Physical Geography by Alan Arbogast Chapter 17
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Transcript of Physical Geography by Alan Arbogast Chapter 17
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Physical Geographyby Alan Arbogast
Chapter 17
Glacial Geomorphology: Processes & Landforms
Lawrence McGlinnDepartment of GeographyState University of New York - New Paltz
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History of Glaciation
• As early as 2.3 B years ago, ice covered much of Earth, and off and on since then
• Most important Ice Age was Pleistocene Epoch, 1.8 M years ago till 10K years ago
• Glacial – period when glaciers expand from poles – cooler temps, lower sea level,
• Interglacial – period when glaciers recede: warmer temps, higher sea level
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Pleistocene Glaciations
• Named for southern extent of ice sheet in North America– Nebraskan – 1 million yrs ago– Kansan – 625 K yrs ago– Illinoisan – 300 K yrs ago– Wisconsin – 35 K to 10 K yrs ago
• Laurentide Ice Sheet – eastern North America
• Cordilleran Ice Sheet – western North America
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Maximum Extent of Pleistocene Glaciation
30% of earth’s surface covered by ice sheets(Only 11% coverage today)
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Oxygen Isotopes
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Evidence of More Glaciations?• Ice core samples suggest
more than the known 4 glaciations – show more cool, glacial periods
• Oxygen isotopes O-16 & O-18 both in water, but O-18 evaporates more in warmer climate, so ratio of O-16 to O-18 in ice cores can indicate relative warmth of climates over 1 million yrs ago!
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Causes of Glaciation• Summer temp (melting) is key to glaciation
• Possible Factors:1. Variations in solar radiation (dust, sunspots…)
2. Reduced carbon dioxide (escaping heat)
3. Increased volcanic activity (reflective dust)
4. Variations in Earth-Sun geometry (axial tilt, shape of orbit, rotation)
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Milankovitch Theory• Dominant theory of causes of glaciation,
based on Earth-Sun geometry: • Orbital eccentricity – strongly elliptical orbit
puts Earth farthest from Sun in summer, cooling it
• Tilt obliquity – Earth’s tilt varies from 22.1º to 24.5º - less tilt means lower angle Sun and less insolation at poles, thus cooler summers
• Orbital precession – wobbles of Earth’s axis - North Pole may point toward Sun at farthest point of orbit, creating a cool summer
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Milankovitch TheoryOrbital Eccentricity Axial Tilt Orbital Precession
When three factors coincide, high probability of glaciation
Glacial Geomorphology: Processes and Landforms
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Climate Change and Glaciers
• Since mid-1800s glaciers have been receding, both alpine and continental
• Alps, Parts of Andes, Mt. Kilimanjaro melting
• Thousands of sq miles of Antarctica & Greenland ice sheet lost over last 30 years due to warming
• Melting area of Greenland has increased rapidly since early 1990s
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Climate Change and Glaciers
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Climate Change and Glaciers
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Periglacial Processes and Landscapes
• In near-glacial environments – constant freeze/thaw cycle effects on landscape
• Permafrost – ground that is permanently frozen– Continuous – poleward of -7ºC mean annual
isotherm – all surfaces frozen exp under water – avg 400 m thick, up to 1000 m thick
– Discontinuous – poleward of -1ºC mean annual isotherm – thinner than continuous, esp. on south facing slopes
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Extent of Permafrost
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Permafrost Processes• Active Layer – soil that melts & refreezes
daily or seasonally – as thin as 10 cm in continuous permafrost, up to 2 m thick in discontinous
• Dramatic warming in arctic is making active layer much thicker & releasing tons of CO2
• Talik – body of unfrozen ground within permafrost, e.g. under a lake, important for movement of groundwater
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Periglacial Landscape(Cross Section)
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Ground Ice• Ground Ice – distinct zones of frozen water
within the ground – variable amts of water
• As these areas freeze & thaw, expand & contract, they cause physical weathering
• Ice Wedge – water enters crack in active layer
• Pingo – surface bulges because of ice under pressure below
• Patterned Ground – land broken into polygons as frost pushes coarser material to surface
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Ground Ice LandformsIce Wedge Pingo
Patterned Ground