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Date and time of observation or avalanche occurrence Location Region Observation Type Observation made by Videos Photos
12/02/2018 - 13:30 Ghoulie - Southern Whitefish Range Whitefish Range - Southern (south of Coal Creek) Snowpack Observation Public
12/01/2018 - 18:00 Forecaster Observation- Doris Lakes, Swan Range Swan Range - East Side (Hungry Horse Reservoir access) Snowpack Observation Forecaster
12/01/2018 - 12:30 Big Mountain Whitefish Range - Southern (south of Coal Creek) Snowpack Observation Public
11/27/2018 - 12:00 Forecaster Observation - Big Mountain Summit, Whitefish Range Whitefish Range - Southern (south of Coal Creek) Snowpack Observation Forecaster
11/26/2018 - 20:30 Mount Edwards - Glacier Natl. Park Glacier National Park - McDonald Lake Area Snowpack Observation Public
11/25/2018 - 19:00 jewel basin Snowpack Observation Public
11/25/2018 - 01:15 Red Meadow Pass, Whitefish Range Snowpack Observation Public
11/24/2018 - 14:45 Forecaster Observation - Apgar Range, GNP Glacier National Park - Apgar Range Snowpack Observation Forecaster
11/18/2018 - 15:30 Whitefish Mountain Resort Snowpack Observation Public
11/17/2018 - 20:30 Pinnacle creek to tunnel ridge Flathead Range/Glacier National Park - John F. Stevens Canyon Snowpack Observation Public
11/16/2018 - 13:15 Jewel Basin Snowpack Observation Public
11/13/2018 - 16:15 Forecaster Observation - Beta Lake, Swan Range Swan Range - East Side (Hungry Horse Reservoir access) Snowpack Observation Forecaster
11/13/2018 - 02:00 Mount Marston Lookout Whitefish Range - Southern (south of Coal Creek) Snowpack Observation Public
11/12/2018 - 19:15 Great Northern, Flathead Range Avalanche Observation Public
11/08/2018 - 14:45 Forecaster Observation - Scalplock Mountain, Glacier Park Flathead Range - Middle Fork Corridor Snowpack Observation Forecaster

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The Flathead Avalanche Center cannot vouch for the quality or accuracy of any observations that come from the general public. This map is not a comprehensive map of avalanche activity; events often go unobserved and the frequency and locations of avalanche observations are often biased by accessibility and terrain visibility.

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