MAKE A MEME View Large Image The Quarterly journal of the Geological Society of London (12735685965).jpg LATER TERTIARY GEOLOGY OF EAST ANGLIA <br> 9D <br> Middle Glacial a thin bed of <br> dark brown loam which also <br> fills a pothole excavated some <br> 5 feet or ...
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Keywords: The Quarterly journal of the Geological Society of London (12735685965).jpg LATER TERTIARY GEOLOGY OF EAST ANGLIA <br> 9D <br> Middle Glacial a thin bed of <br> dark brown loam which also <br> fills a pothole excavated some <br> 5 feet or thereabouts in that <br> drift <br> After what we have observed <br> as to the action of percolating <br> water on the Red Crag and <br> especially the enwrapping of a <br> prominence of Crag by bands of <br> dark brown loam produced from <br> the dissolution of the Crag ma- <br> ° CD <br> terial by the percolating water 3 3 <br> see section II we are far from 3 <br> sure that the loam thus spread- p <br> ing over the denuded surface g <br> and filling the pothole was <br> formed as a surface soil and g <br> the pothole excavated during J <br> the interval represented by the <br> denudation which we have been <br> discussing ; and both the loam <br> and pothole may be due only to IT <br> percolation ; but we think that ST g <br> p <br> p z <br> o <br> p <br> QTQ <br> Hi 1 - ti H <br> p tr § r <br> ~ S CD r T <br> S P /-\ <br> g a- w £ <br> 72 CD J-- P g <br> S-S « <br> J K' 3 <br> SI s <br> r s p 2 <br> 2 3 £ P <br> O Q –º ¢ go <br> -r » ” J Go r <br> s <br> / ' <br> » <br> GO w <br> p a <br> P on <br> - <br> p OTQ <br> 3 ct- <br> 2 o <br> ll <br> QfQ PL <br> p 5 a <br> I' <br> p <br> TO <br> P - <br> o P <br> o <br> ir 1 <br> Pa <br> 4 <br> Jji 00 <br> 3' <br> CD <br> 3 <br> GO <br> a <br> c <br> p <br> p <br> Pj <br> 3 <br> 3 <br> T3 <br> p <br> GO <br> GO <br> 5 <br> Cfq O <br> KJ <br> P ct- <br> rt- <br> 1 <br> P <br> 3 p <br> CD <br> O ri <br> £i <br> 2- PL <br> P <br> °3 <br> 2 <br> S <br> o <br> p <br> o <br> P <br> £ <br> p <br> i ” 1« <br> I ” 1 <br> 00 <br> CO <br> o <br> O <br> as no sign appeared of the sand g ~ J i <br> itself following the loam into g- ' p p <br> the pothole there is some pro- <br> bability of this bed really repre- <br> senting an interglacial land sur- <br> face It is also worthy of no- <br> tice that the interglacially de- <br> nuded slope of the Contorted <br> Drift is almost coincident with <br> the postglacially re-excavated <br> valley-slope <br> Having regard to the two <br> lines of sections XVI and <br> XVII across the Waveney at <br> distant points and to what we <br> have described as to the pre- <br> sence of the Middle Glacial <br> along the valley-sides generally <br> down to the edge of the sheet of Postglacial gravel which fills the <br> valley-bottom in some parts as for some miles on either side of <br> Bungay and to the edge of the alluvium sheet elsewhere there <br> seems to us no reason to doubt that the valley of the Waveney is of <br> interglacial origin like the other valleys of Norfolk which we have <br> been describing and like the valleys of Suffolk which we have <br> presently to describe The following hypothetical section XIX <br> represents what we believe to be the true though concealed structure <br> of this valley <br> Q J G S No 129 h 35818202 110705 51125 Page 99 Text 33 http //www biodiversitylibrary org/page/35818202 1877 Geological Society of London Biodiversity Heritage Library The Quarterly journal of the Geological Society of London v 33 1877 Geology Periodicals Smithsonian Libraries bhl page 35818202 dc identifier http //biodiversitylibrary org/page/35818202 smithsonian libraries Information field Flickr posted date ISOdate 2014-02-24 Check categories 2015 August 26 CC-BY-2 0 BioDivLibrary https //flickr com/photos/61021753 N02/12735685965 2015-08-26 20 00 56 cc-by-2 0 PD-old-70-1923 The Quarterly journal of the Geological Society of London 1877 Photos uploaded from Flickr by Fæ using a script
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