Erta Ale rises in the Afar Region of northeastern Ethiopia, within the Danakil Depression near the Eritrean border, reaching 613 meters as a continuously active basaltic shield volcano. It sits at the Afar triple junction, where the African, Arabian and Somali tectonic plates meet near the southern end of the Red Sea Rift, and its mafic lavas were brought to the surface by dike emplacement during rifting events. Erta Ale holds one or two active lava lakes at its summit, occasionally overflowing to the south, and is notable for the longest-existing lava lake known anywhere, present continuously since at least 1906. Significant eruptions occurred in 2005, 2007 and 2008, and a further eruptive episode ran from January 2017 through at least April 2024, with volcanic pulses continuing across that span. This entity documents Erta Ale specifically as a geological formation, a rift-zone shield volcano holding the world's longest continuously active lava lake.
Facts
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Source Erta Ale (Wikipedia)
Caused By
Source Erta Ale (Wikipedia)
Wikidata P31 formation-type mapped to formative process Volcanism via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.
Source Wikidata: Erta Ale
In Discipline
Wikidata P31 formation-type mapped to discipline Volcanology via reviewed judgment map (earth atlas); source citation is this entity's own cited Wikidata item.
Source Wikidata: Erta Ale
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Source Wikidata: Erta Ale
Sources
1. Smithsonian Institution Global Volcanism Program: Volcanoes of the World, Holocene volcanoes service
Smithsonian Institution Global Volcanism ProgramVolcanoes of the World, volcano 221080Quote, Volcanoes of the World, volcano 221080
"Volcano_Name": "Erta Ale" ... "Last_Eruption_Year": 2025
View the Source Wikidata: Erta Ale
Erta Ale (Wikipedia)
Associated With: Basalt, Lead paragraph
It is composed of basalt, and it is the most active of the volcanoes in Ethiopia.
Caused By: Rifting, Article text, process Rifting
Specifically, it lies almost at the end of the southern Red Sea Rift, where tectonic extension (via normal faults) proceeds in conjunction with igneous intrusions to generate a new oceanic crust between Africa and Arabia.
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