Manda-Inakir
Rekahan erupsi · Ethiopia-Djibouti · 600 m

- Tipe
- Rekahan erupsi
- Negara
- Ethiopia-Djibouti
- Wilayah
- Afrika Timur / Afar Rift Volcanic Province
- Ketinggian
- 600 m
- Koordinat
- 12.380, 42.200
- Letusan terakhir
- 1928
- Kondisi tektonik
- Rift zone / Intermediate crust (15-25 km)
- Bentuk lahan
- Cluster
- Batuan utama
- Basalt / Picro-Basalt
Ringkasan geologi
Manda-Inakir consists of a series of NW-trending fissure vents and pyroclastic cones along the Ethiopia-Djibouti border. The elongated complex represents an uplifted mid-ocean ridge spreading center now exposed above sea level. An elongated dome of basement rocks is cut by two axial rifts, the northern of which was active during historical time. Basaltic cinder cones along the rift's marginal faults have produced lava flows on the flanks of the structural dome, yielding a shield-like morphology. An eruption in 1928 or 1929 at the SE end near the town of Korili (in Djibouti) produced the Kammourta cinder cone and a lava flow.
Riwayat letusan
Ringkasan (VEI dari waktu ke waktu)
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Garis waktu rinci
- 1928VEI 2Teramati1928-12-31 – BerlangsungKammourta
Tautan eksternal
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