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- B248844439ad81c215d0293f67f4c1438 hasDbXref "https://orcid.org/0000-0003-4808-4736" @default.
- B248844439ad81c215d0293f67f4c1438 type Axiom @default.
- B248844439ad81c215d0293f67f4c1438 annotatedProperty comment @default.
- B248844439ad81c215d0293f67f4c1438 annotatedSource ENVO_01001547 @default.
- B248844439ad81c215d0293f67f4c1438 annotatedTarget "Land ice is any part of the Earth's seasonal or perennial ice cover that has formed over land as the result, principally, of the freezing of precipitation; opposed to sea ice formed by the freezing of seawater. Thus, an iceberg or tabular iceberg is land ice as well as its parent glacier, ice sheet, or ice shelf. The two major concentrations of land ice are the ice sheets of Greenland and Antarctica. Glaciers and ice caps are the other important forms; however, some members of the glaciology community hold that glaciers (i.e. rock glaciers) need not have any ice." @default.