Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2–2.5
Large and unusual avalanches, signs of instability, and a poor snowpack structure are all indicators of a persistent slab avalanche problem. Weak upper layers developed during the January drought and are now coated with 2-4 feet of snow. The snowpack has had a couple days to adjust since the storm ended, when we saw multiple human-triggered and natural avalanches, and now it's just waiting for the added weight of a human to stress the weak layer enough to avalanche.
It's hard to identify where exactly you might find this weakness, due to the unusual patchwork of layers that formed during the January drought. Structures vary across the zone, and even across the same slope. Big triggers like a snowmobile or group of people could trigger an avalanche where the weight of a single person might not. If you do trigger an avalanche, it could propagate widely, release in adjacent terrain, from the middle, or maybe even from below a slope.
Don't ignore signs of instability. But, don't expect to experience any signs of instability before you trigger one of these avalanches- the usual indicators like whumphing or shooting cracks may not happen. Snow pits likely don't paint the whole picture, as the weakness is very inconsistent even on a small scale.
You might be able to get away with stepping out onto steep slopes without result, but maybe the next slope over is where you might trigger an avalanche that could kill you. It's hard to tell exactly where an avalanche could happen. If you don't want to risk being caught in one of these avalanches, avoid traveling on large, steep slopes. If in doubt, avoid terrain beneath large steep slopes as well.
(2/3/2025)
Avalanche control work on Monday morning produced this large slab avalanche. The crown was estimated to be around 4' deep. It likely failed at the old-new interface or in weak snow, faceted snow below it.
(SS-AL-D2-O)
Photo: Mount Baker Ski Area