Outlines of Oryctology: An Introduction to the Study of Fossil Organic Remains; Especially of Those Found in the British Strata: Intended to Aid the Student in His Inquiries Respecting the Nature of Fossils, and Their Connections with the Formation of the Earth ...
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Outlines of Oryctology: An Introduction to the Study of Fossil Organic ...
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ambulacra Ammonites animal appears base beak Belemnite belong beneath bivalve bones carinated cavity chalk characters coal columella compressed concave conical convex Cornbrash crenulated crocodile Cuvier cylindrical decussating depressed distinct ditto dorsal du Mus Echinus encrinite equivalved exist figure flat formation fossil remains fusiform gavial genera genus Green sand grooves hinge hyŠna Ichthyosaurus inch inequilateral Klein Lamarck lamellŠ Leske ap lias limestone lobes London clay longitudinal lower valve margin MOUNTAIN LIMESTONE mouth multilocular nearly numerous oblique oblong obtuse oolite opening Organic Remains oval ovate placed plaited plates polypifer pores porous posterior radiating Recent and fossil resembling ribs round rows septa side siphuncle smooth Spatangus species specimens spines spire strata striŠ striated suborbicular substance sulcated surface teeth terminating thick tion tooth transverse striŠ trigonal tubercles tubes tubular turreted umbilicus unequal univalve vegetable vent ventricose vertebrŠ vertex whilst whirls
Page 320 - the tip of the nose. The projection of this great horn very much resembles that of the fanciful unicorn in the British arms. It has a small thick horny substance eight inches long, immediately behind it, which can hardly be observed on the animal at the distance of one hundred yards.
Page 334 - feet above the level of a small river, which, during great part of the year, is engulphed. The bottom of the cavern is nearly horizontal, and is entirely covered, to the depth of about a foot, with a sediment of mud deposited by the diluvian waters. The surface of this mud was, in
Page 334 - into the body of the solid rock, and varying from two to five feet in height and breadth. Its mouth was closed with rubbish, and overgrown with grass and bushes, and was accidentally intersected by the working of a stone quarry. It is on the slope of a hill, about
Page 19 - The hill of calcareous breccia, which we have just regarded as an island in the ancient gulph, is covered with a thick forest of columnar cactus and opuntia, some thirty or forty feet high, covered with lichens, and divided into several branches in the form of candelabras, wearing a singular appearance. Near Maniquarez, at
Page 32 - from the nature of the substances of which they were composed, were they fitted to be applied to the various purposes to which wood, the product of the earth at a subsequent period, has been found to be so excellently adapted, by man. Their remains, it must also be remarked, are now found in conjunction with that
Page 9 - and jet, the transition is so gradual, that there seems no reason to limit the power of water to produce the effect of bituminization in all these varieties; nor is there aught in this change so dissonant from other chemical actions, as to make us hesitate in adopting this cause.
Page 342 - faults in the stratified masses, and the various inclinations of the strata, as well as the vast abruptions by which these several substances are brought to the hand of man, may be regarded as most beneficent provisions resulting from catastrophes too vast and tremendous for human intellect to comprehend.
Page 343 - have proceeded, gradually increasing in superiority, from testaceous animals to reptiles, marine and fresh water amphibia, quadrupeds, and lastly to man, who, in his turn, is destined, with the earth he inhabits, to pass away, and be succeeded by a new heaven and a new earth.