Storm Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Very Likely
- Size
- 1–2.5
Strong westerly winds will transport today's snowfall into fresh slabs downwind of ridgelines, saddles, and on sidewalls of cross-loaded gullies. These slabs will increase in size and thickness as you gain elevation and the day progresses. Drifts, dunes, and rippled snow surfaces confirm that the wind has been working. Today's blowing snow will be an obvious sign that slabs are forming.
As snow totals increase, storm slabs may develop in locations sheltered from the wind. These will be thinner but may become more widespread than the above-mentioned wind slabs. They can be identified by cracking at the surface in consolidated, dense snow.
Whether you are in sheltered or wind-affected terrain, cracking beneath your machine or boards indicates instability, directing you to lower-angle slopes free of overhead hazards.
Triggering a small surface slab may initiate a much larger avalanche on a buried weak layer described in our persistent slab problem below.
(2/24/2023)
Soft slab avalanches are a threat in sheltered terrain when a Storm Slab avalanche hazard exists.
Photo: Mark Dundas