The Quarterly Journal of the Geological Society of London, 19권The Society, 1863 Vols. 1-108 include Proceedings of the society (separately paged, beginning with v. 30) |
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viii 페이지
... stone Jamaica 442 Chert forma - tion . Antigua 426 Marl forma - 426 tion . Antigua Tertiary .... Montserrat 443 Marl - forma - Barbadoes 444 tion . Antigua 421 Conglomerate Antigua 418 [ Chert - forma - tion . Antigua 418 422 412 415 ...
... stone Jamaica 442 Chert forma - tion . Antigua 426 Marl forma - 426 tion . Antigua Tertiary .... Montserrat 443 Marl - forma - Barbadoes 444 tion . Antigua 421 Conglomerate Antigua 418 [ Chert - forma - tion . Antigua 418 422 412 415 ...
xi 페이지
... stone . Bouldon 234 Upper Silurian and Lowest Joggins 90 Devonian Coal - measures 77 Carboniferous 90 90 Lower Oolite Scarborough 153 Wealden ...... Permian Mesozoic ...... Hanover . { Burakova , Kazan , Russia . Low Jurassic ? Kotá ...
... stone . Bouldon 234 Upper Silurian and Lowest Joggins 90 Devonian Coal - measures 77 Carboniferous 90 90 Lower Oolite Scarborough 153 Wealden ...... Permian Mesozoic ...... Hanover . { Burakova , Kazan , Russia . Low Jurassic ? Kotá ...
xvii 페이지
... stone near Ludlow , by George E. Roberts , Esq .; communicated by the President . On the Parallel Roads of Glen Roy , and their place in the History of the Glacial Period , by T. F. Jamieson , Esq . , F.G.S. Feb. 4th . - On a Hyæna ...
... stone near Ludlow , by George E. Roberts , Esq .; communicated by the President . On the Parallel Roads of Glen Roy , and their place in the History of the Glacial Period , by T. F. Jamieson , Esq . , F.G.S. Feb. 4th . - On a Hyæna ...
xl 페이지
... stone , and at Builth and the Longmynd on the highly contorted and denuded Llandeilo and Cambrian strata . The lists of the Geological Survey show that about seventy species of fossils are known in the Lower and Upper Llandovery strata ...
... stone , and at Builth and the Longmynd on the highly contorted and denuded Llandeilo and Cambrian strata . The lists of the Geological Survey show that about seventy species of fossils are known in the Lower and Upper Llandovery strata ...
xliii 페이지
... stone , between the Upper Silurian and Carboniferous Rocks , how did it happen that the life of the two periods was so perfectly distinct ? 1st . The old reply would have been that the Silurian life was destroyed at the commencement of ...
... stone , between the Upper Silurian and Carboniferous Rocks , how did it happen that the life of the two periods was so perfectly distinct ? 1st . The old reply would have been that the Silurian life was destroyed at the commencement of ...
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abundant Ammonites angle Anthracosaurus Antigua appear beds calices Cambrian carapace Carboniferous character clay clay-slate Coal-measures colour conglomerate containing corallites Corals Crustacean delta deposits described Devonian diameter district east Estheria Eurypterus feet formation fossils fragments genera genus Geol Geological Society geologists glaciers Glen Roy gneiss granite Graptolites gravel greenish-grey grey greywacke hill Huronian inch Journ Lake limestone Loch Lower Ludlow margin marl mass mica-slate micaceous miles mineral Miocene nearly noticed occur Old Red Sandstone Oolite organic remains Permian plate Poaka Poaka Beck portion present probably Prof Quart quartzite R. I. Murchison Ragstone Rhynchonella ridge river rocks sand schist Scotland seen septa shales shells side Silurian Skiddaw slates species specimens stone strata stream surface teeth Tertiary thickness thin tion transverse unconformity Upper Lias valley valves vertebræ
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170 페이지 - P. pileiformis, M'Chesney, Descr. of New Species of Fossils from the Palaeozoic Rocks of the Western States of America, p. 40, 1849. P. Cora, Dav., Mon. Carb. Brach. pi. 36. fig. 4, pi. 42. fig.
xliv 페이지 - geology or palaeontology are able to show to the contrary, a Devonian fauna and flora in the British Islands may have been contemporaneous with Silurian life in North America, and
xx 페이지 - To promote researches concerning the mineral structure of the earth, and to enable the Council of the Geological Society to reward those individuals of any country by whom such researches may hereafter be made,"—" such individual not being a Member of the Council." 1831. Mr. William Smith. 1835. Dr. GA Mantell. 1836. ML Agassiz.
xlii 페이지 - Break very nearly complete both in genera and species, and probable unconformity. Tremadoc Slate. Break very nearly complete both in genera and species, and probable unconformity. Llandeilo and Caradoc beds. Large break, especially in species, and probable unconformity. Lower Llandovery beds. Break and
221 페이지 - Hull, E. The Coal-fields of Great Britain; their history, structure, and resources; with notices of the coal-fields of other parts of the world.
468 페이지 - Among the Reptilian remains found in erect trees at the South Joggins, there have occurred several portions of skeletons, •which, from their sculptured cranial bones, plicated teeth, and the forms of their scales and limb-bones, I have referred to the genus Dendrerpeton, but to individuals of much smaller size than the full-grown specimens of
xlii 페이지 - unconformity. Wenlock Shale, &c. Each of these breaks, in my opinion, necessarily implies a lost epoch, stratigraphically quite unrepresented in our area, and the life of which is only 'feebly represented in some cases by the fossils common to the underlying and overlying formations. But
323 페이지 - the strata of deltas, and calculations formed from local superficial deposits. I myself have seen the bricks which formed the foundation of a house I had built carried away, and strewed along the bottom of a river at a depth of 30 or 40 feet below the level of the country.
263 페이지 - will show that, on the whole, the remains of any given animal, if abundant, are not confined to one spot in the cave, but are pretty evenly distributed, and lie large with small, the more with the less dense, not in the least degree sorted by water. There is no evidence of the Bear succeeding to the
64 페이지 - for at least 750 geographical miles, and covering an area fully equal to that of France, that, as it appears to me, a record ought to be preserved of these borings. Southward, at the Rio Colorado, the Pampean formation meets the great Tertiary formation of Patagonia; and northward, at