FlagColombia · Andes5,410 m (17,749 ft)

Ritacuba Blanco 3D Terrain Map & Relief Model

Interactive digital elevation model (DEM) for Ritacuba Blanco. Tilt, rotate, and inspect high-altitude summit ridges, glacial cirques, and approach routes in high-resolution 3D WebGL cartography.

INITIALIZING 3D TERRAIN RELIEF...Loading Copernicus & Mapzen Digital Elevation Model
⛺ High-Altitude Route Staging & Camp Profile:Ascent staging points across documented expedition routes
⛺Cabañas Kanwara4,000 m

Rustic alpine lodge providing comfortable staging and acclimatization at the foot of El Cocuy.

⛺Moraine High Camp4,600 m

Tent camp positioned on level moraine gravel directly beneath the glacier tongue.

⛰️Ritacuba Blanco Summit5,410 m

Airy snow cornice crowning the Cordillera Oriental of Colombia.

🧗 Vertical Relief ClimbTopographic
1,410 m(4,626 ft)

Total vertical rise from Cabañas Kanwara (4,000m) directly to the summit crest.

🧭 WGS84 CoordinatesDatum
6.4967° N, -72.2906° E

DMS: 6°29′48″ N, 72°17′26″ W. Verified against alpine geodesy baselines.

⛰️ Topographic ProminenceKey Col
2,120 m

The vertical drop to the lowest contour encircling the peak with no higher summit inside it.

❄️ Glacial Cirque BasinAlpine Relief
Andes Glacial Field

Surrounded by lateral moraines, active icefalls, and high glaciated ridges feeding regional river systems.

Topographic Architecture of Ritacuba Blanco

Ritacuba Blanco is the 5,410-metre crowning peak of the Cordillera Oriental of Colombia and the Sierra Nevada del Cocuy. Dominated by a massive western ice sheet and sheer eastern rock walls dropping precipitously toward the Amazonian llanos, Ritacuba Blanco is celebrated for its pristine glaciated ramps and high-altitude paramo lakes. The mountain was first climbed on April 3, 1942, by Erwin Kraus, Guido Tamayo, and Heriberto Degen.

Geographical & Glacial Context: Located in the department of Boyacá along the crest of the Eastern Cordillera, Ritacuba Blanco forms the northern terminus of the high Sierra Nevada del Cocuy ice plateau. The peak acts as a critical watershed between the Magdalena River basin and the Orinoco River plains, catching condensation from the eastern savannahs to feed extensive glacial ramps.
First Ascent: 1942-04-03·Expedition Team: Erwin Kraus, Guido Tamayo, and Heriberto Degen