— — ice on the line of the sun.
“A stratovolcano on the equator, second highest in Africa after Kilimanjaro. Batian at 5,199 metres carries the last of the mountain's glaciers, melting back faster each decade. The Kikuyu call it Kirinyaga, the place of brightness, and for centuries faced their houses toward its summit. Clouds usually close by mid-morning. Climbing season runs January to February and August to September.
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Mount Kenya is a stratovolcano in central Kenya, about 200 km north of Nairobi, straddling the equator. Its highest peak, Batian, rises 5,199 metres (17,057 ft); Nelion follows at 5,188 m; the trekking summit Lenana reaches 4,985 m. The mountain anchors Mount Kenya National Park and a UNESCO World Heritage site declared in 1997. Erosion has carved the original cone into a ring of jagged peaks; the last eruption was roughly 2.6 million years ago, leaving the present skyline.
The mountain holds four climatic zones inside its vertical band: forest, bamboo, moorland, and the high alpine desert above 4,000 metres. Above the moorland the air thins fast; trekkers heading for Point Lenana are warned about altitude sickness from 4,200 m onward. Vegetation drops away to giant lobelias and senecios found nowhere else on Earth. Equatorial sun by day, sub-freezing nights, sometimes both in the same hour. The summit glaciers, eleven of them in 1900, are now down to a handful.
The mountain has two dry windows that match the climbing season: January to early March, and June to October. Both are framed by long rains in April and May and short rains in November. Within the dry windows mornings are clear; clouds normally close the summit by ten or eleven. The forest belt holds elephant, buffalo, and bushbuck; the moorland holds rock hyrax and the occasional leopard. The Kikuyu, Embu, and Meru still hold the mountain as sacred ground.