The Geology Of Kilimanjaro

Kilimanjaro lies on a tectonic line intersection 80km.thousands of years to materialize and may consist of
east of the tectonically active Rift Valley. The activitya number of lava forms including dacite, basalt and
which created this stratovolcano dates back less thanandesite to name but a few.
a million years and the central ash pit on Kibo, theOn the Marangu Route you will more than likely come
highest volcanic centre, may be only several hundredacross a number of small cone shaped hills. These are
years old. Steam and sulphur fumaroles here areknown as 'parasitic cones' and are quite simply
indicative of residual activity. Stratovolcanoes areformations that are the product of offshoots of the
formed when erupted ash and cinders mix with lavamain lava flow. In the event that you elect to do the
flows and cool to produce a steep conical formation.optional Saddle Walk, you will pass a cliff face that
These types of volcanoes usually take tens ofappears to be stained with black and white stripes.