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Paul Hilton Posts: 2605 Joined: 21st Nov 2004 Location: UK | quotePosted at 07:33 on 20th August 2013 Hi Ruth; nice to see you here again too; and Sue too of course. York Minster, which seems to have been re-built countless times, was built as we see it now from magnesian limestone quarried from Tadcaster. This stone was formed during a drying up of an inland sea with other deposits added over it during the Permian Period. The stone from the south in the other cathedrals being formed during the Jurassic Period which Dorset's unique coastline is noted from. Thus cathedrals are revealing a bit of the geology of England after the last ice age as it broke off from Continental Europe ( the River Thames once ran into the Danube in Germany) as glaciers retreated and various deposits were being formed. Dorset's famed arch, Durdle Door will one day have the centre of the arch collapse and become two stacks instead like examples of stacks along our coast that began as arches as well. |
Edward Lever Posts: 734 Joined: 22nd Dec 2005 Location: UK | quotePosted at 00:50 on 24th August 2013 On 19th August 2013 00:52, Paul Hilton wrote:
I believe Francis Dashwood had the chalk quarried to provide paid work for local men, at a time when unemployment in the area was high. The stone was used to build the straight road linking West Wycombe with High Wycombe, and the caves were used for the antics you allude to. In modern parlance, Dashwood was a 'party animal'. |
Andy Dodds Posts: 539 Joined: 17th May 2012 Location: England | quotePosted at 14:54 on 28th October 2013 lookin at the pictures theres crags just outside sheffield which look quite similar to that and im sure ive seen them in derbyshire aswell |
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