Storm produced snow 2/12 -2/13. A cloud deck of ~5000ft burned off around noon leading to few clouds.
One human triggered wind slab avalanche, D1, occurred in a steep gully and our impression was that if an avalanche were to occur anywhere it would occur in a place like that. The other slab avalanche was more of a storm slab, possibly with a bit of wind influence. We were surprised we only saw one of those, as that slope was very similar to many others that had tracks on it.
We started our day in near treeline terrain until the clouds burned off. Snow was heavy, but excellent riding. We didn't see signs of instability, but with flat light and/or obscured skies and the recent storm, travel was conservative.
When skies cleared, riders rapidly stepped out onto steeper slopes, and we were surprised with how little avalanche activity we saw. See avalanche ob comments. Generally, most surfaces above approx 5500' were wind textured, and many surfaces were slightly firmer from about 6000ft and up.
Around 1-2ft of storm snow was present over the older layer in pits, although it was very difficult to identify the new/old interface. Failures were not consistent at that location, and hardness differences were barely discernable.
The upper-elevation south-facing terrain wasn't really affected by the sun once the skies cleared. Upon descent at 1600hrs, steep west-facing terrain from about 4000ft and down was moist.
Problem | Location | Distribution | Sensitivity | Size | Comments |
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Storm Slab |
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Layer Depth/Date: 45cm (new/old interface) |
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Wind Slab |
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Layer Depth/Date: ~30cm, within the new snow. |