Manual of Geology: Practical and Theoretical, Tom 2R. Griffin, 1855 - 669 |
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abundance alternating ammonites analogous ancient animals appear argillaceous basalt basin beds bones calcareous calcareous grit carboniferous limestone caverns chalk character clay cliffs coal fields coal measures coal strata coarse coast colour conglomerate containing convulsions cornbrash crystallized deposits Derbyshire Devon dikes diluvial dislocations district Durham earth elevation England Eocene feet thick felspar fissures formation fossils fresh water geological geologists gneiss granite green sand greenstone hills hornblende hyæna igneous Ireland ironstone lacustrine lakes laminated land layers lias lime lower marine marls mass mica millstone grit mineral mountain limestone nearly nodules northern Northumberland observed occur old red old red sandstone oolite organic remains paleozoic pebbles period Permian phenomena plants porphyry quartz range red marl red sandstone remarkable rivers rocks sandy schist seams sediment shale shells Silurian sometimes species stone strata stratified surface syenite tertiary thin tion tracts upper valley veins Wales whole Yorkshire
Popularne fragmenty
Strona 487 - Megna, wheu joined by a smaller stream so called, and afterwards loses this second name on its union with the Ganges, at the distance of about forty miles from the sea. The area of the delta of the Ganges (without including that of the...
Strona 183 - It would have been impossible to have traced so thin a seam of coal, along so extensive a range, without some peculiar facilities — some points of reference more distinct than the varying quality of the coal, and the still more irregular fluctuations of the SANDSTONES and SHALES. This coal seam is covered by a roof...
Strona 268 - Indurated blue Clay, with laminae of sulphate of lime 3 — 13. Indurated red and blue Clay 12 — 14. Indurated brown Clay, with sand and sulphate of lime, irregularly interspersed through it. The fresh water...
Strona 5 - Now, if it were noted how far these extended, and the limits of each soil appeared upon a map, something more might be comprehended from the whole, and from every part, than I can possibly foresee, which would make such a labour well worth the pains. For, I am of opinion, such upper soils, if natural, infallibly produce such under minerals, and for the most part, in such order.