Mt. Kenya is a huge pixie symmetrical volcanic cone. Its measurement at the base midpoints 120 km. It was shaped somewhere in the range of 2.6 and 3.1 million years prior by ejections of progressive layers of magma and agglomerates from a focal vent in the world's surface. The magmas were shaped by the generally brisk surge of fluid shake; Agglomerates are made out of a blend of coarse and fine particles that start from a savagely hazardous ejection in which broke pieces of shake are tossed from a focal vent and fall on the inclines of the cone, in the end experiencing combination into shake.

The lower slants of the mountain have never been glaciated. They are currently for the most part developed and forested. They are recognized by soak sided V-molded valleys with numerous tributaries. Higher up the mountain, in the region that is presently moorland, the valleys progress toward becoming U-molded and shallower with compliment bottoms. These were made by glaciation.

The name of the mountain itself got from either an error of the first Kikuyu name, Kere-Nyaga (mountain of whiteness), or from the locals' epithet for it, Kiinyaa, after a black and white male ostrich.

It is said that the first man to achieve that summit was the primary head of the Kikuyu clan. He was as far as anyone knows lifted to the top by the god Mogai, the master of nature, and appeared at begin his clan. For quite a long time a short time later, different locals wanted to go to the best. They were unnerved by the far off thundering of torrential slides and the enchanted white sheathing that they speculated may be flour. The mountain was enchantment. Evidence of this came when the primary doormen to go with white men to the best came back with accounts of water swinging to stone medium-term. The Mwimbi clan from the mountain's eastern slants trusted it to be possessed by underhandedness spirits that entered men's bodies and made them epileptics. In 1899 an Englishman named Halford J. Mackinder and his two elevated aides were the principal white men to overcome the fundamental pinnacle. He named it Batian after a Masai drug man who had forecasted that creatures with white skin would one day attack their territory.

Lying on the equator Mount Kenya is influenced by the entry of the Intertropical Convergence Zone, which carries with it the principle stormy periods. The most noteworthy precipitation happens between late March and the center of May, and marginally less between late October and mid-December. Greatest precipitation happens in the woodland belt and on the south-east side of the mountain where it achieves 2500mm. every year at 3000m.

Precipitation diminishes with elevation and is about 700mm. every year at 4500m. Rain and, higher up, snow can anyway be experienced whenever of year - even in the driest periods (January and February). Regularly the drier seasons are related with clear, dry climate which can keep going for a long time on end. The best climate is for the most part in the mornings, and convectional precipitation, assuming any, will in general come in the mid-evening.

Temperatures differ impressively with tallness and with time of day. On the fields encompassing Mount Kenya the normal day temperature is about 25°C. At 3000m, ices can be experienced around evening time while day temperatures extend from 5 to 15°C. Evening time temperatures on the summit are well beneath solidifying. The south-bound side of Mount Kenya gets more daylight in the December to March period. Amid this time shake climbs are "in-condition" and snow and ice climbs step by step break down. In the June to October period the north-bound shake ascensions and south-bound ice climbs are ideal.

Mount Kenya is the second most astounding mountain after Mount Kilimanjaro. The odds of one getting to the most noteworthy pinnacle, Batian, 5,199m, without creating height infection are high. The equator goes through Mount Kenya National Park and most trekking route cross it!

We at Popote Africa firmly believe that Mt Kenya hiking is a great adventure by itself because of these reasons:/p>