File:Sketch-map of Europe in the Middle Jurassic period – Geology (1907) (14773981324).jpg

From Wikimedia Commons, the free media repository
Jump to navigation Jump to search

Original file(2,048 × 1,722 pixels, file size: 351 KB, MIME type: image/jpeg)

Captions

Captions

Add a one-line explanation of what this file represents

Summary

[edit]
Description
English:

Identifier: geology00cham (find matches)
Title: Geology
Year: 1907 (1900s)
Authors: Chamberlin, Thomas C. (Thomas Chrowder), 1843-1928 Salisbury, Rollin D., 1859- joint author
Subjects: Geology
Publisher: New York, H. Holt and co.
Contributing Library: Internet Archive
Digitizing Sponsor: Internet Archive

View Book Page: Book Viewer
About This Book: Catalog Entry
View All Images: All Images From Book
Click here to view book online to see this illustration in context in a browseable online version of this book.

Text Appearing Before Image:
. The prevalence of this rock origi-nally gave origin to the name Oolitic for all that part of the systemabove the Lias. The oolitic structure affects not only much of thelimestone, but also lenses and beds of iron ore, in various parts of thecentral province. In England, parts of the Middle Jurassic containestuarine and fresh-water beds, and sometimes (as in Yorkshire) coalseams and beds of iron ore. Marine LTpper Jurassic beds overlie thenon-marine parts of the Middle Jurassic. In southern Europe, the Middle Jura has but little representation,or has not been thoroughly differentiated. In the eastern province, 1 Geikie, op. cit., p. 1132. 2 Idem., p. 1154. 71 GEOLOGY. the larger pari of the Middle Jura is wanting, though the upper horizonsmay be present. Middle Jurassic beds in Lat. 71° have yielded speciesof sub-tropical ferns, cycads, and conifers.1 The Upper Jura.—The encroachment of the sea which was in progressduring the Middle Jurassic time reached its maximum a little later
Text Appearing After Image:
Fig. 355.—Sketch-map of Europe in the Middle Jurassic period. The shaded areas:are areas of deposition, chiefly marine. (After De Lapparent.) as shown by the wide distribution of the Upper Jurassic formations;but before the end of the epoch the sea began to withdraw, for someparts of the area which had been submerged became land, while otherparts were occupied by lakes and bodies of brackish water. The formations of the Upper Jurassic in central Europe containmuch more limestone than those of the lower divisions of the systemin the same province. Corals and sponges were especially abundantin central Europe, and contributed much to the making of the light-colored limestone which, on the continent, has given this member 1 De Lapparent, Trait e de Geologie, p. 1142. THE JURASSIC PERIOD. 75 of the system the name of the White Jura. Some of the sandstonesalso are white. One of the notable phases of the Upper Jurassic in central Europeis the Solenhofen limestone of southern Germany. This

Note About Images

Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original work.
Date
Source

https://www.flickr.com/photos/internetarchivebookimages/14773981324/

Author Internet Archive Book Images
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.
Flickr tags
InfoField
Flickr posted date
InfoField
29 July 2014


Licensing

[edit]
This image was taken from Flickr's The Commons. The uploading organization may have various reasons for determining that no known copyright restrictions exist, such as:
  1. The copyright is in the public domain because it has expired;
  2. The copyright was injected into the public domain for other reasons, such as failure to adhere to required formalities or conditions;
  3. The institution owns the copyright but is not interested in exercising control; or
  4. The institution has legal rights sufficient to authorize others to use the work without restrictions.

More information can be found at https://flickr.com/commons/usage/.


Please add additional copyright tags to this image if more specific information about copyright status can be determined. See Commons:Licensing for more information.
This image was originally posted to Flickr by Internet Archive Book Images at https://flickr.com/photos/126377022@N07/14773981324. It was reviewed on 22 October 2015 by FlickreviewR and was confirmed to be licensed under the terms of the No known copyright restrictions.

22 October 2015

File history

Click on a date/time to view the file as it appeared at that time.

Date/TimeThumbnailDimensionsUserComment
current00:57, 22 October 2015Thumbnail for version as of 00:57, 22 October 20152,048 × 1,722 (351 KB) (talk | contribs)== {{int:filedesc}} == {{information |description={{en|1=<br> '''Identifier''': geology00cham ([https://commons.wikimedia.org/w/index.php?title=Special%3ASearch&profile=default&fulltext=Search&search=insource%3A%2Fgeology00cham%2F find matches])<br> ''...

There are no pages that use this file.