About Shuswap

This page shows the current backcountry snow report, avalanche forecast, and weather conditions for Shuswap. Check the danger rating, field observations, and Doctor's Orders summary above before heading out.

The Shuswap region spans the highlands between the Thompson River system and the northern Monashee Mountains, covering terrain accessible from Salmon Arm, Chase, and the Shuswap Lake corridor northeast toward the Revelstoke area. This is a broad, largely undeveloped region where the transition between the dry BC Interior and the wetter Columbia Mountain wet belt plays out across a complex series of plateaus, ridgelines, and upper drainage systems. The region lacks the dramatic glaciation of the western Monashees and Selkirks, but offers substantial mid-elevation touring terrain in forested and subalpine environments throughout the winter season. The snow climate of the Shuswap region reflects its intermediate position between the maritime wet belt and the dry Okanagan interior, producing a snowpack that is moderate in depth and character. Snowfall is adequate but not extreme, and the base builds reliably through the winter months at upper elevations. During high-pressure events, Interior cold can push through the Thompson Valley and surrounding drainages, introducing faceting and surface hoar formation that can be buried by subsequent loading events. The region's large elevation range means that snowpack character varies significantly between the lower bench terrain and the higher ridgelines, and stability can differ markedly within the same region on any given day.

Terrain within this zone includes: Salmon Arm, Chase, Adams River, Shuswap Highlands, Sicamous.