Northern Gallatin

Roughly 2 inches of new snow in the parking lot at Bear Canyon.  Up high on the top of Mt Ellis at 8300 feet there was 6 to 8 inches.  Did a column test and it broke on the new snow layer above the crust about 23 cm down from the top at 3 taps from the elbow.  Then we kept going and got it to fail at the weak layer near the bottom of the snowpack at 6 taps from the shoulder.

We toured down the west side of the Bridger Range on the edge of Truman Gulch and found predictably weak snow on an upper-elevation NW-facing slope. Conditions were variable and transitioned to a thick crust as we moved on to a lower elevation, west-facing slope. By the time we came down the Ramp, the snow was getting wet, we saw roller balls, and we avoided steep, sun-exposed terrain. 

We dug below NW Passage. It was a 135 cm deep snowpack, dry throughout, with Fist plus hard facets and depth hoar making up the foundation (ECTP30, PST 42/100 end at 30 cm from the ground. 

We rode from the Buttermilk trailhead up Denny Creek to Lionhead Ridge, along Lionhead Ridge through Watkins Creek and to the motorized boundary at the head of Targhee Creek. 

There was a ~1" crust at the surface when we left the trailhead, with dry snow beneath. We saw our first wet loose avalanche of the day running around 11 am. By 12:30 there were dozens and many rollerballs. None of them ran particularly far or picked up too much volume.  The snow surface was moist on sunny slopes by late morning, but not more than a few inches down.

We saw one small slab avalanche that occurred since this weekend's snow. It appears to have been triggered by a snowmobile yesterday (4/1/24). It broke 10" to 2 ft deep, 50 ft wide, and ran ~50 vertical feet. It broke on a thin layer of facets beneath the new snow. Digging in the crown, dry facets at the ground were along still present and weak (fist hardness).

Signs of older avalanches were visible beneath the new snow, including one slide that broke in early March. No cracking or collapsing were observed today.

BZN Snow Rangers rode little bear to check boundary signs and see where closure encroachment issues had been occurring. Boy were we pleasantly surprised to see 10 new inches up high from the previous spring storm cycles which had set up nicely with minimal traffic. Snow was wind affected on high ridgetops but not on less exposed midslopes. Temperatures were below freezing in the morning but by 1400 higher temps and direct sunlight started to cause some roller balls and pinwheeling. We observed no new avalanche activity. There was one pair on a two-seater skandic, and another group of at least two mountain sledders who seemed far above our ability and eluded us despite our best efforts to find them.

200 cm snow depth. Soft on top moving to firm, cohesive layers through the pack. Some weak snow near ground.