Mount Kenya is an extinct volcanic mountain in Africa, formed by the buildup of lava and ash over time. It matters as a significant geographical landmark and natural feature of the African continent.
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Mount Kenya (Meru: Kĩrĩmaara, Kikuyu: Kĩrĩmanyaga, or "Kīrī-nyaga", Kamba: Ki nyaa, Embu: Kĩ nyaga, or "Kirinyaga") is the second highest mountain in Africa. Located about 150 km (90 mi) north-northeast of the capital Nairobi and just 16.5 kilometres (10.3 miles) south of the equator, the mountain's highest peaks are Batian (5,199 m), Nelion (5,188 m), and Point Lenana (4,985 m). Historically situated in the former Eastern and Central provinces, the massif now serves as the intersection of Meru, Embu, Kirinyaga, Nyeri, and Tharaka Nithi counties. The area was officially gazetted as the Mount Kenya National Park in 1949 and was later designated a UNESCO World Heritage Site in 1997 for its outstanding natural beauty and ecological significance. Today, the park and its surrounding forest reserve are managed by the Kenya Wildlife Service and the Kenya Forest Service as a critical sanctuary for endangered species and a primary water tower for the region.
Mount Kenya is a volcano created approximately 3 million years after the opening of the East African Rift. Before glaciation, it was 7,000 m (23,000 ft) high. It was covered by an ice cap for thousands of years. This has resulted in very eroded slopes and numerous valleys radiating from the peak. There are currently 11 small glaciers, which are shrinking rapidly, and may disappear by 2050. The forested slopes are an important source of water for much of Kenya. There are several vegetation bands from the base to the peak. The lower slopes are covered by different types of forest. Many alpine species are endemic to Mount Kenya, such as the giant lobelias and senecios and a local subspecies of rock hyrax. The park receives over 16,000 visitors per year.
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