THREE SNOWMOBILERS CAUGHT, ONE KILLED IN MONTANA AVALANCHE March 9th, 1996 Three snowmobilers from South Dakota were caught in a large avalanche they triggered while riding in the vicinity of Sheep Point, located approximately 12 miles northwest of West Yellowstone, Montana. The avalanche released in a northeast facing bowl at an elevation of 9500 feet. The slide was 3 to 5 feet deep, 1200 feet across, ran approximately 800 vertical feet, and fractured around several rock ridges and cliff bands. The slope angles in the bowl ranged from 35 to 40+ degrees with steeper angles in the cliff bands. Montana has seen variable weather conditions this winter, ranging from subzero cold to mountain temperatures in the 40's with rarely much in between. A clear spell in late December resulted in the formation of a widespread weak layer. Subsequent burial of this layer in January led to a number of avalanche incidents. The end of January brought bitter cold, with nighttime temperatures down to 47 below in West Yellowstone. After a little more snow, the week of February 11th was warm and dry. During the week of February 18th, approximately 3 feet of new snow fell in the mountains around West Yellowstone, with associated strong southwesterly winds. On February 25th, a snowmobiler was killed in an avalanche on Lionhead, which is approximately 5 miles of advanced snowmobile riding southeast of Sheep Point. Very little precipitation fell in the area during the last week of February. Extrapolating data from a couple National Resource Conservation Service SNOTEL sites, it looks like about 2 inches of snow water equivalent fell at Lionhead during March 3-5, with less than 0.2 of an inch falling from March 6-9. Field tests conducted on Saturday, on Lionhead, indicated fairly stable snowpack conditions. However, due to variable snowpack conditions that existed throughout this area, the avalanche advisory for March 9th called the snowpack instability in the Lionhead area moderate on slopes steeper than 40 degrees, with a strong warning to avoid upper elevation slopes near the ridgetops facing from north to east to south that had significant wind slabs deposited on them by westerly winds that had blown earlier in the week. On Saturday, a large group of snowmobilers were riding in the Sheep Point area, when three riders triggered an avalanche at approximately 1130. One rider was able to ride off of the debris, one rider was knocked off of his sled, and one rider was buried approximately 4 feet deep. We were unable to interview the survivors, so it is unclear exactly where the people were when they triggered the slide, and what kind of self rescue efforts were undertaken. The victim was eventually located by an organized search party that had been dispatched from West Yellowstone. The body was located by a spot probe only a few minutes after the search party arrived at approximately 1400 hrs. The body was located near some trees, approximately 20 feet upslope from his snowmachine which was on the surface of the debris. On Monday, March 11th, Karl Birkeland and I investigated the avalanche site. In areas along the crown face, it appeared that the avalanche failed on two layers of faceted grains buried deep in the snowpack. Though these layers didn't appear to be very weak, we did find areas with weak faceted and cup shaped crystals where the snowpack was relatively thin. It is possible that the the riders "hit" an area on the slope that had a relatively thin snowpack and weak faceted crystals. The stress applied to this weak area may have caused local failure, which then spread to the surrounding snowpack, resulting in the large avalanche. If people have questions or comments, they can contact myself or Karl Birkeland at (406) 587-6984. Ron Johnson Avalanche Specialist, Gallatin NF Avalanche Center March 13th, 1996