File:The Quarterly journal of the Geological Society of London (12684568344).jpg

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

Original file(1,773 × 3,200 pixels, file size: 1.09 MB, MIME type: image/jpeg)

Captions

Captions

Add a one-line explanation of what this file represents

Summary

[edit]
Description

1852..
BRICKENDEN ON DEVONIAN FOOT-TRACK.
99
the sandstone strata irom which the slab was obtained are unques-
tionably referable to the Devonian formation, to which they had
always been considered to belong ; the occurrence of foot-prints, ap-
parently of Chelonians, in rocks in which no vestiges of the class
Reptilia had ever been observed in any part of the world, having led
some persons to doubt whether they might not be connected with
the Permian Series. The discovery of the Reptile at Spynie, by Mr.
Patrick Duif, dispels, however, all doubts on this point, for the sand-
stones of Cummingston and Spynie are identical, and at Spynie are
overlaid by the cherty limestone peculiar to the upper division of the
Devonian in this district.
Figs. 1 and 2. — Sections showing the Relation of the Sandstone and
Limestone Rocks in the neighbourhood of Elgin.
Fig. L
N.E.
. Fig. 2.
Stotfield Point.
S.W.
a, a. Sandstone \ T.„„„„;„„
bib. Limestone P^^^'^^^"-
The sandstone quarry from which the
fossil reptile was obtained.
The yellow sandstone of Stotfield is a continuation of that of Covesea, from which
latter the Foot-prints were obtained.
The relative position of the strata in the two localities above re-
ferred to is shown in the accompanying figs. 1 & 2. The quarry from
which the reptile was obtained is situated on the Hill of Spynie ; the
locality whence I extracted the slab with foot-prints is to the north-
west, and separated from the former beds by Loch Spynie.
I am reminded, by the accomplished editor of * The Witness/
Mr. Hugh Miller, "that the Dipterian family, in which M. Agassiz
places that unique ichthyolite the Stagonolepis Robertsoni, is em-
phatically an Old Red Sandstone family, represented in the coal-mea-
sures only by a Biplopterus, and in the Permian series it is without
a representative at all."
By the discovery, therefore, of the foot-prints at Cummingston,
and of the Reptilian skeleton at Spynie, Morayshire, we have now
obtained indisputable evidence in our own country (I believe for the

first time) that the class Reptilia existed at that very remote period
Date
Source https://www.flickr.com/photos/biodivlibrary/12684568344
Author Geological Society of London
Full title
InfoField
The Quarterly journal of the Geological Society of London.
Page ID
InfoField
35461099
Item ID
InfoField
109911 (Find related Wikimedia Commons images)
Title ID
InfoField
51125
Page numbers
InfoField
Page 99
Names
InfoField
NameFound:Reptilia NameConfirmed:Reptilia EOLID:1703 NameBankID:2549792 NameFound:Stagonolepis NameConfirmed:Stagonolepis EOLID:4531012 NameBankID:4350821
BHL Page URL
InfoField
https://www.biodiversitylibrary.org/page/35461099
Page type
InfoField
Text
Flickr sets
InfoField
  • The Quarterly journal of the Geological Society of London. v. 8 (1852).
Flickr tags
InfoField
Flickr posted date
InfoField
21 February 2014
Credit
InfoField
This file comes from the Biodiversity Heritage Library.

This tag does not indicate the copyright status of the attached work. A normal copyright tag is still required. See Commons:Licensing.


العربية  বাংলা  Deutsch  English  español  français  italiano  日本語  македонски  Nederlands  polski  +/−



Licensing

[edit]
w:en:Creative Commons
attribution
This file is licensed under the Creative Commons Attribution 2.0 Generic license.
You are free:
  • to share – to copy, distribute and transmit the work
  • to remix – to adapt the work
Under the following conditions:
  • attribution – You must give appropriate credit, provide a link to the license, and indicate if changes were made. You may do so in any reasonable manner, but not in any way that suggests the licensor endorses you or your use.
This image was originally posted to Flickr by BioDivLibrary at https://flickr.com/photos/61021753@N02/12684568344. It was reviewed on 27 August 2015 by FlickreviewR and was confirmed to be licensed under the terms of the cc-by-2.0.

27 August 2015

This image is in the public domain because it is a mere mechanical scan or photocopy of a public domain original, or – from the available evidence – is so similar to such a scan or photocopy that no copyright protection can be expected to arise. The original itself is in the public domain for the following reason:
Public domain

This work is in the public domain in its country of origin and other countries and areas where the copyright term is the author's life plus 70 years or fewer.


This work is in the public domain in the United States because it was published (or registered with the U.S. Copyright Office) before January 1, 1929.


This tag is designed for use where there may be a need to assert that any enhancements (eg brightness, contrast, colour-matching, sharpening) are in themselves insufficiently creative to generate a new copyright. It can be used where it is unknown whether any enhancements have been made, as well as when the enhancements are clear but insufficient. For known raw unenhanced scans you can use an appropriate {{PD-old}} tag instead. For usage, see Commons:When to use the PD-scan tag.


Note: This tag applies to scans and photocopies only. For photographs of public domain originals taken from afar, {{PD-Art}} may be applicable. See Commons:When to use the PD-Art tag.

File history

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

Date/TimeThumbnailDimensionsUserComment
current21:09, 26 August 2015Thumbnail for version as of 21:09, 26 August 20151,773 × 3,200 (1.09 MB) (talk | contribs)== {{int:filedesc}} == {{BHL | title = The Quarterly journal of the Geological Society of London. | source = http://www.flickr.com/photos/biodivlibrary/12684568344 | description = 1852.. <br> BRICKENDEN ON DEVONIAN FOOT-TRACK. <br> 99 <br> the sandston...

There are no pages that use this file.