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| Keywords: The Quarterly journal of the Geological Society of London (12981454944).jpg 424 <br> PROCEEDINGS OF THE aEOLOGICAL SOCIETY DgC 15; <br> So <br> L- 'O <br> <br> s <br> f <br> <br> <br> so <br> u» <br> e <br> 3 <br> tt <br> 3 <br> <br> « <br> oa <br> 4i <br> S <br> – « <br> V <br> <br> c <br> to <br> ¢r <br> » <br> ¢g <br> 60 <br> e <br> s <br> r <br> to <br> O <br> to <br> » <br> g <br> o <br> to <br> CO <br> 5S <br> 1 ” 1 <br> « <br> 1 <br> ' <br> t-f <br> » <br> i-H <br> <br> - J <br> r- <br> s <br> - <br> <br> tS <br> u <br> 0 <br> C 9 <br> s <br> O <br> D <br> Is <br> 1 <br> e 5 <br> 1 <br> « <br> <br> p <br> 05 <br> 0 <br> ¢ 1-1 <br> <br> w <br> t» <br> s <br> » <br> – ffi <br> 3 r-H « <br> <br> O f e« f <br> - s » o - <br> \M <br> I § 302 <br> ¢ fe O S <br> o © Ph o <br> 06 <br> ; o <br> _Q 3 - <br> CD <br> Is' <br> 03 <br> O S <br> Q <br> -1-3 a <br> -Si r - <br> ' S <br> T3 W O t» Z3 <br> H B O <br> - Scg J <br> c8 <br> to © 02 <br> CO tH o <br> O DQ <br> W I ” I 03 _ <br> - g I <br> O o w «8 <br> r S - fl 2' <br> P -H ¢'-' J5 <br> _C3 t-l _«r -» <br> 0 <br> 53 S <br> iS CO jT – <br> O ¢ - pj 03 o »3 <br> In making an ascending <br> geological section see sec- <br> tion fig 1 from the edge of <br> the crystalline rocks about <br> five miles south of Elgin <br> and passing by that town to <br> Lossiemouth and the coast- <br> ridge which extends east- <br> wards from that place by <br> Covesea to Burgh Head the <br> following phenomena present <br> themselves In the hills east <br> of Delias the older or cry- <br> stalline rocks are finely la- <br> minated quartzose mica- <br> ceous and gneissose flag- <br> stones splitting to the thick- <br> ness of tiles containing some <br> white quartz -veins with <br> layers of pinkish and greyish <br> colours alternating and vdth <br> northerly dips varying from <br> 25° to 45° This crystalline <br> rock is unconformably over- <br> laid by a hard grit sur- <br> mounted by a coarse red con <br> glomerate with interlacing <br> marly beds as in the sections <br> described near Altyre The <br> Palls of the Shoggle Burn to <br> which I was conducted by <br> my friend the Kev G Gor- <br> don exposes such junctions <br> clearly Brick-red breccia <br> or conglomerate with way- <br> bands of red marl follow as <br> you advance into the vale <br> watered by the Lossie ; and <br> these beds are immediately <br> surmounted by soft yellow <br> grits and sandstones in <br> which fish-scales and other <br> fossils occur Bothriolepis <br> c <br> These fossils in a similar <br> matrix also occur according to <br> Mr Gr Gordon on the side of the <br> Buinach Hill halfway between <br> the Shoggle Burn and Pluscardine <br> Priory ” June 1859 36161989 111474 51125 Page 424 Text v 15 http //www biodiversitylibrary org/page/36161989 1859 Geological Society of London NameFound Bothriolepis NameConfirmed Bothriolepis EOLID 4655846 NameBankID 4093042 NameFound Delias NameConfirmed Delias EOLID 20035 NameBankID 3001511 Biodiversity Heritage Library The Quarterly journal of the Geological Society of London v 15 1859 Geology Periodicals Smithsonian Libraries bhl page 36161989 dc identifier http //biodiversitylibrary org/page/36161989 smithsonian libraries Information field Flickr posted date ISOdate 2014-03-07 Check categories 2015 August 26 CC-BY-2 0 BioDivLibrary https //flickr com/photos/61021753 N02/12981454944 2015-08-26 14 58 25 cc-by-2 0 PD-old-70-1923 The Quarterly journal of the Geological Society of London 1859 Photos uploaded from Flickr by Fæ using a script | ||||
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