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Q: A glacier formed long smooth hills?
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What is a glacier formed long smooth hills?

A glacier formed long smooth hills are called drumlins. They are created when a glacier slides over the ground and reshapes the underlying material, depositing sediments and creating elongated, tear-shaped landforms. Drumlins are typically found in areas that were once covered by glaciers.


Glacier formed long smooth hills?

What kind of glacier forms when ice and snow build up in a mountain valley


What agent of erosion and deposition formed long island?

A glacier formed Long Island which came from Canada


What detail can tell you how a moraine is different from a ordinary hill?

Moraines are long, low hills formed by materials made by a glacier. A moraine contains rocks, sand, and clay. if you dig into a moraine, you find these things deposited together. You do not find them together in hills


What is formed in a shape of a long low area between hills or mountains?

What is formed in the shape of a long, low land area between hills or mountains


What is formed in the shape of a long low land between hills or mountains?

What is formed in the shape of a long, low land area between hills or mountains


What is formed in a shape of a long low land area between hills or mountains?

What is formed in the shape of a long, low land area between hills or mountains


What is formed in the shape of a long low land area between hills or mountains?

What is formed in the shape of a long, low land area between hills or mountains


Is long ridge formed by boulders carried and deposited by a glacier moraine?

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The glacial features that occur in swarms of long smooth canoe-shaped hills are?

drumlins


The glacial features that occur in swarms of long and smooth canoe shaped hills are?

drumlins


What are The glacial features that occur in swarms of long and smooth canoe-shaped hills?

The glacial features that occur in swarms of long and smooth canoe-shaped hills are called drumlins. Drumlins are typically formed under moving glaciers and indicate the direction of ice flow. They are important indicators of past glacial activity and can be found in large numbers clustered together in areas that were once covered by ice sheets.