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WHAT IS A GLACIER?

Simply stated, a glacier is a large, slow-moving massive of ice. When there room many types of glaciers, they have the right to be split into 2 categories: alpine and continental. Alpine glaciers are discovered in a mountainous region and flow down valleys. Continent glaciers are dome-shaped glaciers that circulation away native a central region and also are largely unaffected through the land’s topography. The Greenland and also Antarctic ice cream sheets are instances of continental glaciers. Smaller sized masses of ice, referred to as ice caps, are also considered continental glaciers.

Alpine glaciers are further classified by your shape and also the surface they flow onto.

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A couple of types that alpine glaciers include:

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Above-freezing temperatures developed a meltwater currently on the Scott Glacier, Antarctica. Picture courtesy of Blue~Canoe (Flickr).