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GES 101 Handout: Glaciers & Glaciation
Alpine Glaciers
Continental (Ice Sheet)
Ice Cap
Glacial Ice = recrystallized -(firn)
Glacial Movement = plastic flow + basal slip
Economy (Budget) of Glacier = balance between accumulation and ablation
Glacial Erosion
-abrasion
-plucking
Glacier Erosional Features:
arete (Alpine)
roches moutonnees (Continental)
horn (A)
paternoster lakes (A)
cirque (A)
U-shaped valleys (A,C)
tarn (A)
fiord (A,C)
bergschrund (A)
truncated spur (A)
col (A)
hanging valley (A)
groove (A,C)
chatter marks (A,C)
striations (A,C)
col (A)
Glacial Deposits -- Drift
Stratified drift
till
Glacial Depositional Features:
Till
Stratified Drift
erratics (C,A)
outwash plain (C)
moraines (C,A)
-lateral (A)
-medial (A) )
-end (terminal) (C,A)
-recessional (C,A)
-ground (C,A)
valley train (A)
drumlin (C)
kettle (C)
drumlin fields (C)
crevasse fillings (C,A)
Ice-contact deposits (C)
-kame
-kame terrace
-esker
-glacial delta
Alpine glaciation enhances the relief whereas continental glaciation subdues the relief.
Pleistocene = Ice Age
-15 to 20 major ice advances
-30% of Earth's surface imprinted
-N. Hemisphere 2x more ice than S. hemisphere
-Little Ice Age: 1550 - 1850
7 Prepleistocene glaciations
Cause of Glaciation
-no universally accepted theory
-lower T -require higher precipitation
-landmass @ high latitude
-need "triggers" to operate
-Volcanism
-Variations in sun's energy production
on 3 time scales
1. 106 years -plate tectonics
2. 105 years -Milankovitch Cycles
a) eccentricity of Earth's orbit (105,000 yrs.)
b) tilt of Earth's axis (41,000 yrs.)
c) precession of Earth's axis (23,000 yrs.)
-Major changes in oceanic circulation
3. 102 or 103 yrs.
Review Questions Glaciers and Glaciation
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