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Manda Gargori

Frattura eruttiva · Ethiopia · 700 m

Scoria cones and lava flows of the Manda Gargori rift are seen across this December 2019 Planet Labs satellite image monthly mosaic (N is at the top; this image is approximately 9.5 km across).The rift is one of the younger segments in the Red Sea area and NW-SE trending faults are visible through the image. Ridges of older lava flows are visible between the lighter-colored sediment. A tuff ring is visible south of the younger lavas.
Scoria cones and lava flows of the Manda Gargori rift are seen across this December 2019 Planet Labs satellite image monthly mosaic (N is at the top; this image is approximately 9.5 km across).The rift is one of the younger segments in the Red Sea area and NW-SE trending faults are visible through the image. Ridges of older lava flows are visible between the lighter-colored sediment. A tuff ring is visible south of the younger lavas. · Foto: Satellite image courtesy of Planet Labs Inc., 2019 (https://www.planet.com/).
Tipo
Frattura eruttiva
Paese
Ethiopia
Regione
Eastern Africa Volcanic Regions / Afar Rift Volcanic Province
Altitudine
700 m
Coordinate
11.750, 41.480
Ultima eruzione
Sconosciuto
Contesto tettonico
Rift zone / Intermediate crust (15-25 km)
Forma vulcanica
Cluster
Roccia principale
Basalt / Picro-Basalt
Sintesi geologica

The Manda Gargori rift, located north of the town of Aisa Aita NE of Borawli volcano and SE of Kurub volcano, is the youngest rift segment in the Afar depression and is only one third the width of the adjacent Manda Hararo-Goba'ad rift system to the west. Two older lava flows from the Manda Gargori rift have Pleistocene potassium-argon dates. Youthful-looking lava flows, some of which may have been subaqueous, have been emitted from NNW-trending fissures. A hyaloclastite tuff ring is also present, and a rhyolitic lava dome surrounded by two basaltic lava flows is located north of Uddummi lake. No historical activity has been reported at the dominantly basaltic Manda Gargori rift, but human footprints have been observed in a fresh ashfall deposit, and the eruptive activity is considered to be of historical age.

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