An Elementary Treatise on Geology: Determining Fundamental Points in that Science, and Containing an Examination of Some Modern Geological Systems, and Particularly of the Huttonian Theory of the EarthF.C. and J. Rivington, 1809 - 415 pàgines |
Des de l'interior del llibre
Resultats 1 - 5 de 36.
Pàgina xix
... fluid produced by heat , could have power , by its density , to clevate the mass of our continents ; and no sooner should that mass be fractured , than the fluid would escape through the openings , and the mass would sink down again in ...
... fluid produced by heat , could have power , by its density , to clevate the mass of our continents ; and no sooner should that mass be fractured , than the fluid would escape through the openings , and the mass would sink down again in ...
Pàgina xx
... fluids by which our atmosphere was formed . 199. Dr. Hutton's exposition of his hypothesis re- specting the expansive power of heat . 200. He considers this power as exercised by an expansible fluid , which he calls fiery vapour . 201 ...
... fluids by which our atmosphere was formed . 199. Dr. Hutton's exposition of his hypothesis re- specting the expansive power of heat . 200. He considers this power as exercised by an expansible fluid , which he calls fiery vapour . 201 ...
Pàgina xxi
... fluids , which must have escaped through , fissures in their vault . 209 , 210. Evident stability of the state in which depressed masses rest on the bottom of pre - existing ca- verns into which they had sunk , and impossibility of the ...
... fluids , which must have escaped through , fissures in their vault . 209 , 210. Evident stability of the state in which depressed masses rest on the bottom of pre - existing ca- verns into which they had sunk , and impossibility of the ...
Pàgina xxiv
... fluids , liberated in that very act , must have been immediately followed by the sinking of the raised continents : 284. In the theory of subsidence , the expansible fluids contained in the ca- verns must have increased so much in ...
... fluids , liberated in that very act , must have been immediately followed by the sinking of the raised continents : 284. In the theory of subsidence , the expansible fluids contained in the ca- verns must have increased so much in ...
Pàgina xxv
... fluid would be able to pervade with the same facility , with which aqueous zapour per- vades the atmosphere . 312. Could the inference drawn from these experiments be maintained , it would really be fatal to Dr. Hutton's theory ; since ...
... fluid would be able to pervade with the same facility , with which aqueous zapour per- vades the atmosphere . 312. Could the inference drawn from these experiments be maintained , it would really be fatal to Dr. Hutton's theory ; since ...
Altres edicions - Mostra-ho tot
An Elementary Treatise on Geology: Determining Fundamental Points in that ... Jean André Luc Visualització completa - 1809 |
An Elementary Treatise on Geology: Determining Fundamental Points in That ... Jean André Luc,Henry De La Fite Previsualització no disponible - 2015 |
Frases i termes més freqüents
abrupt action adduced alluvial land Alps already ancient appear ascribed attention birth bottom breccia calcareous calcareous stone catastrophes causes caverns circumstance composed consequence considerable considered continents declivity Deluge earth effects elevation evident existence expansible fluids facts formation formed fractured fragments Genesis geologists geology globe gravel heat hills horizontal Hutton hypothesis inclined Jura Kirwan lake of Bienne lake of Geneva lake of Neuchatel latter lavas Letters to Dr liquid masses of strata materials mineral strata Mont Blanc Mont Jura monuments MOSES moun natural philosophy nature neral NOAH object observed operations opinion origin passage phenomena phenomenon plains Playfair precipitations present proceed produced proof remark respect Rhone ridge rivers rock running waters Salève Saussure Saussure's schistus side soil subsidence substances sufficient summit sunk supposed surface tains tion toises trace Urseren valley vallies Vaulion vertical Voirons volcanos whence whole
Passatges populars
Pàgina 400 - And God spake unto Noah, and to his sons with him, saying, And I, behold, I establish my covenant with you, and with your seed after you ; and with every living creature that Is with you, of the fowl, of the cattle, and of every beast of the earth with you ; 15 from all that go out of the ark, to every beast of the earth.
Pàgina 389 - And the waters prevailed exceedingly upon the earth; and all the high hills, that were under the whole heaven, were covered.
Pàgina 392 - Be fruitful, and multiply, and replenish the earth. And the fear of you and the dread of you shall be upon every beast of the earth, and upon every fowl of the air...
Pàgina 385 - And God said unto Noah, The end of all flesh is come before me ; for the earth is filled with violence through them ; and, behold, I will destroy them with the earth.
Pàgina 389 - And the flood was forty days upon the earth; and the waters increased, and bare up the ark, and it was lift up above the earth.
Pàgina 399 - And take thou unto thee of all food that is eaten, and thou shalt gather it to thee ; and it shall be for food for thee, and for them.
Pàgina 402 - I do set my bow in the cloud, and it shall be for a token of a covenant between me and the earth.
Pàgina 399 - And of every living thing of all flesh two of every sort shalt thou bring into the ark to keep them alive with thee ; they shall be male and female.
Pàgina 84 - ... combined with the inequality of hardness in the rocks, prove, that the present line of the shore has been determined by the action of the sea. The naked and precipitous cliffs which overhang the deep, the rocks hollowed, perforated, as they are farther advanced in the sea, and at last insulated, lead to the same conclusion, and mark very clearly so many different stages of decay. It is true, we do not see the successive steps of this progress exemplified in the states of...
Pàgina 89 - Every river appears to consist of a main trunk, fed from a variety of branches, each running in a valley proportioned to its size, and all of them together forming a system of valleys, communicating with one another, and having such a nice adjustment of their declivities, that none of them join the principal valley, either on too high or too low a level...