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Category:Cirque tarns: Difference between revisions

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These are small bodies of water usually formed in mountainous hollows or corries, known also as glacial cirques. These are bowl-shaped, ice-excavated rock basins, some of which are naturally deep, once carved by millions of tonnes of ice, erosion and weather. Cirques typically have three steep sides containing a headwall and two enclosing sidewalls, with a fourth being more open where a glacial till or moraine (rock debris that formed a dam) eventually enclosed and trapped the remaining ice.
These are small bodies of water usually formed in mountainous hollows or corries, known also as glacial cirques. These are bowl-shaped, ice-excavated rock basins, some of which are naturally deep, once carved by millions of tonnes of ice, erosion and weather. Cirques typically have three steep sides containing a headwall and two enclosing sidewalls, with a fourth being more open where a glacial till or moraine (rock debris that formed a dam) eventually enclosed and trapped the remaining ice.


[[Category:Tarns of the Lake District|03]]
[[Category:Tarns by type]]

Latest revision as of 19:12, 9 February 2024

These are small bodies of water usually formed in mountainous hollows or corries, known also as glacial cirques. These are bowl-shaped, ice-excavated rock basins, some of which are naturally deep, once carved by millions of tonnes of ice, erosion and weather. Cirques typically have three steep sides containing a headwall and two enclosing sidewalls, with a fourth being more open where a glacial till or moraine (rock debris that formed a dam) eventually enclosed and trapped the remaining ice.

Pages in category "Cirque tarns"

The following 4 pages are in this category, out of 4 total.

Media in category "Cirque tarns"

The following 8 files are in this category, out of 8 total.

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