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11
Glaciers and Glacial Erosion – GLY 2010- Summer 2012 -Lecture 20
• Ice Margin, Commonwealth Glacier, Antarctica
22
Glacier
• Moving mass of ice that forms when snowfall exceeds snowmelt over a long period of time
• Movement is downhill, due to gravity• Form at or above the snowline, the lowest
altitude at which snow commonly forms in the mountains
• As climates warm, the snowlines are expected to move higher in elevation, and glaciers to retreat
33
Types of Glaciers
44
Continental Ice Sheet
• Large ice masses that blanket a sizable part of a continent
• Ice may be kilometers thick, and movement is limited, occurring mainly in local areas or very slowly over time
5
Present Day Continental Ice
Sheets
• Greenland and Antarctica currently are occupied by continental ice sheets
66
Snowfield and Ice Cap
• Large mass of snow and ice on a flat surface, topped by recent snow
• Ice caps show little movement
• They occupy the tops of mountains
• Outlet glaciers may flow downward from the ice cap
77
Snowfield and Icecap Above Byrd Glacier, Antarctica
• Snow blankets and fills the valleys between the nunataks in the foreground
88
Fox Glacier, New Zealand
• Outlet glacier fed by Ice Cap
9
Mountain Valleys
• High in the mountains, snow may accumulate
• Glaciers are formed in stages Snow Firn Glacial Ice
1010
Snow
• Snow occurs in many forms, for example wet or dry
• Snow accumulates with a great deal of air trapped inside (you need to pack snow to make a decent snowball)
1111
Firn
• During the first summer following snowfall, some of the snow melts
• Meltwaters trickles downward, helping to compact the snow
• As winter approaches, resulting mass freezes together to form firn
1212
Formation of Glacier Ice
1313
Glacial Ice
• Repeated years of thaw/freeze cycles, and the weight of accumulated firn and snow, transform the lower layers to ice
• There are twelve known structural forms of water ice, at least half of which occur in nature
1414
Cirque Glacier
• Ice movement erodes a depression near the head of the glacier
• Glacier occupies the hole for a prolonged period, creating a bowl-shaped depression under the glacier
• After the cirque glacier melts, the depression remains
• Cirque may be filled with water, and is called a tarn lake, or it may be dry
1515
Cirque Glacier Photo
1616
Cirque
• Photo by Dr. Michael Hambrey
1717
Alpine or Valley Glacier• Confined by surrounding bedrock
highlands• Generally move down steep to very
steep surfaces• As cirque glaciers expand, they flow into
pre-existing stream cut channels, enlarging and changing the shape of these valleys
• Stream valleys have V-shaped profiles, whereas glacial valleys are U-shaped
1818
Valley Glacier Photo
Valley glacier flowing through mountains in Alaska
1919
Piedmont Glaciers• One or more valley
glaciers flowing from the confines of valley walls and spread out to form broad sheets
• Piedmont literally means foot of the mountain
• Malaspina Galcier (Alaska) is a classic large piedmont glacier that descends to tidewater from several mountain sources
2020
Tidewater Glacier, Alaska
• Tidewater glaciers flow into the sea, calving icebergs
2121
Calving Glacier Video
• Video was shot from a small ship July 1993 about one-half mile from the calving glacier by the instructor
© David Warburton, 2006
2222
Glacial Zones
• Accumulation
• Wastage (Ablation)
• Fracture
• Flowage
23
Glacial Anatomy
2424
Zone of Accumulation
• Snowfall exceeds snowmelt, on average over many years
• Upper portion of the glacier, at all depths
2525
Zone of Wastage (Ablation)
• Snowmelt exceeds snowfall, on average over many years
• Glacier will retreat unless gravitational movement of glacier downhill replaces glacial ice as fast as it melts
• 85% of world’s glaciers are currently retreating
2626
Glacial Cross-Section
2727
Zone of Fracture
• Upper surface of glacier is under little pressure
• Near toe of glacier, glacier moves faster, and pulls ahead of the ice uphill
• Tensional cracks develop (crevasses)
• Ice behaves as a brittle solid
2828
Zone of Flowage
• Lower part of the glacier, except near the toe, where glacier is thin
29
Glacial Advance and Retreat
3030
Crevasses, Exit Glacier, Alaska
• Extensional crevasses
• Note that they have the same shape as normal fault blocks
3131
Inside a Crevasse
• Photos by Kristina Ahlnas, University of Alaska
• Glacial ice is so blue because the dense ice of the glacier absorbs every other color of the spectrum except blue--so blue is what we see!
