Kyrgyzstan · Tien Shan7,439 m (24,406 ft)Jengish Chokusu / Peak Pobeda 3D Terrain Map & Relief Model
Interactive digital elevation model (DEM) for Jengish Chokusu / Peak Pobeda. Tilt, rotate, and inspect high-altitude summit ridges, glacial cirques, and approach routes in high-resolution 3D WebGL cartography.
Remote moraine camp situated below the colossal north wall of Pobeda, tributary of South Inylchek.
Snow camp located on the lower slopes beneath the initial avalanche chutes.
Tent platforms dug into hard ice on the steep northern spur.
Essential snow cave shelter carved into the ice of the Western Shoulder to withstand hurricane-force gales.
High-altitude snow cave on the long horizontal ridge leading to the summit bastion.
The elongated, icy summit ridge marking the highest point in the entire Tien Shan and Central Asia.
Total vertical rise from Zvyozdochka Glacier Base Camp (4,050m) directly to the summit crest.
DMS: 42°02′05″ N, 80°07′47″ E. 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 Jengish Chokusu / Peak Pobeda
Jengish Chokusu, historically renowned across the mountaineering world as Peak Pobeda ('Victory Peak'), is the supreme summit of the Tien Shan cordillera at 7,439 metres (24,406 ft) and the northernmost 7,000-metre peak on Earth. Rising along the formidable Kokshaal-Too range on the Kyrgyzstan-China border, Pobeda is notorious for catastrophic Arctic-like blizzards, sub-zero jet-stream gales, and massive hanging seracs that have claimed dozens of lives. The mountain was first conquered on August 30, 1956, by a legendary Soviet expedition led by Vitaly Abalakov via the harrowing North Ridge from the Zvyozdochka Glacier, marking one of the greatest high-altitude triumphs in Russian alpine history.