Bergsturzablagerung vom Rinderhorn
Rappresentazione e statuto
- Colore CMYK
- (0%,0%,0%,100%)
- Rango
- instabilità del terreno
- Uso
- Unità in uso.
- Status
- termine informale
Nomenclatura
- Deutsch
- Bergsturzablagerung vom Rinderhorn
- Français
- Dépôt d'écroulement du Rinderhorn
- Italiano
- Deposito di frana del Rinderhorn
- English
- Rinderhorn rock avalanche deposit
- Origine del nome
- Varianti storiche
-
Bergsturz Rinderhorn = Daubensee-Bergsturz = Bergstürze des Kandertales [p.p.] (Flüeler 2011), Daubensee rock avalanche (Grämiger et al. 2020)
Età
- Geomorfologia
-
- Olocene
- Età alla base
-
- Olocene
- Metodo di datazione
-
9,8 +/-0,5 ka (Grämiger et al. 2016)
Referenze
- Revisione
-
(2016) :
Two early Holocene rock avalanches in the Bernese Alps (Rinderhorn, Switzerland). Geomorphology 268, 207-221
Results reveal that the Daubensee rock avalanche released ~4 millionm3 of limestone sliding fromthewestern crest of the Rinderhorn. Debris ran out across a Lateglacial moraine before reaching the valley bottom and spreading, leaving thin (on average 7 m) deposits across a broad area. The runout resulted in a Fahrböschung angle of 21°. Part of the deposit now lies beneath Lake Daubensee.