Key:glacier:type
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| Description |
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| Classification of the type of a glacier |
| Group: natural |
| Used on these elements |
| Documented values: 2 |
| Requires |
| Status: in use |
| Tools for this tag |
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The glacier:type key is used to provide additional information about the morphology and classification of a glacier tagged with natural=glacier. For the specific conventions of mapping glaciers and land ice in the Antarctic see also Antarctica/Tagging.
Values
The following values are in active use, for more proposed values see Proposed features/Glaciers tags
Values for glacier:type=*
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| value | definition | example | image | Taginfo |
=icecap |
Ice masses, dome shaped, with radial flow, raising above the surrounding terrain, see Wikipedia | The Vatnajökull glacier |
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=icefield |
Ice masses significantly covering underlying topography but constrained by mountains (in contrast to ice caps which lie on top of them), see Wikipedia | The Southern Patagonian Ice Field |
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=valley |
Valley glaciers are glaciers at the bottom of a single valley flowing downward | The Mer de Glace in the Mont Blanc massif |
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=mountain |
All smaller glaciers that do not fill a whole valley | The Tré-les-Eaux glacier | ||
=rock |
Flowing ice masses not originating from snow usually containing significant amounts of soil/rocks
Using this tag for |
Active rock glacier, Lange-Wand-Kar, Zillertal Alps, Tux main ridge | ||
=shelf |
Ice shelves are larger areas of thick, permanent glacier ice floating on the ocean | The Ross ice shelf |
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=ice_tongue |
A long and narrow sheet of ice projecting out from the end of a tidewater glacier over water | The Erebus ice tongue, Antarctica |
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_%2526_Mont_Blanc%252C_2010_July.jpg)




