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Get the Himo, Kilimanjaro local weather forecast by the hour and the next 10 days.
Mount Kilimanjaro (/ ˌ k ɪ l ɪ m ə n ˈ dʒ ɑː r oʊ /) [3] is a dormant volcano in Tanzania.It is the highest mountain in Africa and one of the highest free ...
The climate of Mount Kenya has played a critical role in the development of the mountain, influencing the topography and ecology amongst other factors. The area around Mount Kenya is covered by a comparably large number of weather station data with long measurements series and thus the climate is well recorded. [1]
Kilimanjaro National Park is a Tanzanian national park located 300 kilometres (190 mi) south of the equator [1] in the Kilimanjaro Region, Tanzania. The park is located near the region of Moshi. [3] The park includes the whole of Mount Kilimanjaro above the tree line and the surrounding montane forest belt above 1,820 metres (5,970 ft).
Northeast Tanzania exhibits a mountainous terrain and includes Mount Meru, an active volcano, Mount Kilimanjaro, a dormant volcano, and the Usambara and Pare mountain ranges. Kilimanjaro attracts thousands of tourists each year. West of those mountains is the Gregory Rift, which is the eastern arm of the Great Rift Valley.
The lowest altitude of alpine climate varies dramatically by latitude. If alpine climate is defined by the tree line, then it occurs as low as 650 metres (2,130 ft) at 68°N in Sweden, [14] while on Mount Kilimanjaro in Tanzania, the tree line is at 3,950 metres (12,960 ft). [14]
Credner Glacier is on Mount Kilimanjaro in Tanzania, on the northwest slope of the peak and is a remnant of an icecap which once crowned the top of Mount Kilimanjaro. [1] The glacier is situated at an elevation of between 5,800 and 5,500 metres (19,000 and 18,000 ft). [2]
The modern, arid Sahara. The Sahara was not a desert during the African humid period. Instead, most of northern Africa was covered by grass, trees, and lakes. The African humid period (AHP; also known by other names) was a climate period in Africa during the late Pleistocene and Holocene geologic epochs, when northern Africa was wetter than today.