Persistent Slabs
- Hochgebirge
- Waldgrenze
- Unterhalb der Waldgrenze
- Wahrscheinlichkeit
- Likely
- Größe
- 1.5–3
Most upper elevation slopes, and some mid elevation slopes, have at least one weak layer buried below a 1-3 foot slab. These layers have produced natural and human triggered avalanches over the last week with Seeley Lake producing the largest avalanches.
The most dangerous slopes right now are at upper elevation north aspects where 2 distinct and reactive layers of surface hoar are buried. Surface hoar is a particularly nasty weak layer that can remain reactive long after it gets buried and is responsible for many avalanche accidents across the west.
As you move onto south facing or solar slopes, you will encounter buried facet/crust combinations. These layers have shown decreasing reactivity, but poor snowpack structure remains and snowpit test results still show potential for fracture propagation and avalanches.
To identify the problem, dig in the snow. If you find a slab of firm snow on top of weak or sugary snow, avalanches are possible. Surface hoar will present as a thin grey line that runs across the snowpit wall. If you find this, be especially cautious as surface hoar can produce avalanches on slopes down to 30 degrees in slope ang
You may not see any signs of instability like cracking, whumfing, or collapsing before you trigger an avalanche today. It will be possible to trigger avalanches remotely from below, above, or to the side of slopes. Just because you see tracks on a slope does not mean the slope is stable or incapable of producing an avalanche. In conditions like this, the 2nd, 3rd, or 10th rider on a slope can be the one to trigger the avalanche if they find the right trigger point.
Photo: Cam Mackenzie