A streamlined asymmetrical hill composed of till is called a drumlin. Drumlins are formed by glacial activity, with their shape indicating the direction of the glacier's movement. They typically have a steep side facing the glacier and a more gentle slope on the opposite side.
drumlin
A streamlined asymmetrical hill is commonly referred to as a "mound" or "knoll." In geological terms, it may also be described as an "elongated hill" or "ridge," particularly if it has a more pronounced slope on one side, which allows it to efficiently direct wind or water flow. The asymmetrical shape often results from erosional processes or glacial activity.
A low hill formed when a glacier overruns and deposits moraine is called a drumlin. Drumlins are elongated, streamlined hills that indicate the direction of glacial movement. They are composed of glacial till and can vary in size, typically appearing in groups known as drumlin fields. Their formation results from the reshaping of existing moraines by the advancing glacier.
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The crest of a hill is called the summit or peak.
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A very large hill is called a mountain.
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it is a hill
The highest point of a hill is called its summit.
An area of hills is called a hill range or hill country.