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| [[Image:P220598.jpg|frameless| 300px| ]]
| [[Image:P220598.jpg|frameless| 300px| ]]
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| Blea Tarn and Langdale. Glaciated upland scenery. Blea Tarn occupies a combe, the backwall of which has been removed by the valley glacier that flowed down Great Langdale (seen in the distance).[Bedrock_Geology_UK_North:_Lower_Palaeozoic_-_Cambrian,_Ordovician_and_Silurian | see article]
| Blea Tarn and Langdale. Glaciated upland scenery. Blea Tarn occupies a combe, the backwall of which has been removed by the valley glacier that flowed down Great Langdale (seen in the distance).[see article | Bedrock_Geology_UK_North:_Lower_Palaeozoic_-_Cambrian,_Ordovician_and_Silurian]
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Revision as of 14:54, 11 June 2014

Bedrock_Geology_UK_North:_Lower_Palaeozoic_-_Cambrian,_Ordovician_and_Silurian]