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MOUTAIN CLIMBING
MT KENYA READ MORE
MT KENYA CLIMBING NARO MORU ROUTE
CHOGORIA ROUTE DOWN NARO MORU ROUTE
SIRIMONI ROUTE DOWN CHOGORIA
SIRIMONI, NARO MORU WITH PEAK CIRCUIT ROUTE
 
MT KILIMAJORO READ MORE
MACHAME ROUTE
MARANGU ROUTE
RONGAI ROUTE
SHIRA ROUTE
Mount Kilimanjaro
Mount Kilimanjaro was born of the catastrophic movements in the Earth's crust that created the Great Rift Valley that runs from the Red Sea through Tanzania to Southern Africa. Around 25 million years ago East Africa was a huge flat plain that buckled and ruptured after the African and Eurasian Continental Plates rebounded off each other causing huge rifting and weak spots in the thinning crust that led to the formation of many volcanoes in the region. Where the original valley was deepest, the volcanic activity was greatest eventually forming the huge volcanoes of Ngorongoro Crater on the Rift itself and a string of volcanoes to the East including Meru, Kenya and Kilimanjaro. Ecology Mount Kilimanjaro has five major zones and the activity within each of these is controlled by the five factors of altitude, rainfall, temperature, flora and fauna. Each zone occupies an area approximately 1000m in altitude and is subject to a corresponding decrease in rainfall, temperature and life from the forest upwards
 
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