Continental Glaciers Valley
Glaciers
Valley Glacier
Erosion
Valley Glacier
Erosion Features
Valley glaciers are found in mountain regions all around the world. They begin at the top of the mountain where it is snows all year and the temperatures are always below freezing. The glacier is so heavy at the top that it begins to move slowly down the mountain. The glacial ice builds up year after year until the ice is so thick that the bottom layer melts a little and mixes with dirt and soil. This forms a slick layer that makes it easy for the glacier to move as gravity pulls it from the top of the mountain. As gravity pulls the glacier slowly down the mountain, new snow falls to replace the glacier at the top of the mountain. As a glacier moves down the valley it scapes along the sides and bottom of the valley that is already there. It picks up boulders and sediments and takes them down the mountain. Valley glaciers cause a lot of damage to the land that it passes over and makes many new landforms.

 

 
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