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Researches in Theoretical Geology: Cambridge Library Collection - Earth Science

Autor Henry T. De la Beche
en Limba Engleză Paperback – 19 mar 2014
The geologist Sir Henry Thomas De la Beche (1796–1855) made important contributions as both a surveyor and a theorist. Elected to the Royal Society in 1823, he mapped geological strata in Devon during the 1830s and became the founding director of the British Geological Survey, the world's first national geological survey. In 1847, he was elected president of the Geological Society of London. Reflecting the scope of his scientific knowledge, the present work covers a wide range of topics, including the density of planets, the mineralisation of organic remains, and what could be inferred from the fossils thus created. The book was first published in 1834, the year he became embroiled in an argument with his contemporary Roderick Murchison. Lasting several years, the dispute became known as the 'The Great Devonian Controversy'. De la Beche's Geological Manual (third edition, 1833) has also been reissued in this series.
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Specificații

ISBN-13: 9781108066969
ISBN-10: 1108066968
Pagini: 432
Ilustrații: 47 b/w illus.
Dimensiuni: 140 x 216 x 24 mm
Greutate: 0.54 kg
Editura: Cambridge University Press
Colecția Cambridge University Press
Seria Cambridge Library Collection - Earth Science

Locul publicării:Cambridge, United Kingdom

Cuprins

Preface; 1. Different densities of the sun and known planets; 2. Gaseous state of the solar system; 3. Fractured state of the earth's surface; 4. Transport of detritus by rivers; 5. Chemical change in rocks; 6. Mineral crust of the globe; 7. External oxidation of a metallic nucleus; 8. Mountain valleys; 9. Faults on hilly countries; 10. Polish and striated marks in faults; 11. Organic remains; 12. Organic remains imbedded in rocks now forming; 13. Marine life in the ocean; 14. Division of rocks; 15. Fossiliferous rocks; 16. Oolitic group; 17. Supracretaceous group; 18. Igneous rocks; Appendix.

Descriere

First published in 1834, this work covers such topics as the density of planets and the mineralisation of organic remains.