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The Askrigg Block is the name applied by geologists to the crustal block forming a part of The Pennines of northern England and which is essentially coincident with the Yorkshire Dales. It is defined by the Dent Fault to the west and the Craven Fault System to the south whilst to the north it is separated from the Alston Block by the Stainmore Trough. It originated as a geological structure during the Carboniferous Period as a major element in the Pennine Block & Basin Province.[1][2] References ^ British Geological Survey. 1996, Tectonic Map of Britain, Ireland & adjacent areas, Pharaoh et al. 1:1500 000 (Keyworth, BGS) ^ Edwards, W; Trotter, F M, The Pennines and Adjacent Areas, British Regional Geology (Third ed.), London: HMSO. Natural Environment Research Council (published 1954) This geology article is a stub. You can help Wikipedia by expanding it. v • d • e