Juneau Area Avalanche Advisory
2006-03-26
Mt. Stewart
by Bill Glude, SAAC Observer
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We returned to the same slope on Mt. Stewart that we tested three days ago and found the bond between the snow layer from a week ago and the underlying icy melt-freeze crust at 91.3cm had gained enough strength in most places to no longer be sensitive or easily triggerable. But one test in a patch of facets still fractured at a high energy Quality 1 on a first gentle jump, a value of only 4, indicating that there are still tender spots out there.

The 10cm layer of moist new snow at 120cm from yesterday afternoon and last night was much more sensitive, fracturing on approach at a high energy Quality 1 on nearly every test block. It also fractured easily on parallel tracks and switchback tests, but was not quite weak or loaded enough to release on uncut slopes.

We did an extra set of AK Blocks sized to the weights of our two testers for our ongoing AK Block research project, so had a total of ten large blocks today.

We rode with strong precautions, because even a thin layer of high density snow can have serious consequences if an entire bowl of it releases. The snow was softer and smoother riding than the breakable crust we found three days ago.

The instability we found will tend to settle out and diminish quickly in the mild temperatures this week, but there may be tender spots persisting in some areas. Backcountry travelers should take care with routefinding, evaluation of consequences, and strict one at a time travel.

Large slides reaching developed areas are not likely.

Keep an eye out for abrupt thaw, heavy rain, or new snow. Any of these factors will increase the avalanche danger again.

Field Notes
Photos
Tyler Gress takes notes as we prepare to shear the first block set, all on a 42° slope angle.
Bill Glude leaps extra hard to fracture the remaining chunk of the 91.3cm layer after an incomplete Quality 3 shear. Tyler Gress photo.

Our block tests three days ago on the immediately adjacent section of the slope sheared on 4 to 5 values, the first gentle or second hard jump, at high energy Quality 1 to 2. Today the same layer sheared mostly on 6 to 7 values, multiple hard jumps or no fracture at all, all at a low energy Quality 3.

One AK Block in the second set today went at 4, the first gentle jump, at a high energy Quality 1. It was a perfect illustration of the spatial variability of snow, fracturing easily due to a patch of slippery faceted grains that had not been blown off the melt-freeze crust as it had on all the other blocks.

Tyler Gress fractures the 120cm layer of moist new snow from yesterday afternoon and last night. It went at a value of 2 on all our tests except one on pair a flatter 35° slope, where it settled on approach and bonded enough to not fracture at all. In most cases, it went at a high energy Quality 1.

The same layer was very active on parallel tracks and switchback tests, fracturing and sliding easily. But it did not have quite enough load to release on any uncut slopes.

It was nonetheless tender enough that we practiced maximum risk reduction travel, choosing our terrain with care, descending one at a time, and clearing the slope entirely before signaling the next person.

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