Theoretical geomorphology [Libro electrónico] / autor: Adrian E. Scheidegger
Por: Scheidegger, Adrian E [autor/a].
Tipo de material: Libro en línea Editor: Berlin, Germany: Springer, c1961Descripción: xii, 333 páginas : ilustraciones ; 24 centímetros.ISBN: 9783662010365 (Print); 9783662010341 (Online).Tema(s): Physical geographyNota de acceso: Disponible para usuarios de ECOSUR con su clave de acceso Nota de bibliografía: Incluye bibliografía e índice: páginas 328-333 Número de sistema: 56407Contenidos: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 | ECO400564079426 |
Incluye bibliografía e índice: páginas 328-333
1. Physical geomorphology.. 2. Physical background.. 3. Mechanics of slope formation.. 4. River bed processes.. 5. Development of drainage basins.. 6. Theory of aquatic effects.. 7. Niveal effects.. 8. Theory of Aeolian features.. 9. Theory of some special features.. Subject Index
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The surface features of the Earth are commonly split into two cate gories, the first of which comprises those features that are due to processes occurring inside the solid Earth (endogenetic features) and the second those that are due to processes occurring outside the solid Earth (exogenetic features). Specifically, the endogenetic features are treated in the science of geodynamics, the exogenetic features in the science of geomorphology. I have treated the theoretical aspects of the endogenetic features in my "Principles of Geodynamics", and it is my aim to supplement my earlier book with a discussion of the theory of the exogenetic features. It is my hope that the two books will together present a reasonably coherent, if necessarily incomplete, account of theoretical geology. Contrary to endogenetic phenomena, exogenetic processes can often be directly observed as they occur: the action of a river, the development of a slope and the evolution of a shore platform are all sufficiently rapid so that they can be seen as they take place. This has the result that in geomorphology one is generally on much less speculative ground regard ing the mechanics of the processes at work than one is in geodynamics. eng
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