File:The American journal of science (1892) (18151397235).jpg

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

Original file ‎(994 × 1,046 pixels, file size: 305 KB, MIME type: image/jpeg)

Captions

Captions

Add a one-line explanation of what this file represents

Summary

[edit]
Description
English:

Title: The American journal of science
Identifier: americanjourna3441892newh (find matches)
Year: 1880 (1880s)
Authors:
Subjects: Science
Publisher: New Haven : J. D. & E. S. Dana
Contributing Library: Smithsonian Libraries
Digitizing Sponsor: Biodiversity Heritage Library

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:
Metamorphic Conglomerate in the Green Momitains. 275 seen again in the secondary mineral, while the relationship of maximum pleochroism of these zones to the greatest pleo- chroism of the chlorite is handed down as well. This metaso- matic phenomenon has not been observed in other phases of the ,ottrelite-bearing conglomerate thus far studied by me.
Text Appearing After Image:
Alteration of ottrelite to chlorite. A, overlapping plates of ottrelite. B, bifur- cating vein of chlorite allomorphosed after ottrelite and including cores of unal- tered mineral. C, quartz and feldspar mosaic. The background of the rock is composed about equally of quartz and feldspar as principal constituents. The feldspar is fresh and' glassy, untwinned and is probably albite; but it is hardly abundant enough in the ottrelite-bearing phases to make the rock a gneiss even in mineralogical composition; and, structurally, a gneissic habit has been nowhere observed where ottrelite exists to any extent. Sericite is also abundant and occurs in minute prisms between the interlocking quartz grains and enclosed by the albite generally, and rarely by the ottrelite. It also encloses lines of rutile dots arranged parallel to its cleavage planes, and, next to the ottrelite it is the last- formed mineral. Associated with rutile in the groundmass are groups of stout and slender prisms and plates having a very high single and double refraction and a variable color from brownish-yellow to blue even in the same individual. These T identified as anatase and for verification I studied Diller's sections described in his contribution on " Anatas als Umwandlungsprodukt von Titanit im Biotitamphibolgranit der Troas."* Unlike the anatase *N. J. B., 1, 1883, pp. 187-193.

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/18151397235/

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.
Volume
InfoField
1892
Flickr tags
InfoField
  • bookid:americanjourna3441892newh
  • bookyear:1880
  • bookdecade:1880
  • bookcentury:1800
  • booksubject:Science
  • bookpublisher:New_Haven_J_D_E_S_Dana
  • bookcontributor:Smithsonian_Libraries
  • booksponsor:Biodiversity_Heritage_Library
  • bookleafnumber:305
  • bookcollection:biodiversity
  • BHL Collection
  • BHL Consortium
Flickr posted date
InfoField
27 May 2015
The categories of this image need checking. You can do so here.
  • Please remove redundant categories and try to put this image in the most specific category/categories.
  • You can remove this template by clicking here (or on the first line).



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@N07/18151397235. It was reviewed on 22 September 2015 by FlickreviewR and was confirmed to be licensed under the terms of the No known copyright restrictions.

22 September 2015

File history

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

Date/TimeThumbnailDimensionsUserComment
current16:09, 21 September 2015Thumbnail for version as of 16:09, 21 September 2015994 × 1,046 (305 KB)Fæ (talk | contribs)== {{int:filedesc}} == {{information |description={{en|1=<br> '''Title''': The American journal of science<br> '''Identifier''': americanjourna3441892newh ([https://commons.wikimedia.org/w/index.php?title=Special%3ASearch&profile=default&fulltext=Searc...

You cannot overwrite this file.

There are no pages that use this file.

Retrieved from "https://commons.wikimedia.org/w/index.php?title=File:The_American_journal_of_science_(1892)_(18151397235).jpg&oldid=886432873"