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 pages |
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Page xii
... strata one of the greatest objects of this science . 29. Huttonian opinions respecting the degradation of our conti- nents , and the action of external causes upon them . 30. Respect- ing the sediments of rivers , and the materials ...
... strata one of the greatest objects of this science . 29. Huttonian opinions respecting the degradation of our conti- nents , and the action of external causes upon them . 30. Respect- ing the sediments of rivers , and the materials ...
Page xiii
... strata have been successively formed in the same manner : the catastrophes undergone by the whole mass of strata have produced the rela- tive differences of level between mountains and plains . 52. Ne- cessity of studying the effects ...
... strata have been successively formed in the same manner : the catastrophes undergone by the whole mass of strata have produced the rela- tive differences of level between mountains and plains . 52. Ne- cessity of studying the effects ...
Page xiv
... strata of granite form the most ancient geological monu- 55. Effects produced on the new continents by atmosphe- rical causes . 59. The production of granite must have been a first operation , resulting from the accession of some new ...
... strata of granite form the most ancient geological monu- 55. Effects produced on the new continents by atmosphe- rical causes . 59. The production of granite must have been a first operation , resulting from the accession of some new ...
Page xvii
... strata . 111 , 112. Inconsistency of ascribing the formation of loose strata to the rivers , and yet supposing those rivers to have sunk their beds in loose strata , when they first began to flow , 113 , 114. Huttonian opinions relative ...
... strata . 111 , 112. Inconsistency of ascribing the formation of loose strata to the rivers , and yet supposing those rivers to have sunk their beds in loose strata , when they first began to flow , 113 , 114. Huttonian opinions relative ...
Page xix
... strata , and the supposed existence of an expand- ing power , directed from the centre toward the circumference . 174. a . The angular movements of the strata will afford a fair criterion of the two opposite theories of subsidence and ...
... strata , and the supposed existence of an expand- ing power , directed from the centre toward the circumference . 174. a . The angular movements of the strata will afford a fair criterion of the two opposite theories of subsidence and ...
Autres éditions - Tout afficher
An Elementary Treatise on Geology: Determining Fundamental Points in that ... Jean André Luc Affichage du livre entier - 1809 |
An Elementary Treatise on Geology: Determining Fundamental Points in That ... Jean André Luc,Henry De La Fite Aucun aperçu disponible - 2015 |
Expressions et termes fréquents
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
Fréquemment cités
Page 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.
Page 389 - And the waters prevailed exceedingly upon the earth; and all the high hills, that were under the whole heaven, were covered.
Page 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...
Page 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.
Page 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.
Page 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.
Page 402 - I do set my bow in the cloud, and it shall be for a token of a covenant between me and the earth.
Page 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.
Page 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...
Page 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...