3232
Meltwater
• As glaciers melt, water trickles through the glacier, getting under it
• May form under-ice stream channels
• Channels form tunnels under the ice
• Tunnels emerge at snout of glacier
3333
Ice Cave
• Video of tidewater glacier, Prince William Sound, Alaska, July, 1993 © David Warburton, 2006
34
Work of Glaciers
• Like rivers, glaciers alter the landscape
• They may erode the landscape, but they also deposit large amounts of material
3535
Glacial Erosion
• Abrasion• Quarrying• U-shaped valleys• Hanging valleys• Cirque• Arěte• Horn• Roche moutonnée
3636
Abrasion
• Rock fragments imbedded in the base of the glacier scrap, and polish underlying rock, and in some cases create long striations (thin) or grooves (thicker) in the bedrock
• Stria and grooves indicate the direction of glacier movement
3737
Kelley's Island Grooves, Ohio
• Grooves may be of glacial or fluvial origin
• View is in direction of ice flow
3838
Glacial Striations
• Striations are smaller than grooves
3939
Quarrying
• Large masses of bedrock are lifted away from the bed after water from the glacier seeps into cracks and refreezes (frost wedging)
• Rock is incorporated into the glacier
4040
New Zealand Glacier
• Block to the right has been partially quarried
4141
U-Shaped Valleys
• Glacial ice follows previously cut stream valleys
• Stream valleys have V-shaped profiles
• Glacial erosion changes the shape to a U
4242
Glacial Valley Development I
• Typical, meandering V-shaped river valley
4343
Glacial Valley Development II
• Running water erodes and deepens the V - shape
4444
Glacial Valley Development III
• Glacier fills the river valley
• Channel is widened and straightened
4545
Glacial Valley Development IV
• Melting of glacier reveals a U – shaped valley
46
Glacial Trough
• The U-shaped glacial trough seen here is in Glacier National Park, Montana
47
Hanging Valleys
• Where tributary glaciers flow into the trunk glacier, they are often unable to erode as fast as the heavier trunk glacier
• When the ice melts, a hanging valley is left
48
Yosemite Valley
49
Waterfalls in a Hanging Valley
• Yosemite Falls occupies a glacial valley
5050
Cirque
• Cirques remain long after glaciers disappear
• May fill with water to become tarn lakes
• Bowl-shaped depression near the head of an alpine glacier
51
Tarn Lake
• Lake Ann, North Cascades National Park, is a tarn lake, occupying a cirque
5252
Arěte
• Knife-edged ridge of land, formed by parallel erosion of two alpine glaciers
• Another visible sign of previous glaciation
5353
Horn
• A three or four-sided mountain
• Cut by glaciers flowing off an isolated mountain in several directions
• Matterhorn in Switzerland is an excellent example
54
Roche Moutonnée
• From the French, meaning sheep rock
• Glacial abrasion smoothes the slope facing the oncoming ice
• Glacial quarrying plucks rocks from the opposite slope, steepening it
55
Liberty Cap, Yosemite
National Park
• Liberty Cap is a Roche moutonnée
5656
Alpine Glacial Erosion
5757
Glacial Deposition
• Till
• Drift
• Erratics
• Rock flour
5858
Glacial Till
• Deposits directly from glacial ice, with no sorting
• Light rocks are cobbles and pebbles
• Dark tan "matrix" is a mixture of sand, silt, and clay
5959
Formation of a Till Deposit
6060
Glacial Drift
• Includes glacial till, material dumped by glacier when melting
• Deposits from meltwater flowing out under a glacier
• Meltwater deposits are moderately to well-sorted
6161
Rock Flour
• Finally ground sediment produced under a glacier
• Meltwater streams carry the flour to lakes like this one in Alberta, Canada
6262
Moraines
• Masses of glacial drift left behind by a glacier
• Types of Moraine Terminal Lateral Medial
6363
Terminal Moraine
• Left at the end of a glaciers advance
• May act as a natural earth-fill dam
