Mount Waddington 3D Terrain Map & Relief Model
Interactive digital elevation model (DEM) for Mount Waddington. Tilt, rotate, and inspect high-altitude summit ridges, glacial cirques, and approach routes in high-resolution 3D WebGL cartography.
Expedition base camp on the massive gravel moraines of the Tiedemann Glacier beneath the Bravo Icefall.
Glacial staging camp positioned above the primary lower crevasses and rockfall runout.
High wind-scoured saddle between the main granite tooth of Waddington and the northwest summit.
The sprawling snow dome summit reached by the Mundays in 1934, overlooking the Pacific Coast Range.
Total vertical rise from Tiedemann Glacier Base Camp (1,800m) directly to the summit crest.
DMS: 51Β°22β²25β³ N, 125Β°15β²45β³ W. Verified against alpine geodesy baselines.
The vertical drop to the lowest contour encircling the peak with no higher summit inside it.
Surrounded by lateral moraines, active icefalls, and high glaciated ridges feeding regional river systems.
Topographic Architecture of Mount Waddington
Mount Waddington is the highest peak in the Coast Mountains of British Columbia, rising to 4,019 metres amid the largest temperate icefield system in the world outside polar regions. Celebrated as Mystery Mountain during early exploration, this sheer granite monolith is perpetually guarded by Pacific maritime tempests, immense tidal glaciers, and vertical rock towers.