The Wonders of Geology: Or, A Familiar Exposition of Geological Phenomena, Volume 2H.G. Bohn, 1866 |
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Page 473
... changes in the Organic Kingdoms . 44. Geological effects of Dynamical and Chemical Action . 45. Strata composed of Organic Remains . 46. General In- ferences . 47. The Ancient World . 48. Corollary . 49. Fi- nal Effects . 50. Concluding ...
... changes in the Organic Kingdoms . 44. Geological effects of Dynamical and Chemical Action . 45. Strata composed of Organic Remains . 46. General In- ferences . 47. The Ancient World . 48. Corollary . 49. Fi- nal Effects . 50. Concluding ...
Page 542
... change of the calcareous matter held in solu- tion in the water ; and that the usual absence of animal remains in such deposits might be similarly accounted for . Mr. Loftus also refers to volcanic agency as the probable cause both of ...
... change of the calcareous matter held in solu- tion in the water ; and that the usual absence of animal remains in such deposits might be similarly accounted for . Mr. Loftus also refers to volcanic agency as the probable cause both of ...
Page 544
... change is induced on the ter- tiary marls of the Lipari Isles by the gaseous emanations and vapours of the fumaroles ... changes take place in these solutions of chloride of sodium , which thus acquire See Mr. Morris's paper in Mag . Nat ...
... change is induced on the ter- tiary marls of the Lipari Isles by the gaseous emanations and vapours of the fumaroles ... changes take place in these solutions of chloride of sodium , which thus acquire See Mr. Morris's paper in Mag . Nat ...
Page 546
... changes . From the decomposition of the sulphate of iron which takes place , a vast quantity of sulphuric acid must be generated , which , reacting on the different bases of magnesia , lime , & c . , contained in the strata , forms ...
... changes . From the decomposition of the sulphate of iron which takes place , a vast quantity of sulphuric acid must be generated , which , reacting on the different bases of magnesia , lime , & c . , contained in the strata , forms ...
Page 567
... changes in the organic world , as demonstrated by fossil remains , are unquestionably those which separated the paleozoic ages from the secondary , and the latter from the tertiary . There are no less than 166 species of fossil plants ...
... changes in the organic world , as demonstrated by fossil remains , are unquestionably those which separated the paleozoic ages from the secondary , and the latter from the tertiary . There are no less than 166 species of fossil plants ...
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Common terms and phrases
abundant ancient animals appear basalt beds beneath bones British Bryozoa calcareous Carboniferous carbonized Chalk character clay coal coal-field coal-measures colour composed conglomerates coniferous containing corals Cornbrash crater crinoids crustaceans crystalline deposits Devonian England epoch erupted existing extinct feet ferns fishes flora Flustra formation fossil genera genus Geol Geological geologists gneiss granite Hill igneous Iguanodon islands Isle Journ Jurassic land lava layers Lias Lign limestone lower Lyell marine mass matter Medals of Creation Memoir miles mineral molluscs mountain Mountain-limestone Murchison nature North numerous observations occur Old Red Old Red Sandstone Oolite organic remains paleozoic period Permian Petrifactions plants pliocene polypes present Prof Quart Red Sandstone remarkable reptiles rocks sand schists shales shells Sigillaria Silurian South species specimens stems stone Stonesfield strata structure substance surface tertiary thickness tion Trans trees Trias Triassic upper vegetable veins volcanic Wealden Yorkshire zoophytes
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