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Internal constitution of the earth

Colaborador(es): Gutenberg, Beno [editor] .Tipo de material: TextoTextoSeries Physics of the earth 7. Editor: New York: McGraw-Hill book company,Inc., 1939Edición: Primera edición.Descripción: 394 páginas; 23 cm.Tema(s): TIERRA (PLANETA)  | CIENCIAS DE LA TIERRA  | GEOMORFOLOGÍA Clasificación CDD: 550/N57
Contenidos:
1. Introduction -- 2. The origin of the solar system -- 3. Relevant facts and inferences from field geology -- 4. Elastic properties of materials of the earths crust -- 5. The crust of the earth and Its relation to the interior -- 6. Observed temperatures in the earths crust --7. The cooling of the earth and the temperature in its interior -- 8. Forces in the earth -- 9. Hypotheses on the development of the earth -- 10. Evidence on the interior of the earth derived from seismic sources -- 11. Evidence from deep-focus eartquakes -- 12. Structure of the crust. Continents and oceans -- 13. Density, gravity, pressure and ellipticity in the interior -- 14. The elastic constants in the interior of the earth -- 15. Viscocsity, strength and internal friction in the interior of the Earth
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Tipo de ítem Colección Signatura Estado Código de barras
Libros Libros Colección Bibliográfica 550/N57 (Navegar estantería) Disponible ROJ0001115
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Incluye índice: páginas 395-413

1. Introduction -- 2. The origin of the solar system -- 3. Relevant facts and inferences from field geology -- 4. Elastic properties of materials of the earths crust -- 5. The crust of the earth and Its relation to the interior -- 6. Observed temperatures in the earths crust --7. The cooling of the earth and the temperature in its interior -- 8. Forces in the earth -- 9. Hypotheses on the development of the earth -- 10. Evidence on the interior of the earth derived from seismic sources -- 11. Evidence from deep-focus eartquakes -- 12. Structure of the crust. Continents and oceans -- 13. Density, gravity, pressure and ellipticity in the interior -- 14. The elastic constants in the interior of the earth -- 15. Viscocsity, strength and internal friction in the interior of the Earth

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