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Leirfallet ved Knivsvik i Hurum 1940.

dc.contributor.authorHolmsen, Per
dc.coverage.spatial18142 Drøbak
dc.date.accessioned2020-08-26T12:39:48Z
dc.date.available2020-08-26T12:39:48Z
dc.date.issued1946
dc.identifier.urihttps://hdl.handle.net/11250/2674571
dc.description.abstractIn the night preceding to October 11th, 1940, a clay-slide took place by Knivsvik near Drammen. This was a typical clay-slide; some liquid clay (\"Kvikkleire\") flowed down a brooklet called Knivsvikbekken. Most of the displaced territory, however, only settled in the way shown on the photo. This phenomenon supports the theory of \"cylindric sliding surfaces\". Further detailes are lacking.
dc.language.isonor
dc.relation.ispartofseriesNGU (167)
dc.rightsNavngivelse 4.0 Internasjonal
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/deed.no
dc.subjectAVSETNING
dc.subjectLEIR
dc.subjectSKREDAVSETNING
dc.subjectSKREDFORM
dc.subjectKVIKKLEIRE
dc.subjectGEOLOGISK RISIKO
dc.titleLeirfallet ved Knivsvik i Hurum 1940.
dc.typeJournal article
dc.description.localcode35462
dc.source.pagenumber12-13


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Navngivelse 4.0 Internasjonal
Except where otherwise noted, this item's license is described as Navngivelse 4.0 Internasjonal