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Identifier: quarterlyjourna331877geol (find matches)
Title: The Quarterly journal of the Geological Society of London
Year: 1845 (1840s)
Authors: Geological Society of London
Subjects: Geology
Publisher: London (etc.)
Contributing Library: Smithsonian Libraries
Digitizing Sponsor: Biodiversity Heritage Library

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rd to thepublication of this paper in the hope that it will aid in correlating theFrench series. He remarked that in England the subdivisions of the (A ctioi Be ri,s hire B a s i n, Melon N.W W ft. °f •zedwmo\ Hon )•ver ( ation VI. oer (. WttOft posvbouton t%ent?d orGrox\ m.he acmeritdes tCal btaL SectionWft. Quart Joum.G&ol.Soo VolJXXJU 71.27/ JUI Newtondcde Wrn.E. ~by N. exposal,. m Forge Vallev 1Z1/t in E. hard Bands, andydbw Grits.Lower CalcareousGrit. ion.? 6.BdH Be^,lard\Bands d yeUrwGrits. Lower Caharmi&Grit100 ft. 0. c. Tht.Sett£on Z06 ft. o.c. Total SeatwrT 305 n. Weymouth Distent I Sandsfoot Xo8v II Osmington III Milwtstiuly Corallian Rocks of Encland. TabU of Comparative Sections by the Bev. J.F.Blake,MAEG.S,and W.H.Hudleston Esq.MAJF.GS. North Wilts . Berks , and Oxfordshire Range Cambridgeshire Quart Jem The Yorks In V Westbwy ■ VI Calne Ill HighworOb. IX Upwart n .. . . X -V Grimstcn ■ .v 5y W. XI Malltm .17/ llamhlrton XIII Nrivlnndale XIV fbiyi Vullet
Text Appearing After Image:
, , Explanatory Notes.— These sections, with the exception of No. 7, give the full developmentof each tied along a surface line earymg from a few hundred yards to a distance, in the case of No. 12, of eightimhs. As most of the Corallian beds, taken on a large scale, are wedge-shaped, the real thickness of each bed variesmaterially according to (hi point SI I. ct, d. Tims in the case of So. 7- A ction at Highicorlb—llte entire series shrinkswithin a moderate distance in a southerly direction, to about 30//. with a complete extinction of some beds and an.increase of others The arrangement adopted brings the top of the chief limestone series of each section upon the same heelthroughout, and thus enables an estimate to be formed at once, both of the relative volume of the limestones in eachand also of the respeelnr derclopmeut of the I ppi r and Lower Groups. The Upper Group is usually a reddish calcareous grit irith variable clays: it includes certain oolitic ironor.; lias terrumiwus

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Author Geological Society of London
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Volume
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1877
Flickr tags
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  • bookid:quarterlyjourna331877geol
  • bookyear:1845
  • bookdecade:1840
  • bookcentury:1800
  • bookauthor:Geological_Society_of_London
  • booksubject:Geology
  • bookpublisher:London__etc__
  • bookcontributor:Smithsonian_Libraries
  • booksponsor:Biodiversity_Heritage_Library
  • bookleafnumber:470
  • bookcollection:biodiversity
  • BHL Collection
  • BHL Consortium
Flickr posted date
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28 July 2014
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