MAKE A MEME View Large Image The Quarterly journal of the Geological Society of London (12645914533).jpg 1863 <br> HOLL INFERIOR OOLITE <br> 309 <br> <br> o <br> O <br> o <br> – Si <br> o <br> S <br> Cb <br> Bath and Dundry <br> S Doddington Park <br> ¢2 Cross Hands ...
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Keywords: The Quarterly journal of the Geological Society of London (12645914533).jpg 1863 <br> HOLL INFERIOR OOLITE <br> 309 <br> <br> o <br> O <br> o <br> – Si <br> o <br> S <br> Cb <br> Bath and Dundry <br> S Doddington Park <br> ¢2 Cross Hands Inn <br> § Horton <br> Q <br> Avening <br> Nailsworth <br> Rodboro' Hill <br> Stroud <br> Sporebed Hill <br> Painswick ” <br> Leckhampton <br> Cheltenham <br> Cleeve <br> V <br> dotting Hill <br> VOL XIX <br> 3 <br> 3 <br> Pn <br> tf <br> PART I <br> seen separated from uptilted Car- <br> boniferous strata by alternate <br> layers of more or less compacted <br> clay with pebbly bands resting <br> on a bed of conglomerate beneath <br> which Mr C Moore of Bath de- <br> tected a thin stratum containing <br> Avicula contorta <br> North side of the Mendrps ” Be- <br> tween the Mendips and the valley <br> of the Avon the same beds continue <br> to represent the Inferior Oolite <br> and are well exposed in the rail- <br> way-cuttings between Wells and <br> Ammersdown and in a series of <br> roadside-quarries on to Radstoke <br> and further north by the side of <br> the canal near Dunkerton at the <br> foot of the Viaduct Bridge near <br> Limpley Stoke and at Widcombe <br> Hill near Bath In all these lo- <br> calities they continue to preserve <br> those general features which serve <br> to distinguish the one from the <br> other In the neighbourhood of <br> Dunkerton the Upper Bagstone is <br> about 20 feet in thickness and <br> contains Corals of the genera Ana- <br> bacia Stylina and Isastrcea <br> The outlying patch of Inferior <br> Oolite at Dundry Hill is connected <br> with this portion of the main body <br> of the range by the smaller patches <br> of the Barrow Hills Stanton Prior <br> and Timsbury At Dundry the <br> light-coloured partly flaggy partly <br> thick-bedded oolite which caps <br> the hill belongs to the upper sub- <br> division and in certain layers at <br> the top of the hill contains Corals <br> of the same genera and species as <br> the similarly situated beds in the <br> neighbourhood of Dunkerton and <br> Bath Beneath this we find beds <br> of rubbly and ferruginous lime- <br> This interesting section has been <br> given in detail in Mr T R Jones's re- <br> cent Monograph of Fossil Estherice <br> p 74 published by the Palseontogra- <br> phical Society 35328274 109632 51125 Page 309 Text v 19 http //www biodiversitylibrary org/page/35328274 1863 Geological Society of London NameFound Avicula contorta NameConfirmed Avicula contorta NameFound Stylina NameConfirmed Stylina EOLID 4687593 NameBankID 239520 Biodiversity Heritage Library The Quarterly journal of the Geological Society of London v 19 1863 Geology Periodicals Smithsonian Libraries bhl page 35328274 dc identifier http //biodiversitylibrary org/page/35328274 smithsonian libraries Information field Flickr posted date ISOdate 2014-02-20 Check categories 2015 August 26 CC-BY-2 0 BioDivLibrary https //flickr com/photos/61021753 N02/12645914533 2015-08-27 12 00 25 cc-by-2 0 PD-old-70-1923 The Quarterly journal of the Geological Society of London 1863 Photos uploaded from Flickr by Fæ using a script
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