Forecast for the Logan Area Mountains

Toby Weed
Issued by Toby Weed on
Wednesday morning, November 5, 2025

We're back, getting ready for avalanche season, and winter is rapidly approaching! Thanks for checking in. We will restart avalanche forecasting operations as soon as there is enough snow to cover the rocks, so stay tuned. In the meantime, now is a good time to get out your rescue gear, be sure it's all in working order, replace batteries, update software, and practice companion rescue techniques with your backcountry partners.

https://utahavalanchecenter.org/sites/default/files/images/observations/2025-26/IMG_3178.JPG

A little bit of snow accumulated on upper elevation slopes in the Bear River Range in late October, but only a few inches remain on the ground in north-facing terrain.

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Moderate
Considerable
High
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Special Announcements
Weather and Snow
A cold front will push through the Logan Forecast Zone late Wednesday night through Thursday, bringing a round of precipitation in the form of high elevation snowfall and valley rain. 2 to 5 inches of snow (.25" to .65" SWE) could accumulate in upper elevation terrain near the State Line. Much cooler(though near seasonal) temperatures will follow in the wake of the cold front and are expected to persist into the upcoming weekend before a ridge rebuilds early next week.
Recent Avalanches
For observations and avalanche activity in the Logan Zone, go HERE
Additional Information

For more information, visit the UAC weather page here: UAC Weather Page For Logan-specific weather, go here: Logan Mountain Weather

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This forecast is from the U.S.D.A. Forest Service, which is solely responsible for its content. This forecast describes general avalanche conditions and local variations always occur.

General Announcements
This information does not apply to developed ski areas or highways where avalanche control is normally done. This forecast is from the U.S.D.A. Forest Service, which is solely responsible for its content. This forecast describes general avalanche conditions and local variations always occur.