Ol Doinyo Lengai
Encyclopedia : O : OL : OLD : Ol Doinyo Lengai
| Ol Doinyo Lengai | |
|---|---|
![]() Image of 1966 eruption | |
| Elevation: | 2,960 m (9,711 ft) |
| Coordinates: | |
| Location: | Tanzania |
| Range: | |
| Type: | Stratovolcano |
| Last eruption: | 2006 (continuing) |
Whereas most lavas are rich in silicate minerals, the lava of Ol Doinya Lengai is rich in the rare sodium and potassium carbonates, nyerereite and gregoryite. Due to this unusual composition, the lava is erupted at relatively low temperatures (approximately 500-600 degrees Celsius). This temperature is so low that the molten lava appears black in sunlight, rather than having the red glow common to most lavas. It is also much more fluid than silicate lavas. The sodium and potassium carbonate minerals of the lavas formed by Ol Doinyo Lengai are unstable at the Earth's surface and susceptible to rapid weathering, quickly turning from black to grey in color. The resulting volcanic landscape is different from any other in the world. The chemical makeup of the lava has been compared to dish soap.
"Ol Doinyo Lengai" means "Mountain of God" in the language of the native Masai people.
The most recent eruption took place on the 27th of March 2006.
External links
- [Ol Doinyo Lengai at nationalgeographic.com]
- [Global Volcanism Program]
- [Ol Doinyo Lengai at Stromboli Online]
- [Ol Doinyo Lengai at Volcano World]
- [Middle Tennessee State Univ. Mountain of God]
- [Earlham College Ol Doinyo Lengai]
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