Watchet Faults & Sandstone Dykes
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Sea cliffs (~ 20 m high), ~ 500 m west of Watchet Harbour.. Marls of the Mercia Mudstone Group (Triassic) are cut by a north-dipping normal fault with a displacement of several metres, in the footwall of the Helwell Bay Fault (location 132, Watchet and Helwell Bay faults). Some layers show networks of gypsum veins. Steeply-dipping sandstone dykes occur. See Meng, Q., Hooker, J., Cartwright, J., 2017. Genesis of natural hydraulic fractures as an indicator of basin inversion. Journal of Structural Geology 102, 1-20. Virtual Outcrop by David Peacock, University of Bergen
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