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The Quarterly journal of the Geological Society of London . JrDD LIXCOLXSHTRE WOLDS na pjoj ax Tioj jCqnotcqBg lUH eoH IK iFj fl ' to or feet deep entirely in these sands In the upper part we find white ashgrey and mottled sands in the lower part coarse brown sands in places indurated into stone like the Carstone
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