The Quarterly Journal of the Geological Society of London, Volumen39The Society, 1883 Vols. 1-108 include Proceedings of the society (separately paged, beginning with v. 30) |
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Términos y frases comunes
angle appears Assynt Assynt series bands basalt basalt-glass beds bone Boulder-clay boulders calices Cambrian Carboniferous character clay colour conglomerate convex corals crystalline crystals David's deposits described diabase Dimetian distal district dolomite Dundry dykes east evidence fault feet felsite felspar foliation fossils fragments genus Geol Geological glacier gneiss granite gravel grit Hebridean Hicks Hill hornblende Iguanodon inch Inferior Oolite intrusive Journ lapilli lavas limestone lines Loch Logan Rock lower margin mass metamorphism mica microscopic miles Millstone Grit mineral Museum nearly occur paper pebbles Pebidian Plate Pliosaurus porphyries Porth-lisky portion posterior present Prof quartz quartzite resemblance Rhosson ridge river rocks rounded sand Sandstone schists seen septa shales shell side siliceous Silurian species specimens stones strata structure surface thick Torridon trace transverse tuffs Ueber umbo unconformability upper valley valve vertical volcanic group
Pasajes populares
Página 129 - A TREATISE ON THE METALLURGY OF IRON : containing Outlines of the History of Iron Manufacture, Methods of Assay, and Analyses of Iron Ores, Processes of Manufacture of Iron and Steel, &c. By H. BAUERMAN, FGS, Associate of the Royal School of Mines.
Página 82 - Committee for the purpose of investigating the Circulation of the Underground Waters in the Permeable Formations of England, and the Quality and Quantity of the Waters supplied to various towns and districts from these formations ; and that Mr. De Ranee be the Secretary.
Página 140 - CONTRIBUTIONS TO THE PHYSICAL HISTORY OF THE BRITISH ISLES ; with a Dissertation on the Origin of Western Europe and of the Atlantic Ocean. With 27 Coloured Maps. By EDWARD HULL, MA, LL.D., FRS, late Director of the Geological Survey of Ireland.
Página 34 - ... the basis of a disquisition on the general subject of the variability of species (a doctrine early impressed on me by Dr. Prichard), I sent him a copy of the memoir (published in the Philosophical Transactions), with a sort of apology for having tried to make so much out of what might be thought so small and trivial a subject ; he replied with a most kindly approval of the object and manner of my work, adding " any single point is really the universe," — a remark whose pregnancy left an impression...
Página 32 - Donation Fund, and said: — Professor Morris, — The Council of the Geological Society, in awarding to Mr. John Young, of the Hunterian Museum, Glasgow, the balance of the proceeds of the Murchison Donation Fund, wishes to mark its appreciation of the value of his long-continued researches on the fossil polyzoa, especially those of the western part of Scotland, and of his investigations into the structure of the shells of the Carboniferous Brachiopoda. In his absence, I have much pleasure in placing...
Página 21 - as an acknowledgment of eminent services in any department of Geology, irrespective of the receiver's country; but he must not be older than 45 years at his last birthday, thus probably not too old for further work, and not too young to have done much.
Página 18 - 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.
Página 611 - ... considerable quantities of pyroxene, as well as other minerals not yet determined. At various intervals throughout the zone of schistose rocks, occur rather coarsely crystalline white limestones. The structure of Mount Ida is a comparatively simple anticlinal, with so short an axis extending east and west that the upper portion of the mountain is approximately a dome.
Página 21 - as an acknowledgment of eminent services in any department of geology, irrespective of the receiver's country ; but he must not be older than forty-five years at his last birthday, thus probably not too old for further work, and not too young to have done much.
Página 104 - On Mineral Vein Formation now in Progress at Steamboat Springs Compared with the Same at Sulphur Bank.