Annual Report of the Council, with the President's Address ..., 28–50. köideThe Society, 1841 |
From inside the book
Results 1-5 of 56
Page 12
... result has been set forth in the Paper which will appear in the next part of the Geological Trans- actions , about to be published . It would be presumption in me to offer an opinion on the works of such men ; I prefer therefore to ...
... result has been set forth in the Paper which will appear in the next part of the Geological Trans- actions , about to be published . It would be presumption in me to offer an opinion on the works of such men ; I prefer therefore to ...
Page 14
... result . But to return to Mr. Murchison's journey.— He says that the lowest region of stratified rocks visited by him in Russia was Silurian ; and he adds , " The evidences found in Russia leave no doubt that the old red and Devonian ...
... result . But to return to Mr. Murchison's journey.— He says that the lowest region of stratified rocks visited by him in Russia was Silurian ; and he adds , " The evidences found in Russia leave no doubt that the old red and Devonian ...
Page 16
... results may be obtained . The animals entombed in the detritus of these periods would , we should expect , show that , like as with the creatures of the present day , physical influences must have been felt ; or , in other words , that ...
... results may be obtained . The animals entombed in the detritus of these periods would , we should expect , show that , like as with the creatures of the present day , physical influences must have been felt ; or , in other words , that ...
Page 19
... result.— To the upper Palæozoic series .... To the series known on the Continent as the Eifel and Bensberg series .. To the lower Palæozoic series } 55 63 28 But Sir H. De la Beche has suggested to me , that possibly one class of our ...
... result.— To the upper Palæozoic series .... To the series known on the Continent as the Eifel and Bensberg series .. To the lower Palæozoic series } 55 63 28 But Sir H. De la Beche has suggested to me , that possibly one class of our ...
Page 20
... result from the ingredients of the rocks from whose decom- position the land is formed . Perhaps in few other parts of England are such extensive differences to be fouud in the chemical and mineralogical character of the rocks , and in ...
... result from the ingredients of the rocks from whose decom- position the land is formed . Perhaps in few other parts of England are such extensive differences to be fouud in the chemical and mineralogical character of the rocks , and in ...
Common terms and phrases
Abraham Gesner Alfred Fox Ami Boué ANNUAL REPORT Bart Beche beds Bolitho Borlase British Association Camborne carboniferous character Charles Lemon Chyandour coal Constant Prévost copper Council Curator deposits Devon Devonian district ditto DONATIONS Edward Edwin Ley Enys Falmouth fossils geologists granite Grice Griffith Henry Highness Prince Albert Institute of France J. N. R. Millett John J. A. Boase John Phillips John Prideaux Joseph Carne L. R. Willan Lyell Marazion mineral Mines Murchison museum old red sandstone ORDINARY MEMBERS organic remains Paris Pattison Peach Penzance Plymouth Polgooth Polperro present President PRESIDENT'S ADDRESS Proceedings Professor of Geology R. Q. Couch Redruth Richard Davey Richard Pearce rocks Rodd ROYAL Geological Society Samuel Higgs Samuel Pidwell Secretary Silurian Sir Charles Lemon Sir H slates Society of Cornwall Society of France species specimens strata Subscription Transactions Truro Upton Cheyney Vivian Wheal William William Gregor
Popular passages
Page 1 - Notice of Dr. Hare's Strictures on Prof. Dove's Essay on the Law of Storms Am.
Page 8 - And assuredly, there is no mark of degradation about any part of its structure. It is, in fact, a fair average human skull, which might have belonged to a philosopher, or might have contained the thoughtless brains of a savage.
Page 9 - ... rise to races and permanent varieties in animals and plants, are the same as those which in much longer periods produce species, and in a still longer series of ages give rise to differences of generic rank. He appears to me to have succeeded by his investigations and reasonings in throwing a flood of light on many classes of phenomena connected with the affinities, geographical distribution, and geological succession of organic beings, for which no other hypothesis has been able, or has even...
Page 26 - Address delivered at the Anniversary Meeting of the Geological Society of London by William John Hamilton, Esq., President of the Society : — " The Geological Map of India by Mr.
Page 10 - Every thing, in short, bore the stamp of former ages, as if the world had suddenly rolled back a few centuries. Nor was this to be wondered at. Had not the Island of the Seven Cities been for several hundred years cut off from all communication with the rest of the world, and was it not natural that the inhabitants should retain many of the modes and customs brought here by their ancestors ? One thing certainly they had conserved; the old-fashioned Spanish gravity and stateliness.
Page 8 - ... unity of the human race, but neither Mr. Lyell nor any one else has ventured to point out the primordial stock from which the many varieties which exist proceeded. The Ethiopian represented on Egyptian paintings four thousand years old is exactly the Ethiopian of the present day. The skeleton of an Egyptian mummy of the same date does not differ from that of a modern Copt, A Persian colony settled in Western India one thousand years ago, and which have rigorously refrained from intermixture with...
Page 5 - By JOHN KIDD, MD, FRS, Regius Professor of Medicine in the University of Oxford. III. Astronomy and General Physics, considered with reference to Natural Theology.
Page 13 - A Notice of the Origin, Progress, and Present Condition of the Academy of Natural Sciences of Philadelphia.
Page 9 - Geology, by which he has been led to the conclusion, that those powers of nature which give rise to races and permanent varieties in animals and plants, are the same as those which, in much longer periods, produce species, and, in a still longer series of ages, give rise to differences of generic rank.
Page 1 - PREsENTs. ANONYMOUS (continued). Twenty-ninth Annual Report of the Council of the Royal Geological Society of Cornwall, with the President's Address, and Papers and Notices read to the Society. 8vo. Penzance 1842.