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Korath

Korath Range

Kerucut tufa · Ethiopia · 912 m

The fissure-controlled Korath Range is an isolated group of tuff cones and lava flows in southern Ethiopia that were erupted along the Turkana Rift. The lava flows traveled up to about 5 km with visible lobate margins, most prominently on the W flanks.
The fissure-controlled Korath Range is an isolated group of tuff cones and lava flows in southern Ethiopia that were erupted along the Turkana Rift. The lava flows traveled up to about 5 km with visible lobate margins, most prominently on the W flanks. · Foto: NASA Landsat 7 image (worldwind.arc.nasa.gov) · Wikimedia Commons
Tipe
Kerucut tufa
Negara
Ethiopia
Wilayah
Eastern Africa Volcanic Regions / Kenyan Rift Volcanic Province
Ketinggian
912 m
Koordinat
5.117, 35.892
Letusan terakhir
Tidak diketahui
Kondisi tektonik
Rift zone / Intermediate crust (15-25 km)
Bentuk lahan
Cluster
Batuan utama
Trachybasalt / Tephrite Basanite
Ringkasan geologi

The Korath Range is an isolated group of about 20 tuff cones and lava flows in southern Ethiopia that were erupted along the Turkana Rift, which extends north from Kenya. Many of the cones issued lava flows from their flanks that traveled up to about 5 km. The apparent youngest flow issued from the central crater and flowed through a breach in its rim. The absolute age of the dominantly basanitic-tephritic lava flows is unknown, but a shell adhering to the youngest flow was radiocarbon dated at 7,900 years before present (BP) (Brown et al., 1969). Davidson (1983) indicated an age between 30,000 and 7,900-9,500 BP.

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⚠ Untuk referensi saja. Bukan untuk tanggap darurat.