02-13 Mt Troy - Showboat Area

We did a quick reconaissance today to the Mt Troy - Showboat area to see how the weak layers are bonding and how the new light snow from the last two days is behaving.

Though we found some low to medium block test values and a fairly reactive, poorly bonded surface layer, extensive slope tests throughout the area by many parties seemed to be producing no slab releases. We saw only small to moderate sized sluffs.

We did see some examples of parties choosing hazardous routes when much lower risk routes were readily available close by. Remember, going straight up or traversing right up heavily loaded 40°+ slopes is generally a poor choice. Look around, a nearby windswept ridge or rib usually offers much easier trailbreaking and lower risk. Stay spread out too, you are especially vulnerable to avalanches when you are climbing.

Surface snow quality was good. But the facets and surface hoar that are forming in this clear weather will bond poorly to new snow, and the weak layers we found that are not reacting in slope tests now are likely to become active again when the next big load or thaw hits.

The weak test results are an indicator that low risk travel procedures should continue to be used, and that there may be some weaker areas. Watch especially for any signs of windloading.

The surface layer shears off the AK Block as Jimmy Ord steps onto it (AK2 Q2, average shear) on a 38° slope. His skis sank through the surface layer on the Rutschblock, as is common with low density surface layers, so it took a couple more jumps before it went, but the surface layer was still poorly bonded to the underlying snow. It also ripped out all the undermined area with a clean and fast fracture in the slab test, scoring a #2.

Yet slope tests resulted only in sluffs. It appears that the surface layer is just faceted enough, just low density enough, and just bonded enough for it to not produce slabs at its current loading level. Any wind action or further loading is likely to tip it toward instability.

The windslab beneath the surface layer of low density snow fractured on the second, harder jump in both this AK Block and the Rutschblock test (AK5 and RB5, both Q2, average shears) on 38°. This layer showed less fracture propagation in the slab test, ripping out less than half of the area undermined somewhat irregularly (#4). It is a weakness to watch, but does not appear to have a critical load.
Marc Scholten tests the slope and pronounces it turnable. We did kick loose some small sluffs.
Marc Scholten cranks a telemark with full camera pack.
Larry Musarra tests the shaded lower elevation slopes, where the new snow layer is thinner and contains more facets and surface hoar.