File:Annales de géographie (1891) (14590834087).jpg

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Identifier: annalesdegogra14soci (find matches)
Title: Annales de géographie
Year: 1891 (1890s)
Authors: Société de géographie (France)
Subjects: Geography
Publisher: Paris, A. Colin (etc.)
Contributing Library: Robarts - University of Toronto
Digitizing Sponsor: University of Ottawa

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About This Book: Catalog Entry
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Text Appearing Before Image:
rines; la profon-deur de leau y est faible (phol. pi. A). Pour diverses considérationsque nous avons exposées ailleurs1, ces échancrures doivent être consi-dérées comme des vallées creusées à lair libre avant et pendantle Pliocène et envahies depuis par les eaux marines. A partirde Stoura, les directions orographiques redeviennent un peu plusnettes; la direction des chaînes, et, par conséquent, des vallées, estnettement perpendiculaire à la direction générale de lîle. LEubéese termine à son extrémité méridionale par le massif de lOcha(1475 m.). Des coupes successives, perpendiculaires au grand axe delEubée, montrent constamment une dissymétrie nette des versants.Mais cette dissymétrie se traduit diversement, suivant les points : ainsi,dans le N de lîle, le versant le plus abrupt (monts Galtzades) sur-plombe le canal dAtalanti, tandis que dans la région centrale, il sur-plombe la mer Egée. 1. Élude géologique et pétrographique de lîle dEubre. p. 1 î-18.
Text Appearing After Image:
ESQUISSE DE LA GÉOGRAPHIE PHYSIQUE DE LILE DBUBÉE. 129 Érosion marine; les côtes. — LEubée présente un vaste dévelop-pement de eûtes dont les formes sont multiples, en raison de la nature1res variable des roehesqui les composent. Dans la région méridionale,par exemple, elles sont ordinairement escarpées, découpées enéchan-crures étroites et présentent le type de côtes à lias, par suite de Lalter-nance des bandes schisteuses el des bandes marmoréennes perpen-diculaires à la ligne du rivage. Dans la région centrale, la côte quisurplombe la mer Egée et sétend du cap Gérakinikon au cap Koumiforme une haute muraille rocheuse, souvent coupée à pic de plu-sieurs centaines de mètres daltitude, comme dans les monts Soukaro;la profondeur de la mer atteignant 500 m. peu au N des falaisestémoigne de la présence dune grande fosse deffondrement forméepar des affaissements successits ; des témoins très bien conservés deces effondrements sont représentés par les

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https://www.flickr.com/photos/internetarchivebookimages/14590834087/

Author Société de géographie (France)
Permission
(Reusing this file)		 At the time of upload, the image license was automatically confirmed using the Flickr API. For more information see Flickr API detail.
Volume
InfoField
14
Flickr tags
InfoField
  • bookid:annalesdegogra14soci
  • bookyear:1891
  • bookdecade:1890
  • bookcentury:1800
  • bookauthor:Soci__t___de_g__ographie__France_
  • booksubject:Geography
  • bookpublisher:Paris__A__Colin__etc__
  • bookcontributor:Robarts___University_of_Toronto
  • booksponsor:University_of_Ottawa
  • bookleafnumber:142
  • bookcollection:robarts
  • bookcollection:universityofottawa
  • bookcollection:toronto
Flickr posted date
InfoField
29 July 2014

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current09:01, 13 September 2015Thumbnail for version as of 09:01, 13 September 20153,968 × 1,634 (1.65 MB)SteinsplitterBot (talk | contribs)Bot: Image rotated by 90°
05:52, 10 August 2015Thumbnail for version as of 05:52, 10 August 20151,634 × 3,980 (1.64 MB)Fæ (talk | contribs)== {{int:filedesc}} == {{subst:chc}} {{information |description={{en|1=<br> '''Identifier''': annalesdegogra14soci ([https://commons.wikimedia.org/w/index.php?title=Special%3ASearch&profile=default&fulltext=Search&search=insource%3A%2Fannalesdegogra14s...

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