Tarn (lake)

Source: Wikipedia, the free encyclopedia.
Glacial action forming a cirque which may host a tarn

A tarn (or corrie loch) is a mountain lake, pond or pool, formed in a cirque excavated by a glacier. A moraine may form a natural dam below a tarn.[1]

Etymology

Verdi Lake in the Ruby Mountains of Nevada

The word is

Scandinavian languages
, a tjern or tjørn (both Norwegian) or tjärn or tärn (both Swedish) is a small natural lake, often in a forest or with vegetation closely surrounding it or growing into the tarn.

The specific technical use for a body of water in a glacial corrie comes from high number of tarns found in corries in the Lake District, an upland area in Cumbria.[4] Nonetheless, there are many more bodies of water called 'tarn' in the Lake District than actually fit this technical use.

Formation

Tarns are the result of small glaciers called

glacial till, which forms the lip, threshold or sill,[7]
from which either a stream or glacier will flow away from the cirque.

Tarns form from the melting of the cirque glacier. They may either be seasonal features as supraglacial lakes, or permanent features which form in the hollows left by cirques in formerly glaciated areas. [4]

Gallery

See also

References

  1. ^ "Illustrated Glossary of Alpine Glacial Landforms". Archived from the original on 2007-08-11. Retrieved 2007-08-05.
  2. ^ "Tarn Dipping blog. List of the 197 Tarns in the Lake District, Cumbria". 15 March 2016.
  3. ^ "Fresh Water Tarns". Cumbria Wildlife Trust. Archived from the original on 2007-06-27. Retrieved 2007-08-05.
  4. ^ .
  5. .
  6. .
  7. . Retrieved 2010-01-24.

External links

  • Media related to Tarn (lake) at Wikimedia Commons
  • The dictionary definition of tarn at Wiktionary