Tarn (lake)
"Tarns" redirects here. For the hamlet in England, see Tarns, Cumbria.
A tarn (or corrie loch) is a mountain lake or pool, formed in a cirque excavated by a glacier. It is formed when either rain or river water fills the cirque. A moraine may form a natural dam below a tarn.[1]
Etymology
The word is derived from the Old Norse word tjörn meaning pond. Its more specific use as a mountain lake emerges as it is the commonly used term for all ponds in the upland areas of Northern England. Here, it retains a broader use, referring to any small lake or pond, regardless of its location and origin (e.g. Talkin Tarn).[2]
In Scandinavian languages, a tjern or tjärn, tärn or tjørn is a small natural lake, often in a forest or with vegetation closely surrounding it or actually growing into the tarn.
Gallery
- Veľké Hincovo, the largest and deepest tarn in Slovakia
- Lousy Lake (tarn) in N.Cascades National Park, Pickett Range, Washington
See also
References
Wikimedia Commons has media related to Tarn (lake). |
Look up tarn in Wiktionary, the free dictionary. |
- ↑ "Illustrated Glossary of Alpine Glacial Landforms". Retrieved 2007-08-05.
- ↑ "Fresh Water Tarns". Cumbria Wildlife Trust. Archived from the original on 2007-06-27. Retrieved 2007-08-05.
This article is issued from Wikipedia - version of the 9/3/2016. The text is available under the Creative Commons Attribution/Share Alike but additional terms may apply for the media files.