Glaciers and Climate Change (Ch. 14)
Glacial deposits: till and stratified drift
Till: transported
and deposited by ice: poorly sorted and not rounded
Landforms composed of till:
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Ground moraine: till deposited underneath glacier.
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Drumlins: till reshaped into elongated hills
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Moraines:
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Lateral: at edges
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Medial: formed when two glaciers join
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End: at front of glacier
Stratified drift: deposited
by water, sorted and layered
Landforms composed of stratified
drift:
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Kames (round hills) and Eskers (sinuous ridges): deposited in meltwater
tunnels
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Outwash: Stream-deposited sediment
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Kettle: depression formed by melting of ice blocks
Last glacial age peaked 20,000 years ago, covered 30% of earth
Indirect Effects:
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pluvial lakes: from higher rainfall, lower T. Example: Lake Bonneville
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large quantities of meltwater filled lakes, streams
catastrophic floods Example: Channeled Scablands
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Sea Level was 130 m lower
As sea-level rose: glacial valleys were drowned, creating fjords
Previous Glacial Ages have occurred ~ every 100,000 years for 600,000
years
When dinosaurs lived, the earth was up to 15°F warmer than today.
Why does the earth’s temperature change?
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Milankovitch theory: variations in the Earth’s orbit and tilt affect solar
radiation
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Tectonics (position of continents)
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Changes in the atmosphere
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volcanoes or meteorite impacts could increase dust and sulfates, cool Earth
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Greenhouse Effect: gases in atmosphere keep Earth warm
Global Warming
Humans have added CO2 (and other gases) to the atmosphere
by burning coal and oil.
Global temperatures has risen 0.5 to 1° F
Sea level has risen 4 to 10 inches
Difficulty: separating effects due to CO2 from natural climate
trends
Predictions for 2100:
2 to 6°F temperature increase
6 to 38 inch sea-level increase
Impacts:
severe weather (heat waves, hurricanes, floods, droughts)
flooding of coastal areas, saltwater intrusion
ecological: shift in habitats
Over the next few centuries?
1 to 5% chance that W. Antarctic Ice Sheet becomes unstable, raise
sea-level 20 feet