Cement Mountain loop

CB Avalanche Center 2020-21 Observations

Date of Observation: 02/23/2021
Name: Jack Caprio and Eric Murrow

Zone: Southeast Mountains
Location: North Cement Mountain
Aspect: North, North East, East, West, North West
Elevation: 9,000′-12,200


Avalanches: Observed a number of avalanches on Cement Mountain of varying ages from the past month.  Included images for avalanches that likely failed around the Feb 13/14 time frame.  Most of these avalanches failed on drifted features with two below treeline on non-drifted slopes.  Looking around leeward features in Southeast Mountains did not see any other recent avalanches.  While driving pavement in afternoon, I spotted a couple very small loose avalanche on Gothic Mountain coming out of steep, rocky southerly features.
Weather: A cold early morning in the canyon quickly gave way to warm, sunny weather. Above treeline, W and NW winds blew at consistent moderate speeds with high gusts.

Snowpack:  Toured up and over Cement Mountain.  This is a relatively shallow snowpack area as it is in the Southeast Mountains and receives less snow volume than other areas in Southeast Mountains due to its location.

Below 10k, the snowpack consisted of generally 80 cms of thin crust/ facet combos. When HS was less than around 80 cm, ski pen was to the ground. As we increased in elevation to about 10K-ish, HS increased above 80 cms to around 100cm and the snowpack thankfully began to support the weight of a skier while breaking trail. We didn’t get any alarming signs of instability as we were making our way up through the trees on N aspects below treeline.

As we got near and above treeline, we continued to see W and N winds transport snow onto leeward start zones. A snowpit test on a slightly windloaded, NE-facing aspect near treeline produced moderate propagating results. We did get one large rumbling collapse while traveling on ridgeline, adjacent to the NE facing start zones. The collapse did not produce any cracks but it was loud enough to hear over the blustering winds. Much of the avalanche paths we traveled above had already slid during the last 3 weeks. Most of the bed surfaces had not refilled enough to slide again. We chose not to ski any of the slopes that had previously avalanched because of the low quality of skiing, not necessarily avalanche hazard.  Briefly touched a few below treeline sunny slopes that were moist but not wet enough to cause Wet Loose concerns due to winds keeping surfaces relatively cool.