Lawinenlagebericht

Sawtooth & Western Smoky Mtns

Sawtooth Avalanche Center
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Lawinengefahr

Thu
Hochgebirge
3 · Erheblich
Waldgrenze
2 · Mässig
Unterhalb
2 · Mässig
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Veraltet — dieser Lagebericht ist last year abgelaufen. Du siehst vergangene Verhältnisse, nicht den aktuellen Bericht.

Kernpunkte

You could trigger a large avalanche where the wind has formed drifts and stiffened the snow surface. Avalanches may break wider than expected. Expect loose snow avalanches in very steep, rocky terrain receiving direct sun.

Lawinenprobleme

  • Wind Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Likely
    Größe
    1.5–2.5

    Recent storms built slabs in areas exposed to the wind. You could find sensitive slabs at any elevation, but expect them to be thicker and found in more terrain as you climb in elevation. On the northern half of the compass, slabs formed over various persistent weak layers. Triggering an avalanche may be easier on these slopes. You may be able to remotely trigger an avalanche from lower-angle terrain above, below, or to the side of steep slopes.

    Slabs often form near ridgelines, along steep mid-slope gullies, or on aprons below steep cliffs. You can reduce your chances of triggering a wind slab by avoiding slopes with obvious signs of wind-loading, such as new cornice growth and large dunes or pillows of wind-blown snow. Some slabs may not be obvious from a distance as they are masked by soft snow at the surface. A sudden stiffening of the snow you're traveling through or cracks shooting from your skis or sled can indicate an unstable slab.

    (3/18/2025) Very large slab avalanche on Williams Pk, Sawtooth Mountains. Photo: Sawtooth Avalanche Center

  • Loose Wet

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Likely
    Größe
    1–2

    Loose snow avalanches are likely on very steep, rocky slopes receiving direct sun. These slides often initiate near the base of trees and rocks, gathering snow and growing in size as they move downhill. Rollerballs, or pinwheels, signify that the snow is heating up, and wet avalanches may soon follow. 

    While most will start small, they may grow large enough to knock you off your feet or bury you in channeled terrain. Even small slides are consequential above terrain traps such as gullies, creeks, and thick timber. Plan your day to avoid lingering under steep, sunny slopes when the sun is out.

Avalanche Discussion

Yesterday, we observed numerous avalanches that released during our recent storms (photos). These occurred on all aspects as high precipitation intensity caused steep slopes to shed. 

So far, the largest avalanches have been observed in wind-loaded terrain on NW-N-NE-E aspects. These slopes had the weakest snow surfaces before the storm and were loaded heavily by strong SW-W wind. Today, these are the same slopes where you're most likely to get into trouble. Although spring snowpacks often stabilize quickly after storms, observations are limited, and we're exercising extra caution before stepping out into consequential terrain.

Enjoy this beautiful last day of winter, but keep your eyes and ears open for obvious signs of instability. Recent avalanches, muffled collapses, or cracking at the snow surface are your best indications that the slope you're on or connected to may be unstable. When in doubt, dial back your terrain choices; there's plenty of meadow ripping and low-angle powder to be found. 

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