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User:Mehmet Karatay/Geology of Mount Kenya

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The geology of the Mount Kenya area was first considered by Joseph Thomson in 1883. He saw the mountain from the nearby Laikipia Plateau and wrote that it was an extinct volcano with the plug exposed.[1] However, as he had only seen the mountain from a distance his description was not widely believed, particularly after 1887 when Teleki and von Höhnel ascended the mountain and described what they considered to be the crater.[2] In 1893 Gregory's expedition reached the Lewis Glacier at 5,000 m (16,000 ft). He confirmed that the volcano was extinct and that there were glaciers present.[2][3] The first thorough survey was not undertaken until 1966.[4]

Mount Kenya is a stratovolcano that was active in the Plio-Pleistocene. The original crater was probably over 6,000 m (20,000 ft) high; higher than Kilimanjaro. Since it became extinct there have been two major periods of glaciation, which are shown by two main rings of moraines below the glaciers. The lowest moraine is found at around 3,300 m (10,700 ft).[4] Today the glaciers reach no lower than 4,650 m (12,250 ft).[5] After studying the moraines, Gregory put forward the theory that at one time the whole summit of the mountain was covered with an ice cap, and it was this that eroded the peaks to how they are today.[6]

Mount Kenya was a stratovolcano and probably looked similar to this before the glaciations. The lower slopes are still this shape, which is how the previous height is estimated.

The lower slopes of the mountain have never been glaciated. They are now mainly cultivated and forested. They are distinguished by steep-sided V-shaped valleys with many tributaries. Higher up the mountain, in the area that is now moorland, the valleys become U-shaped and shallower with flatter bottoms. These were created by glaciation.[4]

When Mt Kenya was active there was some satellite activity. The north-eastern side of the mountain has many old volcanic plugs and craters. The largest of these, Ithanguni, even had its own ice cap when the main peaks were covered in ice. This can be seen by the smoothed summit of the peak. Circular hills with steep sides are also frequent in this area, which are probably the remains of small plugged vents. However, as the remaining mountain is roughly symmetrical, most of the activity must have occurred at the central plug.[4]

The rocks that form Mt Kenya are mainly basalts, rhomb porphyrites, phonolites, kenytes and trachytes.[4] Kenyte was first reported by Gregory in 1900 following his study of the geology of Mount Kenya.[3]


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Items to later include in this article

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Volcanic plug, Stratovolcano, basalt, viscosity, lava, erosion, vent, glaciation, Ice age, ice cap

Images

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Glowing ʻaʻā flow front advancing over pāhoehoe on the coastal plain of Kīlauea in Hawaiʻi, United States. These cause clinkers that shipton (?) writes about on Batian.
These were likly the type of eruptions that occured on Mt Kenya as they are the same type of volcano. The low viscosity of this type of lava gives shield volcanos their broad shape.


References

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  1. ^ Cite error: The named reference thomson was invoked but never defined (see the help page).
  2. ^ a b Cite error: The named reference gregory was invoked but never defined (see the help page).
  3. ^ a b Cite error: The named reference gregory1900 was invoked but never defined (see the help page).
  4. ^ a b c d e Baker, B. H. (1967). Geology of the Mount Kenya Area. Geological Survey of Kenya. Ministry of Natural Resources.
  5. ^ Cite error: The named reference map was invoked but never defined (see the help page).
  6. ^ Cite error: The named reference glacialgeology was invoked but never defined (see the help page).
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