The Quarterly journal of the Geological Society of London . 5 = = Oxford = Cornbrash. Note.—The base of the Upper Cretaceous rocks is shown by a dark line section. Discussion. The Chairman (Mr. W. H. BZudleston) said that for the secondtime that evening it had been shown to the Society that much stillremained to be done in British geology. The lateness of the hourwould preclude anything like an adequate discussion. The deter-mination of the two systems of faulting, one of mid-Tertiary, andthe other of pre-Upper Cretaceous age, was of g
The Quarterly journal of the Geological Society of London . 5 = = Oxford = Cornbrash. Note.—The base of the Upper Cretaceous rocks is shown by a dark line section. Discussion. The Chairman (Mr. W. H. BZudleston) said that for the secondtime that evening it had been shown to the Society that much stillremained to be done in British geology. The lateness of the hourwould preclude anything like an adequate discussion. The deter-mination of the two systems of faulting, one of mid-Tertiary, andthe other of pre-Upper Cretaceous age, was of great disturbance of which the Broadway fault was a member hadbeen held by a distinguished geologist as dating from early Quater-nary times, whilst he (the speaker) admitted that he had beendisposed to connect it with the one through the Isle of subject of overthrust was most interesting, but could only becriticized by those whose knowledge of the country was of Mr. Clement Beid also spoke, and the Author £ I INTEA-CEEIAOEOU * DISTURBANCI i mm tm, Forest Marblt Combrash Oxford Clay Coralliatt Kimmeridge Clay T The thick lines indicate j>£>st Quart, Journ. Geol. Soc. Vol. LI. PL XVII.
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Keywords: ., bookcentury1800, bookdecade1840, bookidquarte, booksubjectgeology
