Drumlins are formed by glacial movement; eskers from streams under the glacier.
Kame is a hill or mound of sand and gravel formed by glacial meltwater, whereas an esker is a long winding ridge of material deposited by a stream flowing beneath a glacier. Essentially, the key difference lies in their shape and formation process within a glacial environment.
Since the esker was deposited in a flowing water regime, I would not expect to find many fine clays there. And I would not expect to find any large boulders, >1m in an esker. The moraine on the other hand will have parts that have been formed by rocks grinding each other in a comparatively waterless regime. So it will have lots of fine clays. Boulders >>1m could even be a feature of a moraine.
An esker is formed by the deposition of sand and gravel carried by meltwater streams flowing within or on top of glaciers. As the glacier melts, the sediment is deposited in ridges or sinuous mounds along the path of the flowing water, creating a long, narrow ridge known as an esker.
A long winding ridge made from deposits of sand and gravel is called an esker. Eskers are formed by the melting of glaciers and the deposition of sediment as the flowing water carries and deposits material in a sinuous ridge-like form.
A drumlin is a long, narrow hill formed by glacial drift. Drumlins are typically elongated in the direction of glacier movement and have a smoothed, rounded shape.
Drumlins are long smooth hills that are usaully found in groups. Kame are small cone shaped hills of sand and gravel.
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drumlin
Drumlin Heights Consolidated School was created in 2001.
The difference is that a Roche Moutonée is an erosional landform whereas a drumlin is a depositional one. A Roche Moutonée is formed by a glacier moving over the top of the rock plucking one side giving it a jagged edge and abrading the other side giving it a smooth edge. A drumlin on the other hand is deposited by the glacier and are streamlined into elongated hills by the glacier. Drumlins are unknown as to how they are formed with there being many theories as to how they are made but one I feel sounds likely is that when it melts out of the subglacial layers it is lodged on the floor and is shaped by the glacier into the shape. Hope this helps you!
egg shaped
Kame is a hill or mound of sand and gravel formed by glacial meltwater, whereas an esker is a long winding ridge of material deposited by a stream flowing beneath a glacier. Essentially, the key difference lies in their shape and formation process within a glacial environment.
A glacial ridge could be defined as several things:- An arête: a steep-sided ridge between two valleys that were formed by glaciers.- corries: formed through glacier action.- eskir/esker: a ridge of sand and gravel deposited by glacial movement.- drumlin: an elongated hill caused by the streamlined movement of glacial ice sheets across rock-strewn lowlands.serac - pinnacles of ice formed by the intersection of crevasses in a glacier
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an esker is formed by a Glacier
A drumlin.
Drumlins are found on a hill