Cornice Mountain (Cambria Icefield)

Cornice Mountain is a peak located within the Cambria Icefield in British Columbia, Canada. The mountain is named for its prominent snow cornice formations, a characteristic feature resulting from prevailing winds depositing snow onto the leeward side of the summit and ridges.

The Cambria Icefield, a large icefield spanning a significant area of northwestern British Columbia, influences the climate and geography surrounding Cornice Mountain. The mountain's specific elevation and coordinates can be obtained from geographical databases and topographical maps.

Cornice Mountain is generally accessed by experienced mountaineers and skiers. Access typically requires traversing the Cambria Icefield, which poses challenges due to crevasses, unpredictable weather, and the remote location.

The geological composition of Cornice Mountain is characteristic of the Coast Mountains, which are composed primarily of granitic and metamorphic rocks.

The alpine environment surrounding Cornice Mountain supports a limited range of plant and animal life adapted to cold temperatures and high altitudes. The region falls within a zone exhibiting typical glacial and alpine ecosystems.