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eskers and drumlins are features associated with eskers and drumlins are features associated with

Drumlin a. It increases. What typically happens to global sea level during an ice age? Broken ridges or un-assorted depositions looking like hump in a till plain. Some of the other features associated with glacier erosion in alpine regions are cirques, horns, and arêtes (Figure 10af-3). Ground moraine with drumlins and till-covered bedrock rises (Fig. Which of the following features are typical of both alpine and continental glaciation ? D 29 Which of the following features is a result of glacial deposition A) erratic B) arête C) cirque D) horn A 30 Which features form by deposition from glacial meltwater? List four effects of Ice Age glaciers aside from the formation of major erosional and depositional features. 15. The esker (Ir. a. Kettles, kames, and eskers b. Moraines, erratics, and drumlins c. Tarns, hanging valleys, and horns d. Roches moutonnées, arêtes, and fjords. The term esker is derived from the Irish word eiscir (Old Irish: escir), which means "ridge or elevation, especially one separating two plains or depressed surfaces". - Drumlins, Eskers, Kames, Kettle Holes. These would have been part of the debris that was carried along and then accumulated under the ancient glacier. Briefly describe the following glacial features associated with ice sheets: terminal moraine, kettle, drumlin, outwash plain, esker, and kame. b. - Large amount of the water trapped by the glaciers from the water cycle. The eskers resemble the features of an embankment and are often used for making roads. The Irish word was and is used particularly to describe long sinuous ridges, which are now known to be deposits of fluvio-glacial material. Changes to the valleys and rivers are contributed by the glaciers, obliterating the former valleys and streams. running along a glacier in a till plain. In low-lying, boggy terrain these snaking ridges dominate the terrain, providing vantage points and dry route ways. It decreases. The long axis of the drumlin indicates the direction in which the glacier was moving. Esker. Winding ridge of un-assorted depositions of rock, gravel, clay etc. For most alpine glaciers, cirques are the areas in the alpine valleys where snow first accumulated and was modified into glacial ice. Drumlins and eskers are found in glacial areas. They vary in length from a fraction of a mile to scores of miles, and in height from a few feet up to several hundred and more feet. Briefly describe the following glacial features associated with mountain glaciers: cirque, arete, horn, hanging valley, lateral moraine, medial moraine. 22) comprise most of the area up-ice from the front of both lobes. Eskers on paleo-ice-sheet beds are more abundant in areas of crystalline bedrock with thin coverings of surficial sediment than in areas of thick deformable sediment e.g., 9,4.This is because meltwater flowing at the bed is more likely to incise upwards into the ice to form an R-channel where the bed is hard; where the bed is deformable, meltwater is more likely to incise downwards 10. 2-3.2 Glacial History In the last approximately one million years, there have been four glacial advances across central and eastern North America. They can be 1 km long and 500 metres wide, often occurring in groups. Drumlin An elongated hill of glacial till formed by the re-advance of a glacier over existing till deposits. Eiscir) is one of the most striking landforms of fluvioglacial deposition. List four depositional features other than moraines. Drumlins are hills made of glacial sediment and till, while eskers are long ridges of glacial drift. More than a thousand eskers have been found in Michigan. Cirques are the bowl shaped depressions found at the head of glacial valleys. Kame Terraces. Most eskers are on till plains although some are known to cut through moraines and even cross drumlins. The long axis of a drumlin is aligned with the direction of glacier movement. These units are: ground moraine and drumlins, stratified drift, end moraine and stagnate-ice or dead-ice moraine, and special features such as moulin kames, eskers, and crevasse fills. A) striations and erratics B) drumlins and cirques ... drumlins B) striations C) eskers D) kettles . Esker: A long narrow ridge, often sinuous, composed of stratified sediment and marking the former location of a glacial tunnel. 14. Drumlins are elongated hills of glacial deposits.

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