Glacial Topography.pptx
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This document discusses glacial landforms created by erosion and deposition. It describes erosional landforms such as cirques, glacial troughs, hanging valleys, and fjords that are formed by glacial erosion. Depositional landforms created by glaciers depositing debris include outwash plains, eskers, kame terraces, drumlins, and various types of moraines. The document examines how glaciers shape the landscape and leave behind distinctive erosional and depositional features when they melt.
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- 1. Glacial Topography by Dr. R. Prasad (Department of Geography) Dr. Bhim Rao Ambedkar College
- 3. Types of glaciers • Continental • Ice caps • Highland glaciers
- 5. Examples of a Medial Moraine, End Moraine, and Terminal Moraines.
- 6. Erosional Landforms Cirque/Corrie Glacial Trough or U-Shaped Valley Hanging Valley Arete Horn Fjord
- 7. Cirque/Corrie: Steep-sided hollow at the head of a valley formed by glacial erosion
- 8. Cirque Lake
- 9. Glacial Trough: Relatively straight, flat-bottomed, deeper, and steep-sided valley formed by glacial erosion
- 11. Hanging Valley: Tributary valley that is higher than the main valley
- 13. Arete: Narrow ridge of rock which separates two valleys
- 15. Horn: Two or more glaciers erode the sides of a mountain peak
- 16. Fjord: Long, narrow sea inlet with steep sides, created by a glacial erosion
- 17. Depositional Landforms Outwash Plain Esker Kame Terraces Drumlin Moraine Lateral Moraine Medial Moraine Terminal Moraine Ground Moraine
- 18. Outwash Plain: Formed of glacial sediments deposited by meltwater
- 19. Esker: Long, winding ridge of unsorted sand and gravel
- 20. Kame Terraces: Broken ridges or unsorted depositions
- 21. Drumlin: Elongated hill in the shape of an inverted spoon
- 22. Moraine: Unconsolidated glacial debris
- 24. The same landscape filled with valley glaciers
- 25. When the glaciers retreat, the new landscape is unveiled.