earth’s Influence earth’s
energy balance - energy balance - albedoalbedo
• Major component of Major component of (fresh) water storage (fresh) water storage – affects sea level– affects sea level
• Important agent of Important agent of landform evolutionlandform evolution
Center moves faster than margins. Note ogives, annual waves
ObstaclesObstacles• Upglacier, the movement
of ice closes joints in the rock. Only abrasion occurs.
• Downglacier, over the crest of the bedrock, ice flow opens joints. Meltwater gets into cracks and freezes, enlarging cracks. Plucking removes rock.
Davidson Glacier near Davidson Glacier near Haines, AlaskaHaines, AlaskaAn Alpine glacier systemAn Alpine glacier system
Ledges (obstacles) beneath ice reflected by Crevasse Fields and Ice Pinnacles (Seracs)
Accumulation zone extending, ablation zone and buried obstacle compressing
Terminus
Ice Caps and Ice Caps and Continental Ice SheetsContinental Ice Sheets
Sentinal Range, Antarctica
http://www.nmm.ac.uk/server/show/conWebDoc.1221
•Antarctica is the broadest high place on Earth, the ice cap is up to 4km thick and covers the continent•Antarctica is a desert, with only 15 cm (6 inches) of snowfall a year around the South Pole•The lowest recorded temperature is -89.2 °C.•There is no life in Antarctica except near the coast
White, reflective, high latitude, positive feedback
Nunatak
Nunatak: exposed rocky area not covered with ice or snow
Byrd Glacier, Antarctica, an outlet glacierByrd Glacier, Antarctica, an outlet glacier
Zone of Accumulation
Outlet Glaciers
AblationAblation
AblationAblation
Vatnajokullhttp://pubs.usgs.gov/fs/2005/3056/
Formation of Glacier IceFormation of Glacier Ice
FirnBTW: note leading edges thrust over terminal debris
Ice DeformationIce Deformation
Accelerating
slowing
Wet GlaciersWet Glaciers• Warm = wet-based
• Cold = dry-based
• ρice < ρwater, therefore
Pressure increase on ice increases density to that of liquid water.
• Causes "melting point decrease“. Ice than would normally melt at 0oC = 32 o F now melts at a cooler temp. High pressure melting point called PMP - pressure melting point
– 0.7°C/ km of ice above you
• “Warm” ice = thick, fast
• Moves mostly by basal sliding on wet base
PressureMeltingPoint
Cold, High Polar, Dry BasedCold, High Polar, Dry BasedBase ice is frozen
These glaciers do not slide,
they only move by internal deformation
Plucking
Intermediate (subpolar)Intermediate (subpolar)
Temperate, Wet BedTemperate, Wet Bed
Striations, transport by subice flows
Rapidly Flowing GlaciersRapidly Flowing Glaciers
Observed Ice Core TempsObserved Ice Core Temps
• Greenland– Tbed < 0°C
• Antarctica– Tbed ≈ 0°C
Pressure Melting and RegelationPressure Melting and Regelation
• For ice near Pressure Melting Point:– Movement increases pressure, thus melting, on
the up-ice side of an obstruction– Movement away from the obstruction releases
pressure - causes freezing on the down-ice side – “regelation”
meltmeltmeltmelt
Effects of Pressure MeltingEffects of Pressure Melting
• High pressure is experienced on the up-ice side of an obstruction.
• Pressure melt results
• Water migrates around obstacle
• Regelation occurs in low pressure zone
MELTREFREEZE =REFREEZE ="Regelation""Regelation"
Erosion by PluckingErosion by Plucking• Melt then regelation
mix loose bed material and refreezing ice at base – gets into rock cracks, expands w/ freeze and pushes: “plucking”
AbrasionAbrasion
• Plucked material is available to wear away the bed – “abrasion”
Abrasion Features / chattermarksAbrasion Features / chattermarks
PolishPolish
• Typical of similar hardness (bed vs. tool) and fine load (~ sandpaper)
Glacial Abrasion in BedrockGlacial Abrasion in Bedrock
Source: Tom Bean
Glacier HydrologyGlacier Hydrology
Liquid water flows on, within,
and beneath glaciers
Subglacial ChannelsSubglacial Channels
• Eroded into bedrock
• Polar Glaciers– Pressure– Tools
Subglacial - Ice CavesSubglacial - Ice Caves
Ice CaveMendenhallGlacier, AK
Photographer:John Bortniak, 1991
NOAA Corps
Note Ice contact debris
To be continuedTo be continuedoutwash
terminus