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| Keywords: The Quarterly journal of the Geological Society of London (14052749896).jpg 532 <br> H HICKS OX THE PEE-C-OrBElAN <br> supposed by the Director-General the evidence is perfectly clear <br> that the Cambrian strata are here faulted against the Dimetian <br> as shown on the plan Of this there are abundant proofs of various <br> kinds The line of junction is most clearly marked and the con- <br> Fig 5 ” Plan of Allan Valley at Portli-dais <br> to St Da-dds <br> to PortUisky <br> For explanation see fig 3 <br> Fig 6 ” Slcetcli in Allan Valley soidli side at Porth-clais showiiig <br> faulted contact of Camlrian Pods tvitJi Bimetian The place <br> specially referred to by Dr Geikie as showing intrusion of the <br> latter into the former <br> 2 Greenish sandstones <br> 1 Basal conglomerate <br> Cambrian <br> A Dimetian <br> F Fault <br> glomerates can be removed without a particle of the true Dimetian <br> being attached to them There is no alteration set up in the 36941365 113697 51125 Page 532 Text 40 http //www biodiversitylibrary org/page/36941365 1884 Geological Society of London Biodiversity Heritage Library The Quarterly journal of the Geological Society of London v 40 1884 Geology Periodicals Smithsonian Libraries bhl page 36941365 dc identifier http //biodiversitylibrary org/page/36941365 smithsonian libraries Information field Flickr posted date ISOdate 2014-04-30 Check categories 2015 August 26 CC-BY-2 0 BioDivLibrary https //flickr com/photos/61021753 N02/14052749896 2015-08-26 05 53 18 cc-by-2 0 PD-old-70-1923 The Quarterly journal of the Geological Society of London 1884 Photos uploaded from Flickr by Fæ using a script | ||||
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