A temperate glacier remains at melting point from surface to base throughout the year. A polar glacier always remains below freezing point.
Continental and Valley 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.
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.
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 two syllables in the word 'glaciers'.
They generally form mountains.
canyon valley and glaciers bro
Wind can shape alredy present rocks, and glaciers normally form fjords.
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