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action ages altered ancient animals appear basin become beds belong bones calcareous called causes chalk changes chapter characters clay coast common composed cone consider considerable consist containing continued coral course covered currents deposits depth described direction distinct district earth elevation entirely Eocene evidently example existing extended feet formations formed fossil France freshwater Geol geologist granite greater groups height hills hundred inhabited island Italy lakes land lava less limestone living lower manner marine marl mass matter miles mineral mountains nature nearly Newer observed occur ocean older organic remains origin Paris perhaps period plants Pliocene present probably produced recent referred regions remains remarkable rise rivers rocks sand sandstone secondary seen shells side sometimes species strata successive supposed surface tertiary thickness thousand tion upper usually valley vegetable volcanic whole
Side 253 - The seat of desolation, void of light, Save what the glimmering of these livid flames Casts pale and dreadful ? Thither let us tend...
Side 254 - Millions of Spirits for his fault amerced* Of Heaven, and from eternal splendours flung For his revolt; yet faithful how they stood, Their glory withered: as when Heaven's fire Hath scathed the forest oaks, or mountain pines, With singed top their stately growth though bare Stands on the blasted heath.
Side 62 - ... behold a wonder ! they but now who seemed in bigness to surpass earth's giant sons, now less than smallest dwarfs in narrow room throng numberless...
Side 443 - It is not to be expected that we should be able to find tests for conditional convergence as simple and general as those of §§ 173 et seq.
Side 389 - Had there been any record of their eruptions in the time of Pliny or Sidonius Apollinaris, the one would scarcely have omitted to make mention of it in his Natural History, nor the other to introduce some allusion to it among the descriptions of this his native province.
Side 187 - It appeared to them more philosophical to speculate on the possibilities of the past, than patiently to explore the realities of the present ; and having invented theories under the influence of such maxims, they were consistently unwilling to test their validity by the criterion of their accordance with the ordinary operations of nature. On the contrary, the claims of each new hypothesis to credibility appeared enhanced by the great contrast, in kind or intensity, of the causes referred to and those...
Side 505 - We aspire in vain to assign limits to the works of creation in space, whether we examine the starry heavens, or that world of minute animalcules which is revealed to us by the microscope. We are prepared, therefore, to find that in time also the confines of the universe lie beyond the reach of mortal ken. But in whatever direction we pursue our researches, whether in time or space, we discover everywhere the clear proofs of a Creative Intelligence, and of His foresight, wisdom, and power.
Side 115 - ... of many years. In June, 1747, the body of a woman was found six feet deep, in a peat-moor in the Isle of Axholm, in Lincolnshire. The antique sandals on her feet afforded evidence of her having been buried there for many ages; yet her nails, hair, and skin, are described as having shown hardly any marks of decay.
Side 18 - Welcome to their roar! Swift be their guidance, wheresoe'er it lead ! Though the strain'd mast should quiver as a reed. And the rent canvas fluttering strew the gale, Still must I on.; for I am as a weed, Flung from the rock, on Ocean's foam to sail Where'er the surge may sweep, the tempest's breath prevail.
Side 214 - ... mentioned. It is evident that where such accidents occur the want of continuity in the series may become indefinitely great, and that the monuments which follow next in succession will by no means be equidistant from each other in point of .time. If this train of reasoning be admitted, the occasional distinctness of the fossil remains, in formations immediately in contact, would be a necessary consequence of the existing laws of sedimentary deposition and subterranean movement, accompanied by...