Storm Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Storm slabs have been gradually building since the 4th of April, adding up to 1-2 feet above 3000'. This new snow has fallen on temperature crusts in most areas except for high elevation North facing terrain where near surface facets and surface hoar may be present at the interface. Where the new snow overlies a crust good bonding has been observed. Where the new snow overlies faceted snow on high sheltered north facing terrain human triggered avalanches remain possible up to the depth of the new snow. Human triggered avalanches on the nose of Crudbusters on the 9th and Crybabies on Billy Mitchell yesterday fit this pattern. If travelling in consequential terrain that is high and North a slope by slope assessment is reccommended as near surface facet distribution is likely to be spotty.
Aside from the interface of the new snow there is also the possibility of weaknessess within the storm slab created by changes in wind or temperature over the last week. Yesterday saw an increase in south wind with active snow transport along ridgetops. Watch for freshly loaded pockets of wind slab that will be possible for a person to trigger.
Pay attention to your aspect, the depth and consistency of the new snow and search for faceted snow at the interface when traveling at upper elevations. Try not to ignore signs like shooting cracks and collapsing, these are signs that a slope is unstable. Wind loaded snow will be the most likely hazard to encounter and faceted snow at the base of the storm slab will create larger avalanches with more potential for consequences.
Skier triggered avalanche on the Nose of Crudbusters. 20 inches deep. SS-ASu-R3-D2-I
Photo: Oliver