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 pagina's |
Vanuit het boek
Resultaten 1-5 van 54
Pagina xvii
... block of marble with his saw . 109 110. What conclusions a lapidary , thus led to meditate , would probably draw respecting the disorder prevalent in the strata . 111 , 112. Inconsistency of ascribing the formation of loose strata to ...
... block of marble with his saw . 109 110. What conclusions a lapidary , thus led to meditate , would probably draw respecting the disorder prevalent in the strata . 111 , 112. Inconsistency of ascribing the formation of loose strata to ...
Pagina xxi
... blocks of granite , and other stones , scattered over the surface in various parts of our continents . 226-229 . The possibility of their stransportation by running waters , from mountains , whence they had been originally detached ...
... blocks of granite , and other stones , scattered over the surface in various parts of our continents . 226-229 . The possibility of their stransportation by running waters , from mountains , whence they had been originally detached ...
Pagina xxii
... blocks . 234. The only fragments accumulated on gla- ciers are those detached from the steep sides of superincumbent rocks . 235. Mr. Playfair supposes that the waste of the soil under the blocks may have been one cause of their ...
... blocks . 234. The only fragments accumulated on gla- ciers are those detached from the steep sides of superincumbent rocks . 235. Mr. Playfair supposes that the waste of the soil under the blocks may have been one cause of their ...
Pagina xxiii
... blocks of gra- nulated quartz in some counties of England . 263. Mr. Playfair's persuasion of the proportion which prevails between the size of stones , and the vicinity of the mountains whence he supposes them to have proceeded . 264 ...
... blocks of gra- nulated quartz in some counties of England . 263. Mr. Playfair's persuasion of the proportion which prevails between the size of stones , and the vicinity of the mountains whence he supposes them to have proceeded . 264 ...
Pagina xxiv
... blocks to have travelled in some manner upon the surface ; since their ejection from within by the expansible fluids , liberated in that very act , must have been immediately followed by the sinking of the raised continents : 284. In ...
... blocks to have travelled in some manner upon the surface ; since their ejection from within by the expansible fluids , liberated in that very act , must have been immediately followed by the sinking of the raised continents : 284. In ...
Overige edities - Alles bekijken
An Elementary Treatise on Geology: Determining Fundamental Points in that ... Jean André Luc Volledige weergave - 1809 |
An Elementary Treatise on Geology: Determining Fundamental Points in That ... Jean André Luc,Henry De La Fite Geen voorbeeld beschikbaar - 2015 |
Veelvoorkomende woorden en zinsdelen
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
Populaire passages
Pagina 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.
Pagina 389 - And the waters prevailed exceedingly upon the earth; and all the high hills, that were under the whole heaven, were covered.
Pagina 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...
Pagina 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.
Pagina 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.
Pagina 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.
Pagina 402 - I do set my bow in the cloud, and it shall be for a token of a covenant between me and the earth.
Pagina 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.
Pagina 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...
Pagina 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...