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More model informationAt St Brides Haven a small cove forms a natural cross section of a multilayer of sandstones and mudstones which have been folded and deformed during the Variscan Orogeny. The rocks belong to the Sandy Haven Formation (Late Siluarian to early Devonian) and interpreted as alluvial fan deposits into a muddy lake. The grey sandstones have been cut by thrust faults and stacked on top of each other. Have a look at the virtual outcrop: you can follow the fault pathways across the sandstones.
Lat: 51° 45’ 18.8”N, Long: 05° 11’ 08.0”W
Virutal outcrop generated using Agisoft Photoscan from 533 terrestrial and aerial photographs acquired with a DJI Phantom 3 and a Nikon 5000 DSLR. Photos and text by Phoebe Sleath. Processing by Magda Chmielewska.
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