dc.contributor.author | Holmsen, Gunnar | |
dc.coverage.spatial | 15211 Orkanger | |
dc.date.accessioned | 2020-08-26T12:39:54Z | |
dc.date.available | 2020-08-26T12:39:54Z | |
dc.date.issued | 1946 | |
dc.identifier.uri | https://hdl.handle.net/11250/2674574 | |
dc.description.abstract | At Nedre Mule in Byneset about 20 km west of Trondheim, a clay slide occurred on the 24th of May 1943, wasting 20 000 sq. m. of cultivated land. The ground slid into the fjord Gulosen. A mud flow was visible in the course of the slide, surrounded by a 8 a 10 m high precipice of firm clay. The locality is only a kilometer or two from the great clay at Brå, described in this puboication serieal no. 132. The district is most disposed to severe land slides. Even a hundred years ago Nedre Mule was hit by a slide, after which the cow stables had to be moved somewhat further back. | |
dc.language.iso | nor | |
dc.relation.ispartofseries | NGU (167) | |
dc.rights | Navngivelse 4.0 Internasjonal | |
dc.rights.uri | http://creativecommons.org/licenses/by/4.0/deed.no | |
dc.subject | LEIR | |
dc.subject | AVSETNING | |
dc.subject | SKREDAVSETNING | |
dc.subject | SKREDFORM | |
dc.subject | KVIKKLEIRE | |
dc.subject | GEOLOGISK RISIKO | |
dc.title | Leirfall på Nedremule, Byneset 1943. | |
dc.type | Journal article | |
dc.description.localcode | 36302 | |
dc.source.pagenumber | 70-71 | |