Deep Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2.5–3.5
Continue to put a wide buffer between where you travel and large start zones and avalanche paths that are suspect for this dangerous avalanche problem. If you hit the trigger point for the persistent weak layer, the resulting avalanche could be destructive and unsurvivable. These avalanches may give little warning and may be difficult to trigger on some slopes. You may be able to trigger them easier near Harts Pass and drainages east of the Cascade crest.
While the late January facets had been dormant, they've remained weak on shaded aspects at middle and upper elevations. A huge load of recent snow has now made it easier to trigger avalanches. A few deep natural crowns in the Hairpin valley and an avalanche triggered near Hart's Pass on March 3rd (see photo and details below) suggest that this layer may have been reactivated during the last storm. You can find this layer about 5ft deep and sandwiched between two crumbly crusts. Sudden or propagating results in snowpack tests can help you identify the layer. Further east it's closer to the surface and not far below the most recent storm interface from Feb 26th.
(3/3/2022)
A very large (D2.5) and widely propagating slab avalanche was triggered by a snowmobile on March 3rd. The crown is estimated at roughly 5ft deep. 6600-6800ft, NE, near Harts Pass
Photo: Drew Lovell