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GLACIERS AND GLACIATION II. Topics. Glacial landforms Glacial sedimentation Permafrost Glacial lakes Glaciations and global climate. Terminal moraine. Courtesy Gerald Osborn. Other Glacial Landforms . Drumlins- Elongated hills of glacial till Point down-glacier Eskers
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Topics • Glacial landforms • Glacial sedimentation • Permafrost • Glacial lakes • Glaciations and global climate
Terminal moraine Courtesy Gerald Osborn
Other Glacial Landforms • Drumlins- • Elongated hills of glacial till • Point down-glacier • Eskers • Sinuous ridges of stratified till • Form in tunnels under the ice sheet • Some times 100km long or more
Permafrost • Frozen ground • Found in Arctic • North America • Russia • Formed during last ice age • More than 1000 m deep in places • Global warming -> melting of permafrost
Distribution of permafrost in the northern hemisphere Fig. 12.29
Lateral variations in permafrost in Siberia Fig. 12.30
Glacial Lakes • Pluvial Lakes- • Due to wetter climate • Examples: Lake Bonneville, Death Valley • Lake Bonneville flood into Snake River Canyon • Proglacial Lakes • In front of the glacial sheet • Ice dammed lakes • Examples: Great Lakes, Lake Missoula
Lake Bonneville Flood • The lake was up to 1000 feet deep • A ridge on the north side gave way • Peak flow = 33 million cubic feet/second • 33 MCF would fill a tanker train 165 miles long • A raft would move at 75 mph on a wave 300 ft high • Flood left behind giant ripples
Glacial ages • Northern Europe & North America heavily glaciated • Peak of glaciation 18,000 years ago • Ended about 10,000 • We are still in the cold part of the climate cycle • Episodic climate changes • At peak glaciation • Average global temperature only 5 degrees colder
Effects of Past Glaciation • Glacial ages • Direct effects in North America • Scoured much of Canada • Cut Great Lakes • Deposited till & flattened Midwest • Extensive alpine glaciation in mountains • Allowed Natives to walk from Siberia
Effects of Glacial Ages • Indirect effects • Pluvial lakes • Lowering of sea level • Fiord • Crustal rebound
Causes for glaciation • Astronomical • Variations in solar radiation • Atmospheric changes • Tectonic causes
Causes for glaciation • Astronomical (Milankovitch cycles) • Eccentricity of orbit (100,000 yr cycle) • Wobble of rotation axis (41,000 yr cycle) • Precession of equinox (23,000 yr cycle) • Variations in solar radiation
Causes for glaciation • Atmospheric changes • CO2 (Greenhouse effect) • Volcanic ash • Tectonic causes • Continents near the poles • Oceanic circulation patterns
Causes for glaciation • Tectonic causes • Continents near the poles • Oceanic circulation patterns
Retreating Rhone Glacier S. C. Porter