• Multiple terminal moraines may form a series of hills, running parallel to a ridge of mountains
6464
Moraine Formation
65
Terminal Moraine Formation
• Terminal moraine is a more common name for what they call end moraine
6666
Cape Cod From Space
• Cape Cod is a terminal moraine
• It marks the farthest point that the glaciers reached during the most recent "ice age" in North America
6767
Southern New England Moraines
6868
Lateral Moraine
Photo• Lateral
moraines are visible to either side of the glacier
Athabaska Glacier, Jasper National Park, Canada
6969
Medial Moraine Formation
70
Medial Moraine Photo
• Wrangell National Park, Alaska• Lateral moraines merging to form a complex of
medial moraines
7171
Glacier Junction, Southern Alps, New Zealand
7272
Twentymile Glacier, Alaska
• Two tributaries meet in a complex of medial moraines
7373
Outwash, Tasman Glacier, New Zealand
• Running water re-works the glacial gravel into the outwash
• Note the car in the lower center of the image
7474
Braided Outwash Channels, Toklat River, Alaska
• Braided channels are constantly changing
7575
Glacial Erratics
• Large glacial erratic• Ice is capable of carrying all sizes of material
76
Kettle Lakes
• Form when a large chunk of glacial ice is buried as glacier passes over
• Later, it melts, and forms a lake• Bear and Nymph Lakes, Rocky Mountain NP
7777
Drumlin
• Gently rounded hills formed by a massive ice sheet (thicker then a glacier) overriding a moraine
• Massive ice reshapes the moraine into elongated hills
Aerial View of drumlin field
7878
Drumlin Formation
7979
Esker Formation• Meltwater streams, flowing
within or under active glaciers deposit sand and gravel in curving channels
• When the glaciers melt the eskers are exposed as topographically positive features
• Long, linear features, sometimes in a network
8080
Esker Photo
• Esker visible as a sinuous ridge (arrow) in this aerial photo
81
Kame
• Formed when meltwater washes sediment into openings in a stagnant wasting glacier terminus
82
Glacial Features
8383
Glacial Subsidence and Rebound
• Continental ice sheets are so heavy they depress the rock under them (subsidence, due to isostasy)
• When the ice sheets melt, the land begins to slowly rise
• In the Canadian Shield region, the glacial rebound rate is about one foot per century
• Rebound is sometimes visible along lake-shores, where older beaches and wave-cut terraces are now considerably higher then the current lakeshore
84
Glacial Isostasy
8585
Crustal Depression
• Crust bulges on either side of glacier (isosastacy)
8686
Bulging Produces Raised Beaches
8787
Postglacial Effects
8888
Creation of Lake
Missoula
8989
Ice Dam
Breaks
9090
Bretz Floods
• The resulting floods, which recurred numerous times, are called Bretz floods after J Harlan Bretz, who first realized the significance of the gravel ridges meters high, and sometimes with wavelengths of a hundred meters, as Ripple Marks!
9191
Giant Ripple Marks
• Aerial view of giant ripple marks
9292
Catastrophic Flood
• Flooding occurred about 13,000 to 15,000 years ago
9393
Dry Falls
• Dry channels occur hundreds of feet above the present river channels, and former cataracts existed in many areas
• The best known of these, Dry Falls, is a 3.5 mile wide former cataract that dropped 400' over vertical cliffs of basalt
9494
Scablands
• Floods gouged and tore at the land removing surface cover
• Left masses of basaltic lava as remnants, like scabs on a wound
• Area is now called the channeled scablands
9595
Palouse Falls, Washington
• Note the very large channel behind the falls
96
Pluvial Lakes
• During glacial times, the climate was cooler, and evaporation rates were much lower in arid and semi-arid regions
• Many pluvial lakes formed from rainwater which did not evaporate
• Pluvial comes from Latin pluvia meaning rain