Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2
Faceted weak layers from Jan/Feb are capped by dense slabs from snow we received at the beginning of March. As we push further away from the last significant loading event, it's becoming more stubborn to trigger an avalanche but not impossible. Although there's a "lower" likelihood of triggering a slide the consequences are still high as last week's very large natural avalanches showed us. Avoid likely trigger points on the margins of the slab, near rock outcroppings where you're more likely to impact these deeper weak layers. Obvious signs of instability like shooting cracks and loud audible collapses may or may not be present. It also may not be the first or second person on the slope to trigger an avalanche, but may just take finding that right trigger point to release an avalanche.
Faceted weak layers that formed over dry periods during Jan/Feb are now capped by dense slabs from storms at the end of Feb and early March leading to this poor snowpack structure of strong over weak.