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Chapter 12 Section 3 Part 1 Glacier Alpine Glacier Continental Glacier

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Presentation on theme: "Chapter 12 Section 3 Part 1 Glacier Alpine Glacier Continental Glacier"— Presentation transcript:

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2 Chapter 12 Section 3 Part 1 Glacier Alpine Glacier Continental Glacier
Horns Cirques Aretes Glaciers move by? U- Shaped Valleys

3 Glacier A large (enormous) mass of ice

4 Alpine Glacier Glaciers that form in mountainous area.

5 Continental Glacier Glaciers that are huge and spread across entire continents.

6 Horns Sharp, pyramid shaped peaks that form when three or more cirque glaciers erode “a” mountain.

7 Cirques Bowl-shaped depressions where glacial ice cuts back into mountain walls.

8 Aretes Jagged ridges that form between two or more cirques cutting into the same mountain.

9 Glaciers move by? The ice underneath the glacier melts but does not drain away thus it builds up beneath the ice. This buildup of melt-water decreases the friction between the glacier and the land below which causes the glacier to flow.

10 U-Shaped Valleys Forms when a glacier erodes a river valley from its original V shape to a U shape.


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