Persistent Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 2
Monday's NE wind event produced several large, natural persistent slab avalanches in the Boulder Mountains (see Observation and photos below). These avalanches failed on mostly W facing slopes that had especially thin, weak snowpacks and are typically scoured by the predominant winds. Most of the activity occurred hundreds of feet below ridgelines. NE wind events are uncommon, and uncommon weather events can produce uncommon avalanches.
Ben visited an avalanche that released Sunday in the White Cloud Mtns (photo to right). It broke over 500 feet wide, 4-6 feet deep, and wiped out the majority of the season’s snowpack, covering snowmobile tracks from the previous day. It is unclear if this avalanche failed naturally or was triggered remotely from below.
What are the common threads in the recent avalanche activity?
- Steep: slopes in prime-time avalanche terrain around 35-45 degrees.
- Wind-loaded: heavily wind-loaded by recent wind events.
- Alpine flavor: complex terrain with rock ribs, cliff bands, or minor ridges near the avalanche crowns or flanks.
Watch for signs of recent wind loading like ripples, dunes, or wave-like patterns. If you are riding in soft snow and it suddenly gets stiff or hard, it's time to call a time out and carefully evaluate the terrain you're in. The consequences of a triggering a destructive, 2-6 foot thick, persistent slab would be severe. Be aware that even if you aren’t in steep terrain yourself, the snow that you are traveling on may be connected to that sort of terrain above you.