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The snow at higher elevations was much more stable than we have seen at similar aspects at lower elevations. There was not the weak surface hoar layer. It also appeared as though the depth hoar had been bridged over by the stronger layers as we were not able to get any results from our compression or extended column tests.
Snow Profile Image:
Location
40° 32' 9.2976" N, 111° 41' 16.332" W
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The snow at higher elevations was much more stable than we have seen at similar aspects at lower elevations. There was not the weak surface hoar layer. It also appeared as though the depth hoar had been bridged over by the stronger layers as we were not able to get any results from our compression or extended column tests.