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TitleLate glacial and Holocene sedimentation and investigation of fiord tsunami potential in lower Howe Sound, British Columbia
AuthorJackson, L E, Jr.; Blais-Stevens, A; Hermanns, R L; Jermyn, C E
SourceEngineering Geology for Society and Territory vol. 4, 2014 p. 59-62, https://doi.org/10.1007/978-3-319-08660-6 12
Year2014
Alt SeriesEarth Sciences Sector, Contribution Series 20140483
PublisherSpringer
Documentserial
Lang.English
Mediapaper; digital; on-line
File formatpdf
ProvinceBritish Columbia
NTS92G/06; 92G/12
AreaHowe Sound
Lat/Long WENS-123.5000 -123.0000 49.7500 49.2500
Subjectssurficial geology/geomorphology; tectonics; geophysics; Holocene; glacial history; glacial deposits; tectonic history; tectonic setting; earthquake risk; slope failures; landslides; debris flows; physiography; fluvial deposits; tsunami; shorelines; shoreline changes; coastal environment; coastal erosion; coastal studies; geophysical surveys; bathymetry; acoustic surveys; acoustic surveys, marine; topography; geological hazards; Quaternary; Cenozoic
Illustrationslocation maps; photographs; profiles; tables; logs
Viewing
Location
 
Natural Resources Canada Library - Ottawa (Earth Sciences)
 
ProgramMarine Geohazards, Public Safety Geoscience
AbstractPreliminary investigation of the history of sedimentation in lower Howe Sound fjord near Vancouver, B.C. indicates that no rock slide capable of generating a destructive displacement wave has occurred during the latter half of the Holocene. Possible rock slide run-out deposits were detected along the western margin of Bowen Island. These could date from any time during the Holocene. Investigation of the adjacent slope suggests it is creeping and is not an imminent large rock slide failure.
GEOSCAN ID295998