Chapter 17 Glaciers.

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Presentation transcript:

Chapter 17 Glaciers

1. Glacier A large mass of moving ice.

2. Alpine Glacier a narrow, wedge-shaped mass of ice that forms in a mountainous region and that is confined to a small area by surrounding topography; examples include valley glaciers, cirque glaciers, and piedmont glaciers.

3. Continental Glaciers massive sheet of ice that may cover millions of square kilometers, that may be thousands of meters thick, and that is not confined by surrounding topography.

4. Basal Slip process that causes the ice at the base of a glacier to melt and the glacier to slide.

5. Internal Plastic Flow the process by which glaciers flow slowly as grains of ice deform under pressure and slide over each other.

6. Crevasse in a glacier, a large crack or fissure that results from ice movement.

7. Cirque a deep and steep bowl-like depression produced by glacial erosion.

8. Arete a sharp, jagged ridge that forms between cirques.

9. Horn a sharp, pyramid-like peak that forms because of the erosion of cirques.

10. Erratic a large rock transported from a distant source by a glacier.

11. Glacial Drift rock material carried and deposited by glaciers.

12. Till unsorted rock material that is deposited directly by a melting glacier.

13. Moraine a landform that is made from unsorted sediments deposited by a glacier.

14. Kettle a bowl-like depression in a glacial drift deposit.

15. Esker a long, winding ridge of gravel and coarse sand deposited by glacial melt water streams.

16. Ice Age a long period of climatic cooling during which the continents are glaciated repeatedly.

17. Milankovitch Theory the theory that cyclical changes in Earth’s orbit and in the tilt of earth’s axis occur over thousands of years and cause climatic changes.