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- W76806880 abstract "On a grey but fine Saturday morning the field partygathered at the offices of the New Cliffe Hill Quarry atthe start of an excursion aimed at exploring two facetsof Charnwood Forest’s Precambrian geology. At theOld Cliffe Hill Quarry, rocks representing the veryfinal intrusive stage of Precambrian magmatic activityare well displayed. By contrast, at Whitwick Quarry, adiverse assemblage of massive to fragmental igneousrocks is related to the earlier, extrusive phase ofvolcanic activity that was responsible for theaccumulation of the volcano-sedimentary sequencesforming the eastern outcrops of the CharnianSupergroup. Both quarries also offer sections throughthe highly irregular unconformity betweenPrecambrian and Triassic rocks, and in particular theyreveal the details of ‘wadis’, which are remnants of theCharnwood landscape as it existed about 240 millionyears ago. Safety regulations precluded the closeexamination of the higher quarry faces, but goodexamples of the range of lithologies abounded in thevarious piles of quarry waste, and were augmented byinformation obtained during previous visits by theexcursion leader." @default.
- W76806880 created "2016-06-24" @default.
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- W76806880 date "2005-01-01" @default.
- W76806880 modified "2023-09-26" @default.
- W76806880 title "Old Cliffe Hill and Whitwick quarries Charnwood Forest" @default.
- W76806880 hasPublicationYear "2005" @default.
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