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Glaciers and the Great Ice Ages

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Why did the climate change so drastically and repeadedly? Climate change and variations in Earth's orbit ... Precession: cyclic change in'wobble' of the axis ... – PowerPoint PPT presentation

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Title: Glaciers and the Great Ice Ages


1
Glaciers and the Great Ice Ages
2
Pleistocene Epochthe Great Ice Ages
  • 2.0 Ma to 10,000 years ago
  • Four (or more) distinct episodes expansion and
    melting of ice sheets (continental glaciers)

3
Why did the climate change so drastically and
repeadedly?
  • Climate change and variations in Earths orbit
  • Eccentricity elliptical to nearly circular
    cycles
  • Obliquity cyclic changes in tilt of axis
  • Precession cyclic change inwobble of the axis
  • Variations affect amount and distribution of
    solar energy received by Earth

4
How does a glacier form?
  • Cold climate is necessary
  • Annual snow accumulation is greater than annual
    rate of melting
  • Snow builds up over time
  • Snow recrystallizes to ice

5
Glacial Flow
  • Ice begins to flow (plastic deformation) under
    the influence of gravity
  • Glacier mass of flowing ice

6
  • Glaciers are dynamic
  • Flow is constant
  • Some parts of glacier are melting
  • Rate of accumulation vs. rate of melting
    determines if glacier will advance or if end of
    glacier will melt back (glaciers never flow
    backwards)

7
Glaciers and Landscapes
  • Flowing ice picks up sediment, soil, etc.
  • Breaks loose pieces of bedrock
  • Modifies landscape by erosion and deposition

8
Erosion by Glaciers
  • Striations scratchmarks made as ice drags
    rocks across bedrock

9
Erosion by Glaciers
  • Modifies V shaped river valleys to a U shape

10
Deposition by Glaciers
  • Erratics pieces of exotic rock left by
    glacier
  • Till unsorted, unstratified sediments dumped by
    ice
  • Outwash sorted and stratified sand and gravel
    deposited by meltwater

11
Deposition by glaciers
  • Lacustrine sediments
  • Lakes form between melting edge of ice and
    obstructions (often deposits of till)
  • Fine silt and clay settle to the bottom in calm
    water
  • Clay may be used in pottery and brick making
  • If lakes drain or fill with sediment
  • bogs and swamps ecologically important wetlands
  • Water-logged lacustrine sediments may cause
    tilting and sinking of buildings constructed on
    them

12
Glaciers and Landforms
  • Characteristic landforms
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