Field Report

Aspen - CO

2024/12/05
Lat: 39.148, Lon: -106.965
Backcountry Area: Aspen
Author: Dylan Craaybeek, Brian Lazar
Organization: Forecaster, CAIC

Report Information

Observation Summary

The weak layer is not very weak and the slab is mostly discontinuous across the terrain after the extended dry spell weakened it on most northerly slopes. We had to hunt to find slopes where you might be able to trigger an avalanche and found them on partially wind-loaded terrain features between 11,000 and 12,000 feet on shady slopes in West Willow Creek. Even on these slopes of concern, where there is a prominent weak layer and a cohesive overlying slab, snowpack tests show mixed results from easily propagating failures to stubborn propagating failures to non-propagating failures.

Area Description

Baldy, West Willow Creek

Route Description

Snowmass ski area to Baldy Mountain into West Willow Creek and back into the ski area

Avalanches

Saw an avalanche

Observed dozens of large to very large avalanches from the Thanksgiving Storm natural avalanche cycle. Only avalanches observed in West Willow, Willow, and East Snowmass Creeks were included in this observation.

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Date # Elev Asp Type Trig SizeR SizeD Problem Type Location
11/27/2024
4 >TL NE SS N R2 D2.5 Persistent Slab
11/27/2024
1 >TL N SS N R3 D2 Persistent Slab
11/27/2024
1 TL NE SS N R3 D2 Persistent Slab
11/27/2024
1 >TL SE SS N R1 D2 Persistent Slab
11/27/2024
2 >TL NE SS N R1 D2 Persistent Slab
11/27/2024
1 >TL N SS N R2 D2.5 Persistent Slab
11/27/2024
2 >TL NW SS N R2 D2.5 Persistent Slab
11/27/2024
1 >TL N SS N R2 D2.5 Persistent Slab
11/27/2024
1 >TL NW SS N R2 D2 Persistent Slab
11/27/2024
1 >TL NE SS N R1 D1.5 Storm Slab
11/27/2024
1 >TL E SS N R1 D1.5
11/27/2024
1 >TL E SS N R2 D2.5 Persistent Slab
11/27/2024
1 >TL E SS N R1 D1.5 Persistent Slab
11/27/2024
2 >TL NW SS N R1 D1.5

Snowpack

Cracking: Minor
Collapsing: None

Minor cracking on wind-drifted snow along ridgelines. The snowpack above treeline is very wind-affected with ski and boot penetration often 0 cm with a variable breakable wind crust up to 8cm thick. The near treeline elevation band, roughly between 11,000 and 12,000 feet seems to be the area of most concern where the slab is mostly continuous, close to two feet thick, and rests on a weak layer of faceted grains that showed mixed results in snowpack tests. Although these areas of concern with a slab over a weak layer are getting harder to find and growing more stubborn there are still slopes I would avoid traveling on, especially near treeline and the lower levels of the above treeline elevation band. West Willow Creek also notably did not have any depth hoar present in the areas where we dug and any facets near the ground showed clear signs that they had been rounding for an extended period of time and were well-bonded and mostly rounded. Below about 11,000 feet small surface hoar grains were present on most slopes except for steep, sunny slopes where any surface hoar growth overnight was likely melting in the daytime.

Weather

Few clouds and mostly calm with light gusts from the southwest. No noticeable snow transport today.

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