Makalu

Geography and form

The peak is famous for a sharply pointed, four-sided pyramidal summit with pronounced ridges and steep faces. The Makalu massif includes subsidiary summits such as Kangchungtse (commonly called Makalu II) and feeds glaciers that descend into deep alpine valleys. Much of the surrounding terrain is rugged and remote; its physical form and local setting are often described in studies of Himalayan morphology and alpine glaciation. See notes on its shape and position in Nepal.

Climbing history and routes

Makalu drew international attention during the mid-20th century and was first climbed successfully in 1955 by a French expedition. Compared with some 8,000-metre peaks that offer less technical high-altitude routes, Makalu presents sustained steep rock and ice sections, exposed ridgelines and objective hazards such as seracs and avalanches. Climbers require advanced alpine skills, careful acclimatisation and logistical planning; approaches from the Nepalese and Tibetan sides offer different practical challenges and permit regimes. Access from the Tibetan side and Nepalese approaches are both part of its climbing story.

Ecology, conservation and local context

The mountain’s slopes support high-altitude forests, alpine meadows and a range of Himalayan wildlife. Portions of the area around Makalu are included in conservation initiatives and protected zones that aim to balance biodiversity protection with trekking and mountaineering. Local communities—among them Sherpa and other ethnic groups—have long-standing cultural and economic ties to the valleys and trails that lead toward the massif.

Key facts

• Elevation: 8,485 m (27,838 ft).
• Global rank: 5th highest mountain.
• Distinctive features: four-sided pyramidal summit and subsidiary peak Kangchungtse (Makalu II).