THE NATURE OF THE JUNCTION BETWEEN THE LOWER CARBONIFEROUS AND THE MILLSTONE GRIT OF NORTH-WEST YORKSHIRE.
- 1 January 1925
- journal article
- Published by Geological Society of London in Proceedings of the Yorkshire Geological and Polytechnic Society
- Vol. 20 (2), 257-291
- https://doi.org/10.1144/pygs.20.2.257
Abstract
No abstract availableThis publication has 9 references indexed in Scilit:
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- ON THE RHYTHMIC SUCCESSION OF THE YOREDALE SERIES IN WENSLEYDALEProceedings of the Yorkshire Geological and Polytechnic Society, 1923
- THE MILLSTONE GRIT SEQUENCE BETWEEN MASHAM AND GREAT WHERNSIDEProceedings of the Yorkshire Geological and Polytechnic Society, 1914
- II.—A New Trilobite from the Millstone Grit of North YorkshireGeological Magazine, 1914
- The Occurrence of Limestone Conglomerates on the North side of the Craven FaultsProceedings of the Yorkshire Geological and Polytechnic Society, 1894
- On the Gelogy of the Country between Grassington and WensleydaleProceedings of the Yorkshire Geological and Polytechnic Society, 1892
- On the Changes of the Lower Carboniferous Rocks in Yorkshire, from South to NorthProceedings of the Yorkshire Geological and Polytechnic Society, 1890