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Contributions to the Geology of Gloucestershire

Published online by Cambridge University Press:  17 March 2016

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As the Lias in this county is a very bad material for economical purposes, it is not often extensively quarried; and, considering the few available sections, the number and variety of organic remains which have been, from time to time, collected, are really remarkable, and show the prolific nature of the sea of that period. Some localities in that sea, of course, would be richer than others, as is the case in the present day; but, on the whole, this formation is everywhere marked by a great abundance and diversity of fossils. The Palæontologist often looks with a longing eye at some old quarry, long since closed, which had been at one time famous for its zoological contents, and speculates upon the wonders which lie concealed beneath his feet; and he restores in thought some ancient monster of the deep, some curiously-formed shell, or some strange plant; and perhaps, if he had the power, he would dig away, in the hope of possessing some of these treasures which his imagination has conjured up before him. And yet, after all, such speculations are not so imaginative or unreal as they may at first sight appear, for the strange and extraordinary forms of extinct life, which the extended researches of scientific inquirers have brought to light, seem to justify the highest flights of fancy; and none can tell when or where some wonderful relic of the past may be found.

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Research Article
Copyright
Copyright © Cambridge University Press 1858

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References

page 370 note * So called from its resemblance to a horse's hoof. It appears to be allied to Cypricardia or Cardita, and belongs to the same family as Cardinia, another abundant and still more characteristic Liassic form.—P. B. B.

page 371 note * This division is well displayed at Fretherne Cliff, near Newnham (a station on the Great Western Railway between Gloucester and Chepstow); and the student should by all means go there, as it affords a better and thicker section than can be seen elsewhere; and many fossils may be procured. There is, also, a small patch of Lias, still higher in the series, at Pyrton, on the opposite side of the Severn, full of fossils; and this spot is particularly interesting, as it exhibits the junction of the Lias with the upper Ludlow rocks, which are brought up here by a fault and crop out on the banks of the river a little further to the west.—P. B. B.

page 375 note * Figures and descriptions of many of these will be seen in Brodie's “Fossil Insects,” pls. 6—10.

page 376 note * Fresh-water crustacea inhabiting a bivalve shell.

page 376 note † A very probable view of the origin of these “bone beds” is given in “Stones of the Valley,” page 18, an able and interesting work lately published by my friend, the Rev. W. S. Symonds, F.G.S., Rector of Pendock.—P. B. B.