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dc.creatorAdams, John
dc.date1981-06-30
dc.identifierhttps://bulletin.nzsee.org.nz/index.php/bnzsee/article/view/985
dc.identifier10.5459/bnzsee.14.2.93-95
dc.descriptionEarthquake-triggered landslides pose two indirect hazards to large dams: dam collapse due to upstream dam failure, and reservoir infilling by earthquake-generated sediment. The
 Buller earthquake generated sediment equivalent to 800 years of normal erosion in the Karamea catchment. The effects of this and other historic earthquakes in New Zealand indicate the magnitude of the hazard to present dams and may aid in the safe design of future dams.en-US
dc.formatapplication/pdf
dc.languageeng
dc.publisherNew Zealand Society for Earthquake Engineeringen-US
dc.relationhttps://bulletin.nzsee.org.nz/index.php/bnzsee/article/view/985/961
dc.rightsCopyright (c) 1981 John Adamsen-US
dc.rightshttps://creativecommons.org/licenses/by/4.0en-US
dc.sourceBulletin of the New Zealand Society for Earthquake Engineering; Vol 14 No 2 (1981); 93-95en-US
dc.source2324-1543
dc.source1174-9857
dc.titleEarthquakes, landslides, and large dams in New Zealanden-US
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:eu-repo/semantics/publishedVersion
dc.typeArticleen-US


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