File:The Quarterly journal of the Geological Society of London (13369133274).jpg

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1872..
30LLAS — UPPER-GREENSASTD VENTRICULITES.
65
spherical bodies are found from yutt" to j^-" diameter, which agree
in their mineral characters with the opaque yellowish-brown fibre
of No. ii.
The Hexaradiate Elements. — The Ventriculite skeleton is formed by
the regular anastomosis of a number of hexaradiate elements, each
one of which consists of six radial fibres, apparently tubular,
diverging from a common centre at right angles to each other. To
the end of the first quarter of their course the fibres are of the most
microscopic diameter ; but they then suddenly expand, their diameter
becomes many times greater, and continues so to the end of their
entire course, where they open into the similar radii of surrounding
elements. At their point of expansion they give off four fibres of a
diameter of about 2 5 1 00 ", which pass backwards at an angle of about
45° to join similar fibres given off by the other arms of the same
element, so as to form a skeleton octahedron about the common
centre (fig. 2). This is the typical structure of the hexaradiate
Fig. 1.
Fis. 2.
B, radii.
r, interior radii.
o, spaces.
elements. As in the Vitrea, however, abnormalities occur, the ele-
ments sometimes becoming pseudo-heptaradiate (fig. 3), and some-
times apparently triradiate. The additional ray of the heptara-
diates is prolonged merely from one of the octahedral fibres, and
does not start from the common centre of the six normal rays.
The triradiates also have nothing in common with the hexaradiate
elements.
Combination of the Hexaradiate Elements. — Considering one of these
elements, it will be seen that each of its four horizontal radii is
freely continuous in the same straight line with a horizontal radius
furnished to it by one of four other elements symmetrically disposed
in the same plane around it ; each of the vertical radii is continuous
in the same way with a vertical radius derived from each of two
other elements, one placed above and the other below it : all the

VOL. XXIX. — PARTI. F
Date
Source https://www.flickr.com/photos/biodivlibrary/13369133274
Author Geological Society of London
Full title
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The Quarterly journal of the Geological Society of London.
Page ID
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39050969
Item ID
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120601 (Find related Wikimedia Commons images)
Title ID
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51125
Page numbers
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Page 65
Names
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NameFound:Ventriculites NameConfirmed:Ventriculites NameBankID:4390439 NameFound:Vitrea NameConfirmed:Vitrea EOLID:52703 NameBankID:2688242
BHL Page URL
InfoField
https://www.biodiversitylibrary.org/page/39050969
Page type
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Text
Flickr sets
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  • The Quarterly journal of the Geological Society of London. v. 29 (1873).
Flickr tags
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Flickr posted date
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24 March 2014
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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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26 August 2015

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current10:33, 26 August 2015Thumbnail for version as of 10:33, 26 August 20151,853 × 3,186 (1.01 MB) (talk | contribs)== {{int:filedesc}} == {{BHL | title = The Quarterly journal of the Geological Society of London. | source = http://www.flickr.com/photos/biodivlibrary/13369133274 | description = 1872.. <br> 30LLAS — UPPER-GREENSASTD VENTRICULITES. <br> 65 <br> sphe...

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