1s a glacier the other is a watermalon
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.
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.
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.
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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.
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.
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
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.
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.
Ice Sheets Ice Shelves Ice Caps Ice Streams/Outlet Glaciers Icefields Mountain Glaciers Valley Glaciers Piedmont Glaciers Cirque Glaciers Hanging Glaciers Tidewater Glaciers
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.