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28 Cards in this Set

  • Front
  • Back

Glacier

natural body of ice, originating on land, and undergoing movement that transports ice and rock from an area of accumulation to an area of disposal

Valley (alpine) glacier

mountainous areas


flows down valley from accumulation center at its head

ice sheet

larger scale


greenland


antarctica

morraine

ridge like pile of till

drumlins

low smoothly rounded elongated hill of till

outwash plains and valley trains

broad gently sloping sheet of outwash

kames

mound, knob, or ridge of stratified material

eskers

serpentine ridge of material

u-shaped valley

valley carved by glacial ice

arete

knife ridged edge

cirque

bowl shaped feature on the side of a mountain

hanging valley

glacial carved valley above another

horn

triangular peak created by two or more cirques

ice age

began 2 million and 3 million years ago


most glacial stages took place during pleistocene epoch

quarternary glaciations

2.58 mya to present


cenazoic

karoo glaciation

360-260 mya


late paleozoic

andean-saharan glaciation

450-420 mya


early middle paleozoic

cryogenian glaciation

800-635 mya


late precambrian

huronian glaciation

2400-2100 mya


mid precambrian

wisconsonian

85-11 kya


quaternary

illinoian

191-130 kya


quaternary

pre-illinoian

250-0.5 mya


quaternary

indirect effects of ice age

forced migration of animals and plants


changed stream courses


rebounding upward of the crust in former centers of accumulation


change in sea level


climate changes


pinedale

30,000 yr BP- 15,000 yr BP

bull-lake

200,000 yr BP to 130,000 yr BP

pre bull-lake

700,000 yr BP to 300,000 yr BP

causes of glaciation

plate tectonics


variations in earths orbit

milankovich hypothesis

shape of earths orbit varies


angle of earths axis changes


changes of climate over years associated with variations in geometry of earths orbit