The Wonders of Geology: Or, A Familiar Exposition of Geological Phenomena, Volume 2H.G. Bohn, 1866 |
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Page 469
... rocks and fossils we owe very much indeed that is new in our knowledge of the Permian and Silurian formations . Of the latter especially we have a recently corrected classification , which , elaborated by this distinguished geologist ...
... rocks and fossils we owe very much indeed that is new in our knowledge of the Permian and Silurian formations . Of the latter especially we have a recently corrected classification , which , elaborated by this distinguished geologist ...
Page 472
... Rocks . 11 . Silurian and Cambrian Strata of the British Isles . 12. The Longmynd or Bottom Rocks . 13. Silurian Strata of Stafford- shire . 14. The Clent Hills . 15. The Wrekin . 16. The Malvern Hills , & c . 17. Silurian and Cambrian ...
... Rocks . 11 . Silurian and Cambrian Strata of the British Isles . 12. The Longmynd or Bottom Rocks . 13. Silurian Strata of Stafford- shire . 14. The Clent Hills . 15. The Wrekin . 16. The Malvern Hills , & c . 17. Silurian and Cambrian ...
Page 473
... Rocks . 31. Precious Stones . 32. Metalliferous Veins . 33 . Auriferous Alluvia . 34. Cupreous Deposits . 35. Transmu- tation of Metals . 36. Review of the Hypogene Rocks . 37 . Organic Remains in Metamorphic Rocks . 38. Chronology of ...
... Rocks . 31. Precious Stones . 32. Metalliferous Veins . 33 . Auriferous Alluvia . 34. Cupreous Deposits . 35. Transmu- tation of Metals . 36. Review of the Hypogene Rocks . 37 . Organic Remains in Metamorphic Rocks . 38. Chronology of ...
Page 487
... rocks whence the debris was derived ; but the materials were too scanty to throw any satisfactory light upon the ... rocks , with sandstones and clay ; for the quartz- pebbles and the micaceous sands and clays may have been derived from ...
... rocks whence the debris was derived ; but the materials were too scanty to throw any satisfactory light upon the ... rocks , with sandstones and clay ; for the quartz- pebbles and the micaceous sands and clays may have been derived from ...
Page 537
... rocks , having in their composition a large proportion of magnesia . As a whole , the strata are compa- ratively poor in organic remains ; but in some localities land - plants , marine shells , and reptiles are met with ; cer- tain ...
... rocks , having in their composition a large proportion of magnesia . As a whole , the strata are compa- ratively poor in organic remains ; but in some localities land - plants , marine shells , and reptiles are met with ; cer- tain ...
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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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