Eine Plattform für die Wissenschaft: Bauingenieurwesen, Architektur und Urbanistik
Eine Plattform für die Wissenschaft: Bauingenieurwesen, Architektur und Urbanistik
Summary There are many premises both geological and rheological proving that landslides are not sudden phenomena; almost in all cases a long preparatory period precedes the creep of rocks. The creeping zone is adjacent to the potential surface of sliding. Depending on different natural conditions four types of depth creep are observed: planar, rotational, subordinated and compensating. Technical features of those types of depth creep are given. Multi-storeyed landslides are briefly outlined; the need for observations of landslide dynamics is pointed out.
Summary There are many premises both geological and rheological proving that landslides are not sudden phenomena; almost in all cases a long preparatory period precedes the creep of rocks. The creeping zone is adjacent to the potential surface of sliding. Depending on different natural conditions four types of depth creep are observed: planar, rotational, subordinated and compensating. Technical features of those types of depth creep are given. Multi-storeyed landslides are briefly outlined; the need for observations of landslide dynamics is pointed out.
Depth creep of slopes
Georg, Ter-Stepanian (Autor:in)
1974
Aufsatz (Zeitschrift)
Elektronische Ressource
Englisch
BKL:
56.00$jBauwesen: Allgemeines
/
38.58
Geomechanik
/
38.58$jGeomechanik
/
56.20
Ingenieurgeologie, Bodenmechanik
/
56.00
Bauwesen: Allgemeines
/
56.20$jIngenieurgeologie$jBodenmechanik
RVK:
ELIB18
| Online Contents | 1974
On creep flow of natural slopes
| British Library Conference Proceedings | 2000
Stability of slopes undergoing creep deformation
| Engineering Index Backfile | 1969
Creep crack propagation and the progressive failure of slopes
| British Library Conference Proceedings | 1997
Accelerating creep of the slopes of a coal mine
| Springer Verlag | 1987