http://www.cnr.it/ontology/cnr/individuo/prodotto/ID271424
Debris Flow on a Seasonally Frozen Rupture Surface at Moose Lake, British Columbia (Contributo in volume (capitolo o saggio))
- Type
- Label
- Debris Flow on a Seasonally Frozen Rupture Surface at Moose Lake, British Columbia (Contributo in volume (capitolo o saggio)) (literal)
- Anno
- 2014-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1007/978-3-319-00867-7_19 (literal)
- Alternative label
Geertsema Marten (1), Hees Menno (1), Chiarle Marta (2), Hayek Jennifer (1) (2014)
Debris Flow on a Seasonally Frozen Rupture Surface at Moose Lake, British Columbia
Springer International Publishing, CH-6330 Cham (ZG) (Svizzera) in Landslides in Cold Regions in the Context of Climate Change, 2014
(literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
- Geertsema Marten (1), Hees Menno (1), Chiarle Marta (2), Hayek Jennifer (1) (literal)
- Pagina inizio
- Pagina fine
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#url
- http://dx.doi.org/10.1007/978-3-319-00867-7_19 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#titoloVolume
- Landslides in Cold Regions in the Context of Climate Change (literal)
- Note
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
- 1. Ministry of Forests, Lands and Natural Resource Operations, Prince George, BC, Canada
2. Consiglio Nazionale delle Ricerche--Istituto di Ricerca per la Protezione Idrogeologica U.O.S, Torino, Italy (literal)
- Titolo
- Debris Flow on a Seasonally Frozen Rupture Surface at Moose Lake, British Columbia (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#isbn
- 978-3-319-00866-0 (literal)
- Abstract
- In early month of November 2007, a 1.4 km debris flow initiated on a steep south-facing slope above Moose Lake in Mount Robson Provincial Park, British Columbia. Snow meltwater was likely concentrated along a shallow seasonally frozen rupture surface, generating high pore water pressure. The debris flow bifurcated into two concentrated gullies before distributing as a debris flood on a snow-covered fan. The debris flow crossed a twin pipeline corridor and came to rest in a ditch against a highway berm. There was no damage to infrastructure. In many ways, the landslide resembles skin flows described in permafrost zones. (literal)
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