Theoretical geomorphology [Libro electrónico] / autor: Adrian E. Scheidegger
Por: Scheidegger, Adrian E [autor/a].
Tipo de material: Libro en línea Editor: New York, New York, United States: Springer-Verlag, c1991Edición: Tercera edición.Descripción: xiv, 434 páginas : ilustraciones ; 25 centímetros.ISBN: 0387525106; 9783642756610 (Print); 9783642756597 (Online).Tema(s): GeomorphologyNota de acceso: Disponible para usuarios de ECOSUR con su clave de acceso Nota de bibliografía: Incluye bibliografía e índice: páginas 423-434 Número de sistema: 56145Contenidos:Mostrar Resumen:Tipo de ítem | Biblioteca actual | Colección | Signatura | Estado | Fecha de vencimiento | Código de barras |
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Libros | Biblioteca Electrónica Recursos en línea (RE) | Acervo General | Recurso digital | ECO400561454781 |
Incluye bibliografía e índice: páginas 423-434
1. Physical geomorphology.. 2. Physical background.. 3. Mechanics of slope formation.. 4. Theory of river action.. 5. System theory of landscape evolution.. 6. Theory of aquatic effects.. 7. Theory of niveal, glacial, and periglacial features.. 8. Theory of aeolian and desert features.. Subject Index
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The surface features of the Earth are commonly split into two categories, the first of which comprises those features that are due to processes occurring inside the solid Earth (endogenic features) and the second those that are due to processes occurring outside the solid Earth (exogenic features). Specifically, the endogenic features are treated in the science of geodynamics, the exogenic features in the science of geomorphology. I have treated the theoretical aspects of the endogenic features in my Principles of Geodynamics, and it is my aim to supplement my earlier book with a discussion of the theory of the exogenic features, the taxonomy of the latter having been discussed in my Systematic Geomorphology. It is my hope that the three books will together pre sent a reasonably coherent, if necessarily incomplete, account of theoretical geology. Contrary to endogenic phenomena, exogenic processes can often be directly observed as they occur: the action of a river, the develop ment of a slope, and the evolution of a shore platform are all suffi ciently rapid so that they can be seen as they take place. This has the result that in geomorphology one is generally on much less specula tive ground regarding the mechanics of the processes at work than one is in geodynamics. eng
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