Landslides And Their Control (PDF)
Czechoslovak Academy of Sciences
(Sprache: Englisch)
Landslides and Their Control provides information on slope stability; the origin of slope movements; and methods on how they are investigated, controlled, and prevented.
The book covers topics such as soil and rock mechanics; the influence of ground water...
The book covers topics such as soil and rock mechanics; the influence of ground water...
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Landslides and Their Control provides information on slope stability; the origin of slope movements; and methods on how they are investigated, controlled, and prevented.
The book covers topics such as soil and rock mechanics; the influence of ground water on landslides; as well as other factors that produce sliding movement. The book also includes the different types of landslides as well as examples from different territories; its investigation, interpretation of stability, and stability analysis; and corrective measures involved.
The monograph is recommended for geologists who would like to know more about the nature of landslides and how they can be prevented, especially those who work in service for the government.
The book covers topics such as soil and rock mechanics; the influence of ground water on landslides; as well as other factors that produce sliding movement. The book also includes the different types of landslides as well as examples from different territories; its investigation, interpretation of stability, and stability analysis; and corrective measures involved.
The monograph is recommended for geologists who would like to know more about the nature of landslides and how they can be prevented, especially those who work in service for the government.
Bibliographische Angaben
- Autor: Quido Zaruba
- 1969, 214 Seiten, Englisch
- Verlag: Elsevier Science & Techn.
- ISBN-10: 0444601775
- ISBN-13: 9780444601773
- Erscheinungsdatum: 01.01.1969
Abhängig von Bildschirmgröße und eingestellter Schriftgröße kann die Seitenzahl auf Ihrem Lesegerät variieren.
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- Größe: 27 MB
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Englisch
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