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- W2116478710 abstract "The construction of a new railway, however small, affords opportunity for fresh geological sections. In the present instance the line is only 13½ miles long, and presents no new features, but it is interesting in some respects, especially at its western end, where it shows the position of the chalk as regards the underlying beds.It was pointed out long ago by Phillips that a sub-cretaceous anticlinal existed somewhere about Garrowby, stretching east and west, which seemed to cut off the Oolitic rocks in North Yorkshire from those southwards about Market Weighton, but whether these rocks were removed by denudation previous to the deposition of the chalk, or thinned out against an old submarine shore-line was doubtful. The question is by no means settled yet, but the facts are these : the Lower Calcareous Grit and Oxford Clay of the Middle Oolites make their last appearance from the north at Hanging Grimston, near Acklam. The estuarine sandstones of the Lower Oolites share the same fate, except for a small patch at Kirby Underdale and Grimthorpe. These latter come on again south of Market Weighton. Between Hanging Grimston and Sancton the rocks, which underlie the chalk, are composed of Lower Lias, so that a vast gapappears. The mass of rocks, which constitute the moorland of North-East Yorkshire, consisting of estuarine sandstones, with their intercalated marine limestones, notably the Scarborough, Millepore and Dogger beds, which attain at the Peak a thickness of 600 feet, are wanting, as well as the Upper and ..." @default.
- W2116478710 created "2016-06-24" @default.
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- W2116478710 date "1889-01-01" @default.
- W2116478710 modified "2023-10-12" @default.
- W2116478710 title "Notes on the Driffield and Market Weighton Railway" @default.
- W2116478710 doi "https://doi.org/10.1144/pygs.11.2.170" @default.
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