Glaciers primarily pluck resistant rock types such as granite, gneiss, and schist. These types of rocks are more likely to fracture and break when exposed to the stresses of glacial movement, allowing the glacier to pluck and transport them as it flows.
Ice Sheets Ice Shelves Ice Caps Ice Streams/Outlet Glaciers Icefields Mountain Glaciers Valley Glaciers Piedmont Glaciers Cirque Glaciers Hanging Glaciers Tidewater Glaciers
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The two major types of glaciers are alpine glaciers and continental glaciers. Alpine glaciers, also known as mountain glaciers, are found in mountainous regions and flow down valleys, such as those in the Rocky Mountains and the Himalayas. Continental glaciers, or ice sheets, cover vast areas of land and are found in places like Antarctica and Greenland. Both types play significant roles in shaping landscapes and influencing global sea levels.
Glaciers accumulate sediment through various processes. As glaciers move, they pluck and erode rocks from the underlying bedrock, entraining them into the ice. Glaciers also grind and crush the rocks they come into contact with, generating glacial flour or fine-grained sediment. Additionally, glaciers can transport sediment that has been deposited on their surface by wind or landslides, adding to their load of sediment.
The two main types of glaciers are valley glaciers and continental glaciers. Valley glaciers, also known as alpine glaciers, form in mountainous regions and flow down through valleys, while continental glaciers, or ice sheets, cover vast areas of land and flow in all directions from their center. The key difference lies in their size and location: valley glaciers are smaller and confined to mountainous terrains, whereas continental glaciers are extensive, covering large portions of continents, such as Antarctica and Greenland. Both types are crucial in shaping landscapes and influencing global sea levels.
Rocks/Mountains.
Ice Sheets Ice Shelves Ice Caps Ice Streams/Outlet Glaciers Icefields Mountain Glaciers Valley Glaciers Piedmont Glaciers Cirque Glaciers Hanging Glaciers Tidewater Glaciers
Glaciers can move rocks, sediment, soil, and boulders as they travel outward or downward. Through a process called erosion, glaciers can bulldoze and pluck materials, transporting them to new locations.
Continental glaciers and valley glaciers are both types of glaciers that form from accumulated snowfall. They both flow under the influence of gravity, albeit in different directions. While continental glaciers cover vast areas like an ice sheet, valley glaciers are confined to mountain valleys and flow down through them.
canyons can be created
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There are more than three types of glaciers...but I believe you are looking for:Alpine Glacier (found on mountains)Valley GlaciersIce Sheet or Continental GlacierThe USGS has a great site dedicated to just types of glaciers....http://pubs.usgs.gov/of/2004/1216/glaciertypes/glaciertypes.html
There are 2 main types of glaciers, Continental is one, they float away from central regions. The second is alpine or valley which are the glaciers that flow down the valley from the mountain.
The two major types of glaciers are alpine glaciers and continental glaciers. Alpine glaciers, also known as mountain glaciers, are found in mountainous regions and flow down valleys, such as those in the Rocky Mountains and the Himalayas. Continental glaciers, or ice sheets, cover vast areas of land and are found in places like Antarctica and Greenland. Both types play significant roles in shaping landscapes and influencing global sea levels.
1s a glacier the other is a watermalon
All types of glaciers
Glaciers accumulate sediment through various processes. As glaciers move, they pluck and erode rocks from the underlying bedrock, entraining them into the ice. Glaciers also grind and crush the rocks they come into contact with, generating glacial flour or fine-grained sediment. Additionally, glaciers can transport sediment that has been deposited on their surface by wind or landslides, adding to their load of sediment.