TheDenholme Clough Fault is a smallfault located inDenholme,Northern England. The fault is approximately 500 metres (1,600 ft) long. The fault has produced no appreciableearthquake 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 belowmagnitude 3. The Denholme Clough Fault is part of thePennines anticline and is partially visible from the surface.
The fault starts atLeeming alongside another and together the two faults merge and run acrossThornton Moor, through Denholme and own towardsHuddersfield where it is known asTheBailiff Bridge Fault. The throw of the fault (itsVertical displacement) is as much as 500 feet (150 m) across Thornton Moor.[1]
The Denholme Clough Fault forms part of a complex fault system that influencedsedimentation patterns during theCarboniferous Period, particularly theNamurian stage (approximately 326–315 million years ago). The fault shows a northwest–southeast trend and forms agraben structure with theAire Valley Fault to the northeast. This structural configuration played a pivotal role in controlling depositional environments and sediment distribution during the early Marsdenian substage of the Namurian, as evidenced by detailedsequence stratigraphic analyses of theMillstone Grit Group in this region. Sedimentological studies indicate that the graben formed between the Denholme Clough Fault and theAire Valley Fault acted as a conduit forfluvial systems, withpalaeocurrent indicators suggesting a southeasterly flow direction along the axis of the graben. The term "R2b3 sequence" denotes a particular package of sediments laid down during the early Marsdenian substage of the Namurian. In this interval, braided river channels were funnelled directly into the graben formed between the Denholme Clough Fault and the Aire Valley Fault, concentrating fluvial fairways in that structural corridor.[2]
At several sites, evidence shows that the Denholme Clough Fault was active while sediments were being laid down. At Cock Hill Quarry, arcuate sets of cross-cutting faultlets within the East Carlton Grit suggest at least two episodes of syn-depositional faulting during the R2b2 sequence. Similarly, disturbed bedding features at Bingley Road Quarry within the Woodhouse Flags of the R2b3 sequence exhibitliquefaction-style flame and ball structures that may represent sediment liquefaction triggered by seismic activity associated with movements along the fault system. The fault also influenced accommodation space anddepositional thickness patterns across the region, with apparent thinning of the R2b3 sequence observed in the vicinity of the Denholme Clough Fault footwall at localities such as Nan Scar Clough, suggesting that differentialsubsidence across the fault controlled sediment accumulation rates.[2]
The fault played a major role in controlling the distribution of certain distinctive lithological units, particularly the Keighley Bluestone. This indurated and brittle purple to dark grey siltymudstone, characterised by abundantZoophycosbioturbation andHyalosteliasponge spicules, is geographically restricted to the fault block between the South Craven–Aire Valley Fault System to the northeast and the Denholme Clough Fault to the southwest, south of the intersection of thesestrike-slip faults with the Pendle lineament. The restricted occurrence of the Keighley Bluestone has been interpreted as indicating the presence of ahorst block elevated at the time of deposition, demonstrating how the Denholme Clough Fault contributed to creating localised depositional environments during the Carboniferous. The fault thus represents an important structural element that influenced the complex interplay between tectonics,eustasy and sedimentation in thePennine Basin during the late Carboniferous.[2]
53°47′45.6″N1°53′10.4″W / 53.796000°N 1.886222°W /53.796000; -1.886222