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Manda Gargori

Fisura volcánica · 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
Fisura volcánica
País
Ethiopia
Región
Eastern Africa Volcanic Regions / Afar Rift Volcanic Province
Altitud
700 m
Coordenadas
11.750, 41.480
Última erupción
Desconocido
Contexto tectónico
Rift zone / Intermediate crust (15-25 km)
Forma volcánica
Cluster
Roca principal
Basalt / Picro-Basalt
Resumen geológico

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.

Historial de erupciones

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Enlaces externos

⚠ Solo como referencia. No apto para respuesta ante emergencias.