how we glacial horn is from
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Glaciers are compacted sheets of ice formed from multiple layers of snow accumulation. There are two basic types of glaciers. The first is a continental glacier, which expands over a wide area. The second is an alpine glacier, which only forms high in the mountains where the air stays cold.
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A horn is a glacial landform that develops when at least three glaciers carve away the surface of a single mountain top. This geological structure is characterized by steep sloping sides and a sharp-edged summit. Glaciers are massive layers of ice that gradually move over land areas, such as mountain valleys.
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