The Quarterly Journal of the Geological Society of London, 23±ÇThe Society, 1867 Vols. 1-108 include Proceedings of the society (separately paged, beginning with v. 30) |
µµ¼ º»¹®¿¡¼
100°³ÀÇ °á°ú Áß 1 - 5°³
xii ÆäÀÌÁö
... present year . This part of the Society's collection is much superior to the British portion , and is more con- sulted ; and your Committee would therefore invite the attention of Fellows , Foreign Members , and Foreign Correspondents ...
... present year . This part of the Society's collection is much superior to the British portion , and is more con- sulted ; and your Committee would therefore invite the attention of Fellows , Foreign Members , and Foreign Correspondents ...
xxxi ÆäÀÌÁö
... present superficial temperature which is due to internal heat proves how in future no appreciable change of climate can result from the refrigeration of the globe , and how , looking back into the past , we shall require an enor- mous ...
... present superficial temperature which is due to internal heat proves how in future no appreciable change of climate can result from the refrigeration of the globe , and how , looking back into the past , we shall require an enor- mous ...
xxxvii ÆäÀÌÁö
... present , but to rivet the attention of geologists in all parts of the world . Those who have enjoyed the advantage of hearing Prof. Rogers at a meet- ing of the British Association , or in our own ANNIVERSARY ADDRESS OF THE PRESIDENT ...
... present , but to rivet the attention of geologists in all parts of the world . Those who have enjoyed the advantage of hearing Prof. Rogers at a meet- ing of the British Association , or in our own ANNIVERSARY ADDRESS OF THE PRESIDENT ...
xxxix ÆäÀÌÁö
... present it gratuitously to the Society . He After he had been in business some years , he visited Germany , and was much interested in the mining - operations of certain dis- tricts there , to which he gave special attention . It was at ...
... present it gratuitously to the Society . He After he had been in business some years , he visited Germany , and was much interested in the mining - operations of certain dis- tricts there , to which he gave special attention . It was at ...
xliv ÆäÀÌÁö
... present widow , by whom he leaves three children : -Harry , who served in the Artillery in India ; Albany , now a Lieutenant in the Royal Engineers ; and Georgiana , an only daughter . " " In 1839 he returned from America , with strong ...
... present widow , by whom he leaves three children : -Harry , who served in the Artillery in India ; Albany , now a Lieutenant in the Royal Engineers ; and Georgiana , an only daughter . " " In 1839 he returned from America , with strong ...
±âŸ ÃâÆǺ» - ¸ðµÎ º¸±â
ÀÚÁÖ ³ª¿À´Â ´Ü¾î ¹× ±¸¹®
Ammonites appear Avicula base beds Belemnites bones Boulder-clay Brachiopoda Brick-earths British Brocastle Bucklandi calcareous Carboniferous Limestone cavern chalk clay Clod Coal-measures conglomerate containing corals Crustacea denudation deposits Devonian Devonian rocks district Drift east Eurypterus fauna feet flint formation fossiliferous fossils fragments genera genus Geol Geological Society Glacial Goldf granite gravel grey grits Hill Hunstanton Ilfracombe inches incurva Journ Jurassic Keuper Liassic Lima lime Lower Lias Lynton marl Martin mass Middle Devonian miles mineral Moore North Devon noticed numerous occur Old Red Sandstone Oolite organic remains Ostrea Pecten Phill planorbis plate portion posterior Postglacial present Professor Pterygotus quarry quartz Rh©¡tic river sand Schloth shale shells side siliceous Silurian slates Southerndown spec species specimens strata stri©¡ structure surface Sutton Stone Terq Thames thickness tion Uitenhage unconformably Upper Devonian valley veins White Lias whorls zone of Ammonites
Àαâ Àο뱸
xxxi ÆäÀÌÁö - On the Elevation and Denudation of the District of the Lakes of Cumberland and Westmoreland.
lxiv ÆäÀÌÁö - In conclusion, he showed that the various silicates already mentioned were directly deposited in •waters in the midst of which the Eozoon was still growing or had only recently perished, and that they penetrated, enclosed, and preserved the structure of the organisms precisely as carbonate of lime might have done ; and he cites these and other facts...
322 ÆäÀÌÁö - supported wholly or in part by annual voluntary contributions, and shall not, and " by its laws may not, make any dividend, gift, division, or bonus in money unto or " between any of its members, and provided also that such society shall obtain the " certificate of the barrister-at-law or lord advocate, as hereinafter mentioned.
263 ÆäÀÌÁö - If all specimens of Eozoon were of the acervuline character, the comparisons of the chamber-casts with concretionary granules might have some plausibility. But it is to be observed that the laminated arrangement is the typical one; and the study of the larger specimens, cut under the direction of Sir WE Logan, shows that these laminated forms must have grown on certain strata-planes before the deposition of the overlying beds, and that the beds are, in part, composed of the broken fragments of similar...
74 ÆäÀÌÁö - Progress of the Geological Survey of Canada from its commencement to 1863. Atlas of Maps and Sections, with an introduction and appendix.
279 ÆäÀÌÁö - Arranged to meet the requirements of the Syllabus of the Science and Art Department of the Committee of Council on Education, South Kensington.
179 ÆäÀÌÁö - Counties, indubitable specimens of the Bos longifrons from freshwater deposits, which are rich in the remains of Elephas and Rhinoceros.
260 ÆäÀÌÁö - I have not found in any of these fragments a canal system similar to that of Eozoon Canadense, though there are casts of large stolons, and, under a high power, the calcareous matter shows in many places the peculiar granular or cellular appearance which is one of the characters of the supplemental skeleton of that species. In a few places a tubulated cell-wall is preserved, with structure similar to that of Eozoon Canadense. " Specimens of Laurentian limestone from Wentworth, in the collection of...
370 ÆäÀÌÁö - Ragged stone, and of the dykes at its base (xiv. xx.), the ratio of the oxygen of the silica to that of all the bases taken together is nearly as 3 : 2.
253 ÆäÀÌÁö - Vennor's section, which is appended, has a thickness of more than 21,000 feet ; but the possible occurrence of more numerous folds than have hitherto been detected, may hereafter render necessary a considerable reduction. These measures appear to be arranged in the form of a trough, to the eastward of which, and probably beneath them, there are rocks resembling those of Grenville, from which the former differ considerably in lithological character ; it is therefore supposed that the Hastings series...