We dug one snowpit. Info is below:
Location: Northside of McHugh
Elevation: 2,600'
Aspect: North
Slope: 20 degrees
Test: We did get ECTN24 on the top layer of near-surface facets. If this layer gets buried deeper it could be more of a concern.
All the 1' of fresh snow from last week has been moved around by the wind in the last two major wind events. One of the wind events was from the southeast and the other from the northeast. The cross-loading has caused some loading in areas that don't normally get loaded (midslope or mid-run).
I decided to talk through our decision to not go to Falls Creek in my video for a couple of reasons- wanted to highlight the concern about the wind loading on top of the reactive near-surface facet layer we've been getting propagation on over the last two weeks (see the forecaster Bear Valley or Peak 3 observations for more info). That layer has been spotted at multiple locations throughout the state park and it's not just isolated to just Falls Creek area. Lastly, wanted to bring attention to the overhead hazard at the start of the Falls Creek trailhead (especially with the most recent wind events adding stress to the snow pack) in case the observation generates more human traffic to that spot right now.
Basically, the avalanche hazard has increased with the last wind events and we have some funky wind-loading on top of a reactive near-surface facet layer.