File:The Quarterly journal of the Geological Society of London (1862) (14577987687).jpg

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Identifier: quarterlyjourna181862geol (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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Text Appearing Before Image:
ive the whole of this portion to theBarton series, we shall not be able to allow as much thickness tothe superior part of the Bracklesham Beds as the Stubbington sectionand the New Forest beds would lead us to attribute to them. Ittherefore seems most probable that the line of separation at thisplace is to be sought somewhere in the concealed portion of No. 17(No. xix. of the following section). The upper part is probably theequivalent of a bed near the base of the Barton series, which is 52feet thick at Alum Bay, and at that place very fossiliferous, havingbeen formed under a less deep-water condition. The next portion * A pcbble-bod, forming the base of the Bracklesham series, is very fullydeveloped at Bishopstoke. See Geol. Survey Map, sheet No. xi.t See Quart. Journ. Geol. Soc. vol. ii. p. 254.\ Memoirs of the Geol. Survey, Isle of Wight, 1856. § Even at Alum Bay the dark clays of the central portion of the Barton seriesare replaced by sands. 1861.J FISHER BRACKLESIIAM BEDS. (it)
Text Appearing After Image:
70 PROCEEDINGS OF THE GEOLOGICAL SOCIETY. (Dec. 4, will be the equivalent of the green bands which form the base of theBarton beds at High Cliff and Alum Bay, and there contain theNimimulina jplanulata, var. Prestwichiana, while the lower part willrepresent the upper beds of the Bracklesham group as seen at Stub-bington and Hunting Bridge. No. 16 of Mr. Prestwich (Nos. xvm.& xvn. of the following section) undoubtedly belongs to the Brac-klesham group, as I shall prove when speaking of the New Forestbeds. It is on the horizon of the highest bed seen at BrackleshamBay, and locally known as the Clibs #. In the following section the numerals within brackets agree withthose in Mr. Prestwichs section, where the numbers run through-out all the Eocene beds seen at the Bay. The Roman numeralsrefer to the Bracklesham Beds alone, which I have subdivided some-what more minutely. It is well to premise that the colours of thestrata at this locality are, for the most part, much altered by recent

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https://www.flickr.com/photos/internetarchivebookimages/14577987687/

Author Geological Society of London
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Volume
InfoField
1862
Flickr tags
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  • bookid:quarterlyjourna181862geol
  • bookyear:1845
  • bookdecade:1840
  • bookcentury:1800
  • bookauthor:Geological_Society_of_London
  • booksubject:Geology
  • bookpublisher:London__etc__
  • bookcontributor:Smithsonian_Libraries
  • booksponsor:Biodiversity_Heritage_Library
  • bookleafnumber:148
  • bookcollection:biodiversity
  • BHL Collection
  • BHL Consortium
Flickr posted date
InfoField
28 July 2014



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