File:The Quarterly journal of the Geological Society of London (1881) (14768367614).jpg

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Identifier: quarterlyjourna371881geol (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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diam. Figs. 18-25. Diastopora cricopora, Vine. 18. Natural size of colony from which the type is drawn. The specimensin the School of Mines vary considerably. 19. Portion of colony, enlarged in the direction of line I, fig. 18, to showthe disposition of the partially immersed cells. 20-22. X 25 times, giving a fair illustration of the ornamentation of thecells. 23, 24. X 75 times. 25. Two separate colonies: the uppermost, D. cricopora (marginal edge),incrusting Elect, foliacea, Lamx. Discussion. The President bore witness to the great value of the authorsstudy of this group of microscopic organisms. Pro! Seeley stated that his study of the Polyzoa had led him toconclude that many of the supposed generic differences were mereaccidents of age and growth. He thought that Mr. Vines paperwas a valuable addition to science. He doubted the wisdom ofinventing wholly new names for previously described species, as hadbeen done in one instance by the author. Quart .Journ.Geol. Soc.Vol.XXXVE.PIXX
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VITBEOUS ROCKS OF MONTANA -U. S n F. RUTLET ON THE VITREOUS ROCKS OF MONTANA, U.S.A. 391 30. The Microscopic Characters of the Vitreous Rocks of Montana,U.S.A. By Frank Rutley, Esq., F.G.S. With an Appendixby James Eccles, Esq., F.G.S. (Read April 6, 1881.) (Plate XX.) The specimens which have supplied the material for this paper werecollected by Mr. James Eccles during a tour in Montana. Theypresent so many interesting points of structure that a description oftheir microscopic characters may prove acceptable to those who areengaged in the study of British vitreous and devitrified rocks.Among the latter we have already found that certain structuralpeculiarities may still be clearly recognized, notwithstanding thechanges which have led to their more or less complete devitrification.Through these changes, once vitreous rocks assume the character offelstones; and as it is highly probable that many of our ancient felstones and hornstones were once vitreous, it becomes im-portant that we s

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Author Geological Society of London
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Volume
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1881
Flickr tags
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  • bookid:quarterlyjourna371881geol
  • 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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