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Elmenteita Badlands

Kerucut piroklastik · Kenya · 2126 m

Prominent dark lava flows (center) erupted from vents in the Elmenteita Badlands, located between Lake Elmenteita (top) and Eburru volcano, the flanks of which appear at the bottom of this Landsat image. Cones and lava flows of varying ages are visible, some of which post-date the 10,000-year-old high-stand of Lake Elmenteita and are of Holocene age.
Prominent dark lava flows (center) erupted from vents in the Elmenteita Badlands, located between Lake Elmenteita (top) and Eburru volcano, the flanks of which appear at the bottom of this Landsat image. Cones and lava flows of varying ages are visible, some of which post-date the 10,000-year-old high-stand of Lake Elmenteita and are of Holocene age. · Foto: NASA Landsat image, 1999 (courtesy of Hawaii Synergy Project, Univ. of Hawaii Institute of Geophysics & Planetology). · Wikimedia Commons
Tipe
Kerucut piroklastik
Negara
Kenya
Wilayah
Eastern Africa Volcanic Regions / Kenyan Rift Volcanic Province
Ketinggian
2126 m
Koordinat
-0.546, 36.249
Letusan terakhir
Tidak diketahui
Kondisi tektonik
Rift zone / Continental crust (> 25 km)
Bentuk lahan
Cluster
Batuan utama
Basalt / Picro-Basalt
Ringkasan geologi

The Elmenteita Badlands, located between Lake Elmenteita (N) and Eburru volcano (S), is an area of pyroclastic cones and lava flows of varying ages. Large basaltic lava flows and ash cones post-date the 10,000-year-old high-stand of Lake Elmenteita (Thomson and Dodson, 1963).

Ringkasan Wikipedia

Ringkasan Inggris

The Elementeita Badlands, also known as the Otutu Forest or Ututu Forest, is a lava flow in Kenya that covers approximately 36 square kilometres. The area was previously covered in thick dryland forest characterized by cedar trees,, and Leleshwa bushes. In addition, Wild Jasmine and Boophone are also found.

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