Sunbiggin Tarn
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Sunbiggin Tarn
Sunbiggin Tarn is a tarn near Sunbiggin in Cumbria. It is in a Site of Special Scientific Interest (SSSI) which also includes the surrounding moorland and limestone pavement of Little Asby Scar. Site history Site location and designation Significant site content Flora common bent, mother of thyme, sheep fescue, Sesleria albicans, Galium sterneri grassland Calluna vulgaris Erica cinerea, Vaccinium myrtillus heath Scirpus cespitosus, Erica tetralix wet heath Carex elata, Equisetum fluviatile, Cladium mariscus, Carex rostrata, Potentilla palustris, Phragmites australis swamp, sedge and reed-beds Fauna black-headed gull, gadwall, little grebe, osprey, starling, water rail, wigeon Geyer's whorl snail Geology Dinantian, Karst Karst is a topography formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. It has also been documented for more weathering-resistant ...
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Tarn (lake)
A tarn (or corrie loch) is a Proglacial lake, proglacial mountain lake, pond or pool, formed in a cirque excavated by a glacier. A moraine may form a natural dam below a tarn. Etymology The word is toponymy, derived from the Old Norse word ''tjörn'' ("a small mountain lake without tributaries") meaning pond. In parts of Northern England - predominantly Cumbria but also areas of North Lancashire and North Yorkshire - 'tarn' is widely used as the name for small lakes or ponds, regardless of their location and origin (e.g. Talkin Tarn, Urswick Tarn, Malham Tarn). Similarly, in 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. Nonetheless, there are ...
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