Storm Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Possible
- Größe
- 2
This avalanche problem is currently believed to be specific to the Mount Rose portion of the forecast area. This geographic limitation is based on the limited collective snowpit data from around the forecast area pre-storm. This avalanche problem is known to exist on N and NE aspects where a layer of basal facets around 1 foot thick is at the base of the snowpack. Uncertainly exists as to presence/absence of this avalanche problem on NW aspects due to a lack of data. The lower elevation boundary of this avalanche problem is also uncertain due to a lack of available data but might be limited to areas above 8,500' to 8,700'.
A human triggered deep slab avalanche occurred today on Tamarack Pk in Hourglass Bowl, more info is available here. Numerous snowpit tests on other portions of Tamarack Peak today produced unstable results on the basal facet layer. Sensitivity to triggering for this avalanche problem is stubborn and it exists in specific areas. Signs of instability may not be readily observed prior to triggering an avalanche. Conservative terrain selection of slopes less than 30 degrees in steepness and/or avoidance of NW-N-NE aspects are sound mitigation techniques for this avalanche problem.