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Toothill Rock

STAND WELL BACK FROM THE EDGE!

For a panoramic view of the Churnet Valley there is no better place than Toothill Rock, but beware there is a steep drop and a very long fall.

The rock was formed because the Hollington Sandstone has greater resistance than the underlying Hawksmoor Sandstone - responsible for the valley's steep sides.

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This page was last updated on 15 July 2016. Contribute here if you have information or photos to add to this page.

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