Lava Plateaus

Fissure eruptions at Mt Nyiragongo. Image credit Imgsoup.

Fissure eruptions at Mt Nyiragongo. Image credit Imgsoup.

ZIMSEC O Level Geography Notes: Lava Plateaus

  • Lava eruptions through narrow cracks (fissures) tends to be very quiet and subdued.
  • The lava spreads out over the surrounding countryside.
  • Successive lava outpourings causes successive layers of lava to build up.
  • This may completely cover up the features of the surrounding region.
  • Sometimes these layers of lava may be hundreds of meters thick
  • The lava layers may accumulate in the depressions within the vicinity of the eruptions and rise to be high enough to bury the preexisting terrain.
  • Resulting in high and fairly level features often that are referred to as lava plateaus.
  • Some lava plateaus are very extensive in size and can cover thousands of kilometers for example the Haruj al Aswad (sometimes anglicized as Charudsch al-Aswad)   Plateau in Libya.
  • Part of the Drankesberg Mountains in South Africa may be remnants of a lava plateau.
  • At times due to subsequent erosion by rivers the original surfaces may be exposed on the floor of very deep valleys.
  • Rivers crossing these plateaus often carve out deep gorges.
  • These plateaus sometimes provide fertile soils.

To access more topics go to the Geography Notes page.

By |2017-01-17T11:22:18+00:00June 8th, 2015|Landform Studies, Notes, O Level Geography, Ordinary Level Notes|Comments Off on Lava Plateaus

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He holds an Honours in Accountancy degree from the University of Zimbabwe. He is passionate about technology and its practical application in today's world.
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