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Kilimanjaro Research Paper

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Kilimanjaro with its three volcanic cones, Kibo, Mawenzi, and Shira, is an inactive stratovolcano in north-eastern Tanzania rising 4,600 m (15,100 ft) from its base (and approximately 5,100 m (16,700 ft) from the plains near Moshi), and is additionally the highest peak in Africa at 5,891.8 metres (19,330 ft), providing a dramatic view of the surrounding plains. Mount Kilimanjaro is one of the largest stratovolcanoes in the world. Otherwise known as a composite volcano, it comprises numerous layers of lava, tephra and volcanic ash. Tephra is rhyolitic (an igneous, extrusive rock) in composition, and is formed by air-fall material of an eruption, which suggests the composite volcano was once active. However, at the moment it is dormant. According to experts there have been no eruptions in living memory. Recent studies suggest the last eruptions on the mountain were between 150,000 and 200,000 years ago. …show more content…
Mount Kilimanjaro is made up of tephra, i.e. it has a cinder cone. They are made up of blobs of congealed lava and particles. When the mountain erupted millions of years ago, the gas-charged lava would be blown violently into the air, then breaking into smaller fragments which would solidify and fall as cinders. This left Mount Kilimanjaro with a bowl-shaped crater. It is not be uncommon for a stratovolcano such as Mount Kilimanjaro to have experienced explosive eruptions. The lava from the mountain is viscous so it cools down before it spreads very far. The lava's viscosity also helps explain why Mount Kilimanjaro has relatively small crater formations. The rock on the mountain is felsic and thus has high levels of silica, especially tephratic silicate. This silica is also in alternating sectors, with lava flows and ejecta in different

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