Schneedecke

Observation: Bonner Ridge

Joey DempsterProvo
Auf der Karte ansehen

Quick report

Red Flags
Heavy Snowfall, Cracking
Red Flags Comment
<p>1. Lots of new water weight on a snow surface that was subjected to several very cold nights and developed some facets. 2. Top several inches of snow this morning was cracking easily and was reactive in tests.</p>

The ECT result was a bit worrisome, but it was shallow. If more snow piled up on it during the day, if that layer was deeper up higher, or if wind transported snow loaded on top of it, it could easily fail and produce slab avalanches. Underneath that, the new snow was well behaved, at least at the mid elevation sheltered terrain that I observed. I felt comfortable on the 30 degree slope, but would not have skied anything steeper today. I feel like this particular weakness will heal quickly. On Tuesday morning, I would expect to see less cracking in the top of the snowpack, but I would be on the lookout for it, particularly since it could be buried more deeply after a few more hours of snowfall.

I did not observe any weakness below this in the new snow.

Winds were obviously high above so I would assume that the avalanche hazard was higher up above on the ridges, and will remain so tomorrow, but 30 degree sheltered slopes should have a hazard rating at least 1 step lower than the ridges tomorrow. (i.e. if considerable, these slopes will have a moderate hazard)

Snowpack

Instability Comment
<p>I had just enough time to get to 9000 feet this morning for a look around. In non wind affected terrain, there was an obvious density inversion at about 5-6 inches down in the new snow. This top layer was cracking easily on rollovers and switchback corners. An ECT on a 33 degree sheltered slope well down off the ridge produced a partial fracture (ECTN11) at 11. It did not run cleanly, but the fracture did propagate. </p>

2' depth is for the Sat/Sun/Mon total.  It's hard to tell exactly where the boundary is between the first and second systems.  In any case the interface between the two does not appear to be a critical discontinuity.  Overall the new snow was medium density.  However, there were a few palpable density changes that could be felt when pole probing.  Only the top layer was reactive, however.  All lower density shifts seemed to be adhering to one another.