Zobrazeno 1 - 10
of 64
pro vyhledávání: '"W.Z. Savage"'
Autor:
W.Z. Savage, J.W. God
Publikováno v:
Landslides ISBN: 9780203749227
Autor:
W.Z. Savage, J. Wasowski
Publikováno v:
Engineering geology 83 (2006): 4–21. doi:10.1016/j.enggeo.2005.06.024
info:cnr-pdr/source/autori:Savage W.; Wasowski J./titolo:A Plastic Flow Model for the Acquara-Vadoncello Landslide in Senerchia, Southern Italy./doi:10.1016%2Fj.enggeo.2005.06.024/rivista:Engineering geology/anno:2006/pagina_da:4/pagina_a:21/intervallo_pagine:4–21/volume:83
info:cnr-pdr/source/autori:Savage W.; Wasowski J./titolo:A Plastic Flow Model for the Acquara-Vadoncello Landslide in Senerchia, Southern Italy./doi:10.1016%2Fj.enggeo.2005.06.024/rivista:Engineering geology/anno:2006/pagina_da:4/pagina_a:21/intervallo_pagine:4–21/volume:83
A previously developed model for stress and velocity fields in two-dimensional Coulomb plastic materials under self-weight and pore pressure predicts that long, shallow landslides develop slip surfaces that manifest themselves as normal faults and no
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a65b250aedda84aef69f6a2120ebce2a
https://publications.cnr.it/doc/41540
https://publications.cnr.it/doc/41540
A preliminary finite-element analysis of a shallow landslide in the Alki area of Seattle, Washington
Autor:
S. Debray, W.Z. Savage
Publikováno v:
Open-File Report.
Publikováno v:
Open-File Report.
The Clear Creek Forks landslide near Central City, Colorado, threatens a major highway junction in Colorado's Front Range. Movement of the landslide was first reported during the mid-1940's when highway engineers noted deformation in bridges at the b
Autor:
E.L. Harp, W.Z. Savage
Publikováno v:
Open-File Report.
Publikováno v:
Open-File Report.
Autor:
P.S. Powers, W.Z. Savage
Publikováno v:
Open-File Report.
Publikováno v:
Open-File Report.
Autor:
W.Z. Savage
Publikováno v:
Open-File Report.
Publikováno v:
Professional Paper.
Gravitational spreading of steep-sided ridges products characteristic geomorphic forms including grabens and depressions along ridge crests, trenches, and uphill-facing, as well as downhill-facing scarps, on the mountain flanks, and outward bulging o