Calving of a glacier is the process by which ice blocks break away from the front end of a glacier, under the influence of gravity (if the glacier is above water and does not touch it) or buoyancy (if the front end of the glacier is below the water surface).

Lumps of ice that calve off the front end of the glacier can have very different sizes – from small slivers of ice to giant icebergs, which can have a surface area of up to hundreds of square kilometres. Solid ice that  detaches from the front end of a glacier located at the surface of the water float away as icebergs or growlers (sort of ice rubble).

The water on the front end of a glacier causes the ice in the glacier to disintegrate into smaller parts. This disintegration simultaneously causes waves to form on the surface of the water. Such waves can pose a threat to vessels, if calving happens close by.

Calving is a very important factor in the normal retreat of glaciers as they flow towards the sea. The point at which a glacier no longer flows on land but starts to flow out over the water is known as the grounding line.

Calving of Hans Glacier ice cliff (Hornsund, Svalbard)

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