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Yangudi

Gunung api kompleks · Ethiopia · 1383 m

Yangudi volcano contains an elliptical summit caldera that lies near the center of this NASA Landsat image (with north to the top). Very recent scoria cones and lava flows form the dark-colored areas south and north of Yangudi along graben faults. Numerous NNE-SSW-trending faults parallel the Ethiopian Rift.
Yangudi volcano contains an elliptical summit caldera that lies near the center of this NASA Landsat image (with north to the top). Very recent scoria cones and lava flows form the dark-colored areas south and north of Yangudi along graben faults. Numerous NNE-SSW-trending faults parallel the Ethiopian Rift. · Foto: NASA Landsat 7 image (worldwind.arc.nasa.gov) · Wikimedia Commons
Tipe
Gunung api kompleks
Negara
Ethiopia
Wilayah
Eastern Africa Volcanic Regions / Main Ethiopian Rift Volcanic Province
Ketinggian
1383 m
Koordinat
10.580, 41.042
Letusan terakhir
Tidak diketahui
Kondisi tektonik
Rift zone / Intermediate crust (15-25 km)
Bentuk lahan
Composite
Batuan utama
Rhyolite
Ringkasan geologi

Yangudi volcano, lying in the Addado graben of the northern Main Ethiopian Rift, is a complex rhyolitic stratovolcano with an elliptical summit caldera. A trachytic lava flow originating in the caldera covers part of the southern flank of Yangudi, also known as Angudi, Jangudi, or Langudi. Rhyolitic obsidian domes on the NW flank are surrounded by younger basaltic lava flows. Very recent scoria cones and lava flows are located south of Yangudi along the eastern graben faults.

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⚠ Untuk referensi saja. Bukan untuk tanggap darurat.