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.
Two kinds of glaciers are valley glaciers and ice sheets. Valley glaciers are long, narrow glaciers that form in mountain valleys, while ice sheets are vast, continent-sized glaciers that cover large land areas. The main difference is in their size and location, with valley glaciers typically being smaller and found in mountainous regions, while ice sheets are much larger and exist in polar regions.
They form a huge mass that covers the entire continent?
Antarctica is a continental glacier. Alpine glaciers are a different type of glacier.
Land once covered by glaciers might have features such as moraines, glacial erratics, and u-shaped valleys, as well as evidence of glaciation in the form of striations and polished bedrock. In comparison, places that never had glaciers may have smoother topography and lack these distinctive glacial landforms.
Ice Sheets Ice Shelves Ice Caps Ice Streams/Outlet Glaciers Icefields Mountain Glaciers Valley Glaciers Piedmont Glaciers Cirque Glaciers Hanging Glaciers Tidewater Glaciers
It is valley and continental glaciers they are different because continental glaciers are the largest, and valley glaciers are on the top of mountain peaks.
Continental and Valley Glaciers.
Two kinds of glaciers are valley glaciers and ice sheets. Valley glaciers are long, narrow glaciers that form in mountain valleys, while ice sheets are vast, continent-sized glaciers that cover large land areas. The main difference is in their size and location, with valley glaciers typically being smaller and found in mountainous regions, while ice sheets are much larger and exist in polar regions.
Continental and Valley Glaciers.
Glaciers are ice sheets. There are 2 kinds of glaciers: alpine glaciers and continental glaciers. Alpine glaciers are formed when valleys above the snow line fill with ice and snow. Snow is compacted and gradually begins to flow downhill due to gravity. -Cham11
The two main types of glaciers are alpine glaciers, which form in mountainous regions and flow down valleys, and ice sheets, which are massive continental glaciers that cover large areas of land. Alpine glaciers are smaller and more common, while ice sheets are much larger and thicker.
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.
Two types of glaciers are valley glaciers, which flow down valleys, and ice sheets, which cover large land areas. Valley glaciers are narrower and are found in mountainous regions, while ice sheets are massive and cover extensive areas.
1. Mountain/Valley Glacier 2. Piedmont Glacier 3. Continental ice-sheets
Three different kinds of natural reservoirs are lakes, underground aquifers, and glaciers. Lakes store large amounts of water on the Earth's surface, aquifers are underground layers of rock that hold water, and glaciers are massive ice sheets that contain frozen water.
You must mean left begins by glaciers! Well there was big boulders for starters. And I think as they receded they left big hills and valleys called coulees! Hope this helps!
Yes, it can be. There are different kinds of lawyers across the country.