Structural characterization of rockfall sources in Yosemite Valley from remote sensing data and field surveys
Détails
ID Serval
serval:BIB_6CB718DBA7C3
Type
Actes de conférence (partie): contribution originale à la littérature scientifique, publiée à l'occasion de conférences scientifiques, dans un ouvrage de compte-rendu (proceedings), ou dans l'édition spéciale d'un journal reconnu (conference proceedings).
Collection
Publications
Institution
Titre
Structural characterization of rockfall sources in Yosemite Valley from remote sensing data and field surveys
Titre de la conférence
Proceedings of the 64th Canadian Geotechnical Conferance and the 14th Pan-American Conference on Soil Mechanics and Geotechnical Engineering
Editeur
Canadian Geotechnical Society
Statut éditorial
Publié
Date de publication
2011
Volume
54
Langue
anglais
Notes
Matasci2011
Résumé
Yosemite Valley poses significant rockfall hazard and related risk
due to its glacially steepened walls and approximately 4 million
visitors annually. To assess rockfall hazard, it is necessary to
evaluate the geologic structure that contributes to the destabilization
of rockfall sources and locate the most probable future source areas.
Coupling new remote sensing techniques (Terrestrial Laser Scanning,
Aerial Laser Scanning) and traditional field surveys, we investigated
the regional geologic and structural setting, the orientation of
the primary discontinuity sets for large areas of Yosemite Valley,
and the specific discontinuity sets present at active rockfall sources.
This information, combined with better understanding of the geologic
processes that contribute to the progressive destabilization and
triggering of granitic rock slabs, contributes to a more accurate
rockfall susceptibility assessment for Yosemite Valley and elsewhere.
due to its glacially steepened walls and approximately 4 million
visitors annually. To assess rockfall hazard, it is necessary to
evaluate the geologic structure that contributes to the destabilization
of rockfall sources and locate the most probable future source areas.
Coupling new remote sensing techniques (Terrestrial Laser Scanning,
Aerial Laser Scanning) and traditional field surveys, we investigated
the regional geologic and structural setting, the orientation of
the primary discontinuity sets for large areas of Yosemite Valley,
and the specific discontinuity sets present at active rockfall sources.
This information, combined with better understanding of the geologic
processes that contribute to the progressive destabilization and
triggering of granitic rock slabs, contributes to a more accurate
rockfall susceptibility assessment for Yosemite Valley and elsewhere.
Création de la notice
25/11/2013 17:26
Dernière modification de la notice
20/08/2019 15:26
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