Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Unlikely
- Size
- 1–2
Weak snow formed during a prolonged dry period in November lies buried one to three feet below the surface of the snowpack on shady slopes with a northerly tilt (W-N-E aspects). Observations of that weak layer in pits has shown that it has remained dry, loose and largely intact, pretty much since it's formation, despite settlement that has stiffened and strengthened the overlying slab. This strengthening of the slab and some subtle changes in the deeper stratigraphy has reduced the number of obvious alerts to its existence such as whoompfing and shooting cracks but has not reduced its tendency to propagate a crack in stability tests, albeit stubbornly.
If venturing into very steep terrain, digging or probing in the snowpack can help you determine where and how deep lies the weak faceted snow. You'll find lots of tracks on steep slopes and generally strong snow. Taking the time to dig is good practice and may be the reality check that you need before center-punching a consequential slope. Skiing or riding on lower angle slopes is a more certain method to avoid triggering what could be a hard slab avalanche up to three feet thick.
Avalanche on the recent (12/24) snow interface in the Big Holes on an east aspect around 8,400 feet.