A glacier is a large, long-lasting river of ice that is formed on land and moves in response to gravity.

A glacier is formed by multi-year ice accretion in sloping terrain.

Glaciers can be found on every continent, including on the greater Australian continent.

Glaciers are more or less permanent bodies of ice and compacted snow that have become deep enough and heavy enough to flow under their own weight.

Glacier ice is the largest reservoir of freshwater on Earth, and second only to oceans as the largest reservoir of total water..

For more information about the topic Glacier, read the full article at Wikipedia.org, or see the following related articles:

Ice sheet — An Ice sheet is a mass of glacier ice that covers surrounding terrain and is greater than 50,000 square kilometers (19,305 square miles). The only ...  > read more

Ice shelf — An ice shelf is a thick, floating platform of ice that forms where a glacier or ice sheet flows down to a coastline and onto the ocean surface, ...  > read more

Sequence stratigraphy — Sequence stratigraphy is a relatively new branch of geology that attempts to link prehistoric sea-level changes to sedimentary deposits. The ...  > read more

Sediment — Sediment is any particulate matter that can be transported by fluid flow and which eventually is deposited as a layer of solid particles on the bed ...  > read more

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