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- W2042118090 abstract "After alluding to the progress which had been made of late years in the study of the glacial deposits, and to several important papers on the subject which had appeared in the Transactions of this Society, Dr. Fraser said he was persuaded that observers in this department were in the way of collecting data which would yet be of the greatest service in discussions as to geological time. He believed that a useful paper in that direction might be given, based on facts that had already been ascertained and classified. At present, however, he avoided these more important general questions, and confined himself to the statement of a few recent observations. The Paisley clays presented the following general order:— (1) Underlying all was the old boulder clay or till, the conditions of which were altogether unfavourable to life. It represented a cold, bleak, and in part tumultuary period. (2) Immediately above this was a laminated clay, whose texture was in every way distinct from the preceding. It was generally shell-less and stone-less, and in many instances beautifully and delicately laminated, the structure being at times so regular as to resemble the edge of a closed book, and specimens kept for a year or two had shown a texture and taken a polish like jasper. (3) Above the laminated clay, which was also useful in brickmaking, there occured a thick bed in which shells of arctic and boreal types were found— Tellina proxima, Panopaea Norvegica, Pecten islandicus, Cyprina islandica, and others too" @default.
- W2042118090 created "2016-06-24" @default.
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- W2042118090 date "1873-01-01" @default.
- W2042118090 modified "2023-09-25" @default.
- W2042118090 title "XIV. On some Recently-Exposed Sections in the Paisley Clay-beds, and their Relation to the Glacial Period" @default.
- W2042118090 doi "https://doi.org/10.1144/transglas.4.2.178" @default.
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