The Eskdale Anticline is a dip-slip fault at Whitby in North Yorkshire, England. The anticline was thought to have stretched for approximately 20 kilometres (12 mi) in a north–south direction underneath the mouth of the River Esk in Whitby, with a depth of 200 feet (61 m). However, modern geological studies have cast doubt on this, with a suggested displacement of only 12 metres (39 ft).
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