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Korath

Korath Range

Cono di tufo · 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
Tipo
Cono di tufo
Paese
Ethiopia
Regione
Eastern Africa Volcanic Regions / Kenyan Rift Volcanic Province
Altitudine
912 m
Coordinate
5.117, 35.892
Ultima eruzione
Sconosciuto
Contesto tettonico
Rift zone / Intermediate crust (15-25 km)
Forma vulcanica
Cluster
Roccia principale
Trachybasalt / Tephrite Basanite
Sintesi geologica

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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⚠ Solo a scopo informativo. Non adatto a situazioni di emergenza.