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|style="padding:0 0.9em 0 0;" | [[File: | |style="padding:0 0.9em 0 0;" | [[File:Antarctic Sound-2016-Iceberg 02.jpg|300px]] | ||
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An '''[[iceberg]]''' is a large piece of freshwater [[ice]] that has broken off a [[glacier]] or an [[Ice-shelf|ice shelf]] and is floating freely in open water. It may subsequently become frozen into [[pack ice]] (one form of sea ice). As it drifts into shallower waters, it may come into contact with the seabed, a process referred to as seabed gouging by ice. About 90% of an iceberg is below the surface of the water. | |||
In addition to size classification, icebergs can be classified on the basis of their shape. The two basic types of iceberg forms are tabular and non-tabular. Tabular icebergs have steep sides and a flat top, much like a plateau, with a length-to-height ratio of more than 5:1. This type of iceberg, also known as an ice island, can be quite large, as in the case of Pobeda Ice Island. [[Antarctic]] icebergs formed by breaking off from an [[ice-shelf|ice shelf]], such as the [[Ross Ice Shelf]] or [[Filchner-Ronne Ice Shelf]], are typically tabular. The largest icebergs in the world are formed this way. | |||
<p><small>Photographer: Andrew Shiva</small></p> | |||
<p><small>Photographer: | |||
[[:Category:Images|'''(More Featured Images)''']] | [[:Category:Images|'''(More Featured Images)''']] | ||
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