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The Global Volcanism Program has no activity reports for Gada Ale.
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Gada Ale, also known as Kebrit Ale, is the most prominent volcano at the northern end of the Erta Ale Range. It is formed of interstratified lava flows and hyaloclastites. Fumarolic activity is continuing, and a small lake filled by boiling mud occupies the crater. Like other Erta Ale Range volcanoes, Gada Ale is considered to be of Holocene age (Barberi and Varet, 1970). A fissure on the SE flank has produced spatter cones and a cinder cone; the latter fed lava flows that reach to Lake Bakili. The symmetrical Catherine tuff ring is located along this same SE trend west of Lake Bakili, and other tuff rings occur on the east side of the lake. A 2-km-wide salt dome west of Gada Ale has uplifted lava flows as much as 100 m, and the structure of Gada Ale itself also appears to be related to salt diapir uplift.
The Global Volcanism Program is not aware of any Holocene eruptions from Gada Ale. If this volcano has had large eruptions (VEI >= 4) prior to 10,000 years ago, information might be found on the Gada Ale 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.
|Kibreale | Chebrit Ale | Kebrit Ale|
|Feature Name||Feature Type||Elevation||Latitude||Longitude|
|Catherine||Tuff ring||100 m||13° 55' 0" N||40° 25' 0" E|
|Gada Ale (upper right) is the most prominent volcano at the northern end of the Erta Ale Range. The 287-m-high volcano is seen here from the south, with two small lakes on its lower NW flank. Lake Aasale (Lake Karum), whose surface lies about 116 meters below sea level, is in the background. Prominent fissures (lower right) are adjacent to an uplifted salt dome (lower left). Salt diapir uplift has affected both this 2-km-wide area west of the volcano (where lava flows are uplifted as much as 100 m) and Gada Ale itself.
Copyrighted photo by Marco Fulle, 2002 (Stromboli On-Line, http://stromboli.net).
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.
Barberi F, Varet J, 1970. The Erta Ale volcanic range (Danakill depression, Northern Afar, Ethiopia). Bull Volc, 34: 848-917.
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.
Pagli C, Wright T J, Ebinger C J, Yun S-H, Cann J R, Barnie T, Ayele A, 2012. Shallow axial magma chamber at the slow-spreading Erta Ale Ridge. Nature Geoscience 5, 284–288.
Richard J J, Neumann van Padang M, 1957. Africa and the Red Sea. Catalog of Active Volcanoes of the World and Solfatara Fields, Rome: IAVCEI 4: 1-118.
WoldeGabriel G, 1987. . (pers. comm.).