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Snowpack Observations
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We dug 2 pits at 6700' and 7000' on the west aspects we skied. There was around 20" of new snow from the past 3 days. High winds were recorded 3 or 4 days ago. An extendened column test resulted in no fracture (ECTX).
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During a tour from the top of Coyote at the Mount Shasta Ski Park to the top of Grey Butte:
- Height of new snow (since 02/28) ranged from 70-95cm
- Height of snow ranged from 100-220cm
- No avalanches were observed with visibility up to 10k on the south side of Mount Shasta
- Multiple whumphs occurred near and below treeline
- Wind loading has occurred near and above treeline on N-NE-E-SE-S aspect
- Wind scalloped snow surfaces visible above 8500ft on Mount Shasta
- Hand pits and stability tests conducted near treeline and below treeline on NE, E, SE, S, SW, W aspects revealed the greatest layer concern to be the new snow/ old snow interface. A layer of .5mm rounding facets sitting just below a crust buried 70-95cm below the snow surface produced sudden collapse fractures in compression tests and inconsistent propagation in extended column and propagation saw tests
- The new snow was right side up and low-density
- Ski penetration was 30cm, and boot penetration was 60-80cm
- A .5cm thin zipper crust formed at the snow surface up to 7500ft
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Storm dig out and observations
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test 2
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Old Ski Bowl - Wind Slab & General Conditions Assessment
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Prior to skiing off the summit of McDonald Peak we decided to take a look at the snowpack. At 7100' on a northeast facing slope we dug a pit and conducted a compression test. The total height of snow was 85cm. Most significant result was a CTMSCQ1 on a 15cm thick layer of facets buried by 45cm of new and wind-transported snow. We were able to dig into this layer in our observation wall with ease, pulling out handfuls of faceted snow. Unfortunately we could not conduct an ECT to test for propagation. Throughout the day we had seen no signs of recent avalanches, no whumping or shooting cracks, and no rapid warming. The wind was still light to moderate but no significant transport of snow. After discussion we decided to ski one at a time on a 28 degree slope about 30m from our pit. Another solo skier had skied a 30 degree slope in the same zone multiple times prior to our CT and yielded no results. We skied 2 laps on McDonald before departing this zone. We determined that our unseasonable shallow snowpack combined with well-below average temperatures is what drove the faceting.
On a side note, on Saturday 2/24, Southern Oregon University's AIARE Level 1 course dug a pit on a North facing slope just west of Mount Ashland Ski Area at 7,000. The total height of snow was 140cm. We found a faceted layer at around 80cm down that yielded a CTHPCQ2. We assume that this faceted layer is the same layer we saw on McDonald.








































































Sunny skies and calm westerly winds made for a beautiful tour up Giddy Giddy/Avalanche Gulch today.