WE RARELY get out into East Yorkshire, the county formerly known as North Humberside and before that as the East Riding of Yorkshire. In Winifred Holtby's novel of the 1930s it becomes the South Riding. I hope they've made their mind up once and for all this time.As we head east along the M62 it's the cooling towers of Drax and Eggborough that dominate the flat landscape, which is underlain by soft Triassic rocks, dating from a time when desert conditions prevailed in Britain. However there's very little to be seen of these sandstones in this part of Yorkshire because they're almost entirely covered by clay, peat and silt. During the last glacial period, some 18,000 years ago, ice sheets filled the North Sea. Meltwaters from glaciers to the north ponded up to form Lake Humber which flooded over the Vale of York.The power stations are a reminder of even older rocks that lie concealed beneath the Triassic desert sediments. The seams in the Selby Coalfield are the remnants of tropical forest that grew here 300 million years ago. Between the coal and the desert sandstones there's the Magnesian Limestone, dating from a time around 250 million years ago when a dying sea, the Zechstein, covered much of Yorkshire. It must be all that work at Brimham that is bringing my research on Yorkshire Rock to mind again. Prehistoric East YorkshireJust to go over that again, in chronological order;
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