After a precip event early last week in which rain line rose close to the tops of the peaks in the Southern Wallowas, natural wet loose avalanches were observed. The storm finished cool, formed a stout rain crust as 2 inches of light snow fell on top. This caused widespread natural dry loose on steep slopes with the ‘dust on crust’ effect.
On Saturday, moderate to strong winds from the NW stripped the new snow away and back to the rain crust, and loaded Southern aspects at start zones. Intentionally triggered a 30 ft wide, 3 in deep windslab on SSE slope near an exposed ridgetop at 7,500 ft. Many other small isolated wind pockets were observed to have slid naturally on southeast aspects. Smaller wet loose slides were observed and experienced on steep SW slopes by mid afternoon Monday.
Beyond the smaller avalanche concerns, the snow surface in many places has been stripped back to the rain crust and makes for challenging riding and exposed conditions.
Problem | Location | Distribution | Sensitivity | Size | Comments |
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Layer Depth/Date: 2-4 in S-SE aspects near tree line and alpine |
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Layer Depth/Date: - |