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Kenya is located in the eastern part of Africa. It has an area of about 150,000 square kilometers. It is a very popular tourist destination and also a hotspot for climbing and hiking. In the central highlands a couple of hundred kilometers north of the equator lays Mt.Kenya. It is here, where the Kikuyu god ngai resides. It is the highest mountain in Kenya and the second highest in Africa. It is one of the few places near the equator on Africa with permanent glaciers. The name of the country has been known to have been derived from Mt.Kenya which was formerly known as Mount Kirinyaga.
The mountain is located 180 kilometers north of
Nairobi and it can often be seen from high-rise buildings
in Nairobi and from Thika. It is an extinct volcano, which
formed a couple of million years ago. The mountain is
located in the Mount Kenya National Park, which is a
designated protected area around the mountain above 3200m
altitude. The Kenya Wildlife Service manages the park. The
national park covers an area of 700 square kilometers and
was established in 1949. Kenya enjoys an equatorial climate with average annual temperatures of about 26oC and diurnal temperatures of about 3oC. There are two rainy seasons on the mountain from April-June and October-December. The mountain is an important water catchment area and many rivers such as the Naro Moru emerge from the melting glaciers. The first documented ascent of the mountain was by Halford Mackinders. At the moment the mountain attracts several thousand climbers both local and international annually. It is this popularity, which has contributed to the deterioration of the environment and the litter accumulation. At the base and around this mountain are famous hotels such as the Mount Kenya Safari Club, Outspans, Naro Moru River Lodge, Treetops, Mountain Lodge, Bantu Lodge and several others. Tourists who do not wish to climb often visit the hotels for the view, luxury accommodation, fresh air and the tranquil atmosphere. Compared to Mt.
Kenya Africa’s highest mountain Kilimanjaro is a
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