Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 3
Poor snowpack structure remains on slopes that face W-N-E. Abundant snowfall in March has built a well connected dense slab 2-3 feet thick above weak layers of faceted snow. These layers have been very slow to heal this season due to relatively shallow snow depths. With each passing day, it is becoming harder to trigger an avalanche on these weak layers. You will not see signs of instability today, and the snowpack will feel strong beneath your skis. Even though the chances of triggering an avalanche are becoming less, we have a structure that most snow professionals won't trust their lives with. The most suspect areas are very steep northerly aspects, and likely trigger points are steep convexities, thin slab margins, and shallow rocky areas. If you are biting off pieces of avalanche terrain, choose smooth planar slopes with clean run-out zones.
I dug this pit on Sunday on a north-facing slope. The overlying slab is dense, with mostly 4F to 1F snow. A dense slab like this will most likely bridge the weight of a skier, but if you find a shallower snowpack zone, the weight of a human can trigger an avalanche on the weak fist-density facets. A triggered slide would likely take out the entire season's snowpack down to the depth hoar.