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They are called drumlins.
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Are valley glaciers longer than continental glaciers?
No. Valley glaciers are a few miles to a few tens of miles long. Continental glaciers are hundreds to thousands of miles long.
Physical features of St Lawrence Lowlands?
The St. Lawrence Lowlands region in Canada is characterized by rolling hills, fertile farmland, and long, narrow river valleys. The landscape also includes numerous lakes and streams, as well as a mix of forests and wetlands. The region's topography was shaped by glaciers during the last ice age, resulting in a relatively flat and smooth terrain.
Do glaciers move material over a long distance?
Yes, glaciers can move material over long distances by picking up debris as they flow downhill. This material can range in size from tiny particles to large boulders, and as the glacier moves, it can deposit this material in different locations as it melts or retreats, forming moraines and other glacial landforms.
How can movement of glaciers cause lakes to form?
As glaciers move, they can carve out deep depressions in the land called cirques. When the glacier retreats or melts, these cirques can become filled with water, forming lakes. Glaciers can also create moraines, which are piles of debris that dam up valleys, creating lakes behind them.
What is a glaciers made of?
Glaciers are made of ice that has been formed a long time ago.
A glacier formed long smooth hills?
Glaciers form smooth hills by eroding and shaping the landscape as they move down a slope. The weight of the ice and the movement of the glacier over time smooth out the terrain beneath it, resulting in the formation of long smooth hills called drumlins.
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?
These long smooth hills are known as drumlins, which are created by the movement of glaciers during the process of glaciation. As a glacier advances, it reshapes the landscape by depositing and sculpting materials, forming these distinctive elongated landforms. Drumlins are typically found in regions that were once covered by ice sheets during the last Ice Age.
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.
Which agent of erosion was primarily responsible for forming the long U-shaped valleys in the Finger Lakes region of New York State?
ICE in the form of glaciers.
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 is the difference between kame and drumlin?
Drumlins are long smooth hills that are usaully found in groups. Kame are small cone shaped hills of sand and gravel.
A is a long place between hills or mountins?
The term for a long place between hills or mountains is a valley. Valleys are typically formed through erosion by water or glaciers over time, creating a low-lying area between higher elevations.
What is a low area of land between hills or mountains?
A valley is a low area of land between hills or mountains. It is often formed by erosion or the movement of glaciers or rivers over time. Valleys can be long and narrow or wide and open.
What is a long narrow area that lies between two mountains or hills?
A long narrow area that lies between two mountains or hills is called a valley. Valleys are formed by the erosion of water or glaciers over time. They are typically fertile and surrounded by higher land on either side.
Are valley glaciers longer than continental glaciers?
No. Valley glaciers are a few miles to a few tens of miles long. Continental glaciers are hundreds to thousands of miles long.
