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history, but it is still subject to stresses that may cause it to slip. The maximum earthquake arising from a slip of this fault has been estimated to be below
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Evans, DJ; Walker, ASD; Chadwick, RA (2002). "The
Pennine Anticline, northern England - a continuing enigma?".
31:, England. The fault is approximately 500 metres (1,600 ft) long. The fault has produced no appreciable
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Stephens, John Victor; Mitchell, G H; Edwards, Wilfrid (1953). "VII; Structure".
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alongside another and together the two faults merge and run across
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Geology of the country between
Bradford and Skipton
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39:3. The Denholme Clough Fault is part of the
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