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Section 15.2 Glacial Movements and Erosion

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Presentation on theme: "Section 15.2 Glacial Movements and Erosion"— Presentation transcript:

1 Section 15.2 Glacial Movements and Erosion

2 How do glaciers move? What are some reasons why glaciers move?
Heavy snow fall Steep slopes Temperature increase/summer What slows glaciers down? Friction

3 Slip and slide on a layer of water (friction)

4 2 main types of glacial movement
1. Basal slip 2. Plastic flow

5 1. Basal slip Basal slip = immense weight of the glacier puts pressure on the bottom causing grains of ice to partially melt creates a slushy layer glacier “slips and slides” on the slush

6 2. Plastic Flow Due to pressure (weight) of snow above
Grains of ice actually deform and flatten Ice in the interior of the glacier moves forward like a plastic putty

7

8 As a glacier moves… Crevasses form
cracks in the glacier due to increased speed often associated with a steep incline

9 What happens at the end of a glacier?
If the glacier is below the snowline… ice front -the ice starts to melt, signifying the end of the glacier

10 What happens at the end of a glacier?
If the snowline is at sea level… calving -large pieces of glacier break off of the front (icebergs!)

11 How do glaciers cause erosion?
Till -breaking down boulders, rocks, pebbles, and small grains into smaller pieces Moraine -the accumulation of till

12 The Ransom Moraine is a large moraine that cuts diagonally across Kendall County

13 Aftermath of glaciers Striations -occur when the glacial load scratches parallel groves in the underlying bedrock Roches mountonnees a distinct pattern of rocks that are often exposed that bare a resemblance to a flock of sheep. “sheep rocks”


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