About North Shore

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

The North Shore region encompasses the rugged mountains rising abruptly from the Pacific Ocean directly above Vancouver and the Burrard Inlet. This area serves as the southernmost tip of the Coast Mountains' glaciated belt, though its current landscape is defined more by its steep-sided, heavily forested drainages and rounded granitic summits than by active ice. The terrain transitions quickly from sea level to over 1700 meters, featuring the prominent twin peaks of The Lions, along with accessible sub-alpine hubs like Hollyburn, Mount Seymour, and Mount Strachan. While much of the region is centered around local ski area infrastructure, the surrounding backcountry offers a maze of technical gullies, open ridges, and steep glades that provide a wild, wilderness character despite their proximity to the urban center. The snow climate is purely maritime and is characterized by its direct exposure to moisture-laden storms sweeping off the Pacific. Because these mountains are the first major barrier for incoming weather, they receive prolific amounts of precipitation, often resulting in high-volume, dense snowfall that settles rapidly into a deep and exceptionally well-consolidated pack. However, the proximity to the ocean and lower average elevations make the region highly sensitive to the freezing level, leading to frequent rain-on-snow events and a snowpack that can transition quickly from deep powder to a firm, resilient crust. Snow behavior is defined by this rapid cycling, which builds a massive base capable of masking the rugged understory of the coastal forest, providing a reliable surface for touring and steep-slope skiing throughout the mid-winter and spring months.

Terrain within this zone includes: Hollyburn, Pump Peak, Seymour, Cypress, Strachan.