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Borrowdale Volcanic group in the central Lake District have been transported 13km south-east.

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The Naddle Valley has a small terminal moraine. Originally 200-400 metres long, and 10-15 metres high, a small lake existed behind it.

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320 million years old shell and small animals remnants.

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Uldale is in the north of the Lake District. It is home to the Skiddaw Slates and these are the oldest rock type in the area. It was formed nearly 500 million years ago when black muds and sands settled. Since then they have been pushed up by tectonic forces and are now found in the north and in the mountain ranges which are typically smooth.

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There is a remarkable set of crescentic ridges of moraine at the end of the tarn. These are recessional moraines.

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Erosion has revealed granite outcrops. 400 million years old.

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Erosion has revealed granite outcrops. 400 million years old.

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Erosion has revealed granite outcrops. 400 million years old.

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The Windermere group are are sedimentary mudstones.

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The Helvellyn Range is an 11km long ridge, over 600m high with numerous glacial erosional landforms. The summit of Helvellyn is an example of a pyramidal peak. However, due to erosion, during the  coldest part of the glacial period when ice completely covered the area. It lacks more than two corries on its flanks, hence has been less sharply eroded by the retreat of their back walls.

In the Hellvelyn range, there is a corrie that contains a tarn called the Red Tarn. This is separated from the Nethermost Cove by a narrow Arete called Striding Edge. Ice from Red Tarn flowed into the valley of Glenridding, forming a glacier large enough to create a small glacial trough. This is through the process of abrasion.

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Lake District National Park, United Kingdom

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Borrowdale Volcanic Group consist of very hard lava and ash formed in major eruptions about 450 million years ago.

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Skiddaw and Ingleton groups