Watchet Faults & Sandstone Dykes
sketchfab
Sea cliffs stretch high above Watchet Harbour, towering about twenty meters into the air. Roughly five hundred meters to the west, a dramatic landscape unfolds. The Mercia Mudstone Group, a geological formation from the Triassic era, is being pulled apart by a north-dipping normal fault that has displaced several metres of rock in its path. This particular fault lies within the Helwell Bay Fault's footwall, marked location 132 on any relevant map. Watchet and Helwell Bay faults are notable features of this region. Some strata exhibit intricate networks of gypsum veins, while steeply-dipping sandstone dykes rise up from the earth.
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