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The Global Volcanism Program has no activity reports for Mallahle.
The Global Volcanism Program has no Weekly Reports available for Mallahle.
The Global Volcanism Program has no Bulletin Reports available for Mallahle.
Mallahle is the central of three NE-SW-trending stratovolcanoes in the Danakil horst SW of Dubbi volcano, and lies SSW of Nabro volcano. These two volcanoes, along with Bara Ale and Sork'Ale, form the Bidu volcanic complex. The complex Mallahle stratovolcano is truncated by a steep-walled 6-km-wide caldera. Mallahle is formed of rhyolitic lava flows and pyroclastics. Basaltic lava flows blanket the slopes of the volcano. Recent obsidian flows are found on the NW flank of Mallahle 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 blanket the countryside.
The Global Volcanism Program is not aware of any Holocene eruptions from Mallahle. If this volcano has had large eruptions (VEI >= 4) prior to 10,000 years ago, information might be found on the Mallahle page in the LaMEVE (Large Magnitude Explosive Volcanic Eruptions) database, a part of the Volcano Global Risk Identification and Analysis Project (VOGRIPA).
This compilation of synonyms and subsidiary features may not be comprehensive. Features are organized into four major categories: Cones, Craters, Domes, and Thermal Features. Synonyms of features appear indented below the primary name. In some cases additional feature type, elevation, or location details are provided.
|Sorc-ali | Mallali | Sorc-alli|
|The smaller (left-hand) of the two large calderas at the bottom center of this NASA Space Shuttle image is Mallahle. The steep-walled 8-km-wide caldera truncates a stratovolcano formed of rhyolitic lava flows and pyroclastics. Basaltic lava flows blanket the slopes of the volcano, and flank vents are most numerous on its western side. Mallahle lies SW of the larger Nabro caldera (right-center) and is the central of three NE-SW-trending stratovolcanoes in the Danakil horst SW of Dubbi volcano.
NASA Space Shuttle image S-61A-36, 1985.
The following references have all been used during the compilation of data for this volcano, it is not a comprehensive bibliography. Discussion of another volcano or eruption (sometimes far from the one that is the subject of the manuscript) may produce a citation that is not at all apparent from the title.
CNR-CNRS, 1975. Geological Maps of Afar: 1, Northern Afar (1971); 2, Central and Southern Afar (1975). La Celle St Cloud, France: Geotechnip.
CNR-CNRS Afar Team, 1973. Geology of northern Afar (Ethiopia). Rev Geog Phys Geol Dynam, 15: 443-490.
IAVCEI, 1973-80. Post-Miocene Volcanoes of the World. IAVCEI Data Sheets, Rome: Internatl Assoc Volc Chemistry Earth's Interior..
Katsui Y (ed), 1971. List of the World Active Volcanoes. Volc Soc Japan draft ms, (limited circulation), 160 p.
Wiart P, Oppenheimer C, 2005. Large magnitude silicic volcanism in north Afar: the Nabro volcanic range and Ma'alalta volcano. Bull Volc, 67: 99-115.
Wood C A, 1980. . (pers. comm.).