File:The Quarterly journal of the Geological Society of London (12683224815).jpg

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1856.. WRIGHT UPPER LIAS SANDS.
Fig. 2. — Section of Frocester Hill, near Stonehouse.
303
a, b, c. Inferior Oolite ; 70 feet.
D, B. Calcareo-ferruginous sandstone (Cephalopoda-bed) ; 6 feet ")
F. Yellow and brown sands, with inconstant and concretionary V" Upper Lias Sands."
bands of calcareous sandstone ; 1 50 feet ? J
G. Upper Lias shale ; 80 feet.
H. Marlstone ; hard calcareous sandstone, resting on brown and grey sands, with bands
and nodules of ferruginous sandstone ; 150 feet.
I. Lower Lias shale.
Inferior Oolite.
Ft. in.
a.
h.
A fine-grained oolitic limestone, similar to the freestone of
Birdlip, Painswick, and Leckhampton Hills ; the upper
beds exhibit a most remarkable example of oblique bed-
ding, the flaggy layers of which rest horizontally on in-
chned beds of freestone : thickness about 50
A coarse, hght-cream-coloured, gritty, crystalline oohte,
traversed at intervals by shelly layers extremely crystal-
line ; a great part of the rock appears to be composed
of the fragments and plates of Crinoidea, the plates and
spines of Echinidce, and comminuted fragments of the
shells of MoUusca. This white rock has a most remark-
able lithological character, and glistens briUiantly when
lit up by the sun's rays. The shelly and pisolitic seams
which traverse this bed resemble those in the Pea-grit.
The surface of weathered slabs discloses numerous mi-
croscopic objects; the rock is in fact almost entirely
composed of organic debris. It measures about 10
c. A hard, fine-grained, ooHtic, sandy limestone, of a hght-
brown colour, lithologically dififerent from b. It contains
many fossil shells, which are extracted with difficulty ;
and passes into a hard yellow oohte with few fossils :
thickness from 8 to 10
.The lithological character of this rock is very different
to that of d, on which it rests..
The Cephalopoda-bed — Upper Lias.
d. A coarse, dark-brown, calcareo-siliceous rock, full of small,
dark, flattened grains of hydrate of iron. It contains

an immense quantity of fossils, but Ammonites and Be-
Date
Source https://www.flickr.com/photos/biodivlibrary/12683224815
Author Geological Society of London
Full title
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The Quarterly journal of the Geological Society of London.
Page ID
InfoField
35338756
Item ID
InfoField
109655 (Find related Wikimedia Commons images)
Title ID
InfoField
51125
Page numbers
InfoField
Page 303
Names
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NameFound:Crinoidea NameConfirmed:Crinoidea EOLID:11119143 NameBankID:594597
BHL Page URL
InfoField
https://www.biodiversitylibrary.org/page/35338756
Page type
InfoField
Text
Flickr sets
InfoField
  • The Quarterly journal of the Geological Society of London. v. 12 (1856).
Flickr tags
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Flickr posted date
InfoField
21 February 2014
Credit
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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.


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current21:14, 26 August 2015Thumbnail for version as of 21:14, 26 August 20151,247 × 2,106 (488 KB) (talk | contribs)== {{int:filedesc}} == {{BHL | title = The Quarterly journal of the Geological Society of London. | source = http://www.flickr.com/photos/biodivlibrary/12683224815 | description = 1856.. WRIGHT UPPER LIAS SANDS. <br> Fig. 2. — Section of Frocester Hi...

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