Blea Tarn

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File:Blea Tarn Lingmoor Fell.jpg
Blea Tarn from Lingmoor Fell

Blea Tarn in lies in a small hanging valley between Great Langdale and Little Langdale in Westmorland.

The tarn itself was shaped anciently by glacial ice moving over the col from nearby Great Langdale, but the ice was cut off as the glacier shrank, leaving "moraines very different from those at the head of the main valley".[1] A carpark for twenty vehicles is sited close to the tarn with an all-ability trail leading around the tarn.[2]

The tarn is forested on its western shore with rhododendrons also found there, the other shores being grassland. Blea Tarn was characterised in 1969 as being low in nutrients and acidic but not having suffered from fertiliser pollution. Brown trout, perch and pike can all be found in the tarn.

Blea Tarn was designated a 'site of special scientific interest' in 1989 because of its importance for palaeo-environmental studies relating to the Devensian and Flandrian times.[3][4] Pollen analysis from Blea Tarn shows evidence for elm branches being collected as fodder from 3300 BC and forest clearances occurring from around 3000 to 2000 BC, corresponding with the dates of the Langdale axe industry in the Neolithic Age.[5]

The nearby Side Pike SSSI was designated in 1977 as one of the few areas in the British Isles where rock demonstrating subaerial volcanic processes are seen. The ignimbrite and tuff rocks there form part of the Borrowdale Volcanic Group.[6]

Outside links

("Wikimedia Commons" has material
about Blea Tarn)

References