Mallahle
Stratovolkan · Ethiopia-Eritrea · 1875 m

- Tipe
- Stratovolkan
- Negara
- Ethiopia-Eritrea
- Wilayah
- Eastern Africa Volcanic Regions / Afar Rift Volcanic Province
- Ketinggian
- 1875 m
- Koordinat
- 13.270, 41.650
- Letusan terakhir
- Tidak diketahui
- Kondisi tektonik
- Rift zone / Intermediate crust (15-25 km)
- Bentuk lahan
- Composite
- Batuan utama
- Trachyte / Trachydacite
Ringkasan geologi
Mallahle is the central of three NE-SW-trending stratovolcanoes (along with Asavyo and Nabro) in the Danakil horst SW of Dubbi volcano. These volcanoes, plus Sork'Ale, form the Bidu Volcanic Complex. The volcano is truncated by a steep-walled 6-km-wide caldera, and is formed of rhyolitic lava flows and pyroclastics. Basaltic lava flows cover the slopes. Recent obsidian flows are found on the NW flank, and older obsidian flows were erupted on the northern caldera floor. Flank spatter and scoria cones are most numerous on the western side of the volcano. Extensive ignimbrite deposits associated with the collapse of Mallahle and Nabro volcanoes cover the countryside.
Ringkasan Wikipedia
Ringkasan InggrisMallahle is a stratovolcano on the border of Ethiopia and Eritrea, with a 6 km wide caldera.
Wikipedia · CC BY-SA · Baca artikel lengkap →
Riwayat letusan
Garis waktu rinci
Tidak ada catatan letusan.
Tautan eksternal
⚠ Untuk referensi saja. Bukan untuk tanggap darurat.