Kilimanjaro is a Maasai word meaning Large Rock. Kilimanjaro is 340 km south of the Equator, 280 km from the Indian Ocean and just over 400 km from Lake Victoria. It is about one hour’s drive from Kilimanjaro airport. It lies on the eastern side of the eastern branch of the Great Rift Valley, and north-north east of the Maasai steppe, the great plain of north-eastern Tanzania renowned as the homeland of the nomadic Maasai cattle-herders. Kilimanjaro has three volcanic cones, Kibo, Mawensi, and Shira, and is an inactive stratovolcano in north-eastern Tanzania. Although it does not have the highest elevation, Kilimanjaro is the tallest free-standing mountain rise in the world, rising 4,600 m (15,100 ft) from its base, and includes the highest peak in Africa at 5,895 meters (19,340 ft), providing a dramatic view from the surrounding plains.

Kilimanjaro, by any name, is a metaphor for the compelling beauty of East Africa. When you see it, you understand why. Not only is this the highest peak on the African continent; it is also the tallest free-standing mountain in the world, rising in breathtaking isolation from the surrounding coastal scrubland – elevation around 900 metres – to an imperious 5,895 metres (19,336 feet).

Tantalising glimpses of the magnificent snow-capped summit from the plains below belie the unique combination of eco-climatic zones which hikers will experience; rainforest, montane forest, heath and moorland, alpine desert and then, finally, snow and ice.

Second Stage: Open Moorland
From around 3,200m a wide expanse of moorland extends beyond the heath and the cloud line, so that here the skies are generally clear, making the sunshine intense during the days and the nights cool and clear. The climbing incline remains gentle, but thinning oxygen provides less fuel to energise the muscles and can dramatically slow the pace of walking. Hardy endemic species of Giant Groundsels (Senecio) and Lobelia (Deckenii) towering up to 4m high thrive in this moorland zone and give the landscape a strangely primeval atmosphere.

Third Stage: Alpine Desert, Sparse Vegetation
Even higher, beyond 4,000m, this sensation intensifies as the landscape develops into a more bizarre alpine desert, with sandy loose earth and intense weather conditions and temperature fluctuations so dramatic that barely any plant species survive other than everlasting flowers, mosses and lichens. Only the odd lichen survives beyond 5000m, after Kibo Huts and beyond the Saddle, where the landscape is predominantly rock and ice fields. Here, climbers experience the final steep push to the summit.

Final Stage: Saddle to Summit
The easterly routes, Marangu, Mweka, Loitokitok and Rongai all converge west of the saddle near Gillmans Point, between the peaks of Mawenzi and Kibo. Kibos crater is roughly circular with an inner cone extending to 5,800m, (100m lower than the summit at Uhuru Peak). At the centre an inner crater with walls between 12 and 20 m high contains another concentric minor cone, the centre of which falls away into the 360m span of the ash pit. This is the 120 metre deep central core of the volcano, and casts sulphurous boiling smoke from its depths despite the frozen, snowy outskirts.