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Mount Kilimanjaro

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Mount Kilimanjaro
NameMount Kilimanjaro
Photo captionThe summit of Kibo featuring the Rebmann Glacier and Furtwängler Glacier.
Elevation m5895
Prominence m5885
ListingSeven Summits, Volcanic Seven Summits, Highest mountain peaks of Africa, Ultra-prominent peak, Country high point
LocationKilimanjaro Region, Tanzania
Coordinates3, 4, 33, S...
TypeStratovolcano
Last eruptionBetween 150,000 and 200,000 years ago
First ascent6 October 1889 by Hans Meyer and Ludwig Purtscheller
Easiest routeHike

Mount Kilimanjaro. It is a dormant stratovolcano in Tanzania and the highest mountain in Africa, rising approximately 4,900 metres from its base to 5,895 metres above sea level. The mountain is composed of three distinct volcanic cones: Kibo, the highest and central summit; Mawenzi; and the extinct Shira. Its iconic, snow-capped peak, isolated on the East African plains, has made it a subject of global fascination, scientific study, and a premier destination for high-altitude climbing.

Geography and geology

The mountain is located in northeastern Tanzania near the border with Kenya, within Kilimanjaro National Park. It is a massive stratovolcano formed by the eruption of magma from the East African Rift system. The three cones were formed during different volcanic periods, with Kibo being the youngest and only cone retaining a volcanic crater named the Kibo Caldera. Geological studies indicate its last significant activity occurred in the Pleistocene, with fumarole activity recorded in the 19th century within the crater. The formation's immense size dominates the local topography and influences regional weather patterns.

Climate and ecosystems

The climate ranges from tropical at the base to arctic at the summit, creating a series of distinct ecological zones. The lower slopes are characterized by cultivated farmland and montane forest, which give way to heath and moorland zones featuring unique flora like giant groundsels and giant lobelias. Higher up, the alpine desert zone transitions into the summit's ice cap, which consists of remaining glaciers such as the Furtwängler Glacier. These glaciers have undergone dramatic retreat since the late 19th century, a process extensively documented since the expedition of Hans Meyer.

History and exploration

The mountain has been known to local peoples, including the Chagga people, for centuries. It appeared on Ptolemy's maps but was dismissed by European geographers until its confirmation by Johannes Rebmann of the Church Missionary Society in 1848. Reports of snow near the equator were met with skepticism by the Royal Geographical Society. The first recorded ascent to the highest point, Uhuru Peak, was achieved on 6 October 1889 by German geologist Hans Meyer and Austrian mountaineer Ludwig Purtscheller, aided by their Chagga guide Yohanas Kinyala Lauwo. The mountain later became part of German East Africa before coming under British administration as a League of Nations mandate.

Climbing routes and tourism

It is one of the world's most accessible high peaks, requiring no technical mountaineering skill, which attracts tens of thousands of trekkers annually. There are several established routes, including the popular Marangu Route, the scenic Lemosho Route, and the challenging Machame Route. All climbs are regulated and require the accompaniment of licensed guides from operators registered with the Tanzania National Parks Authority. The ascent presents significant risks, primarily from altitude sickness, and success rates vary considerably by route and duration. The economic impact of this tourism is substantial for the Kilimanjaro Region and the nation.

Conservation and threats

The mountain and its surrounding forests are protected within Kilimanjaro National Park, a UNESCO World Heritage Site since 1987. Major conservation threats include the rapid recession of its glaciers, attributed to climate change, and deforestation on the lower slopes from agricultural expansion and fuelwood harvesting. Other concerns involve the impact of high visitor numbers, waste management, and water resource stress for local communities. Conservation efforts are coordinated by the Tanzania National Parks Authority in collaboration with international bodies and research institutions like the NASA Earth Observing System, which monitors glacial loss.

Category:Mountains of Tanzania Category:Stratovolcanoes of Africa Category:Volcanoes of the Great Rift Valley Category:World Heritage Sites in Tanzania