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Etiopia · Rekahan erupsi

Manda Gargori

Tipe
Rekahan erupsi
Ketinggian
700 m
Letusan terakhir
Tidak diketahui
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/).
Tipe
Rekahan erupsi
Negara
Etiopia
Wilayah
Afrika Timur / Afar Rift Volcanic Province
Ketinggian
700 m
Koordinat
11.750, 41.480
Letusan terakhir
Tidak diketahui
Kondisi tektonik
Zona rift / Kerak menengah (15-25 km)
Bentuk lahan
Gugusan gunung api
Batuan utama
Basal / Pikrobasal
Ringkasan geologi

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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