Danakil Depression, where salt flats meet active volcanoes

Danakil Depression and Dallol sit in Ethiopia’s rift landscape, where salt pans, volcanic cones and mineral colours shape the scene.

Danakil Depression in Ethiopia is a vast rift basin shaped by the East African Rift System, with Dallol near its northern end. The floor lies far below sea level and opens onto salt pans, volcanic cones and bright mineral deposits.

Rift basin and salt plain

The depression lies between the Ethiopian Plateau and the Danakil microplate, in the northern Afar region. It is part of a tectonic zone where the crust is pulling apart, and the landscape records that movement in faults, basins and volcanic landforms.Dallol geothermal area

The northern half includes salt flats and evaporitic surfaces around Lake Karum and the Dallol area. The basin reaches about 124 m below sea level at its lowest recorded points, placing it among Africa’s deepest land surfaces.124 m below sea level

Dallol and the volcanic edge

Dallol sits within the depression as a volcanic and geothermal area with salt, brine and vivid mineral crusts. The landscape includes hot springs, hydrothermal fields and sulphur-rich deposits that stain the ground in greens, yellows and rust tones.geothermal area

The Dallol volcanic dome rises only a short way above the surrounding salt plain, and its summit crater marks a compact volcanic form rather than a broad mountain. The nearby Erta Ale volcanic range belongs to the same wider rift setting and underlines the active geology of the depression.Dallol volcanic dome

A landscape of extreme contrast

What makes Danakil Depression distinctive is the visible combination of depth, salt and volcanism. The place is not a single feature but a whole basin where tectonic rifting, evaporation and volcanic activity meet in one low-lying expanse.

Scientists place the formation of the Danakil rift in the Miocene, with rifting continuing through the present geological setting. That long timescale helps explain why the basin, the salt flats and the volcanic fields read as parts of one continuous terrain.Miocene

Visiting Danakil Depression: what travellers from Western Europe should know

• The depression lies in northern Ethiopia, near the border with Eritrea. Dallol and the salt flats are reached by road from the wider Afar region.
• The terrain is low, open and exposed, with salt crusts, rough volcanic ground and hot ground in the Dallol area. Footing changes from hard salt surfaces to uneven mineral surfaces.
• The official language is Amharic and the currency is the Ethiopian birr.
• Entry requirements depend on your nationality; UK travellers can check the FCDO travel advice at gov.uk/foreign-travel-advice, Irish travellers the Department of Foreign Affairs at ireland.ie.

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Frequently asked questions about Danakil Depression

Where is Danakil Depression?

Danakil Depression lies in northern Ethiopia, in the Afar region near the border with Eritrea. It forms part of the broader Afar rift system.

What does a visit involve?

The landscape centres on salt flats, volcanic ground and geothermal features around Dallol. Paths and surfaces are uneven, and the terrain changes from place to place.

What makes it distinctive?

The depression combines deep lowland topography with salt, volcanism and active rifting. Dallol adds strong mineral colour and geothermal landforms to that setting.