Dallol, Hydrothermal system in Kilbet Rasu, Ethiopia.
Dallol is a hydrothermal system with salt formations, iron oxide pools, and sulfur springs located about 91 meters below sea level. The landscape consists of colorful mineral deposits and hot springs that together create an extraordinary terrain.
The volcanic formation emerged in 1926 when underground water pressure caused an eruption. This led to the creation of a network of geysers and acidic thermal springs in the area.
The Afar communities extract salt from this region and transport mineral blocks along traditional desert routes using camel caravans. This practice has shaped the daily life of people in this harsh area for many generations.
Access requires permits, guided tours, and specialized vehicles due to extreme heat and remote desert location. It is important to travel with an experienced guide and follow local safety guidelines.
Scientists study microorganisms living in the mineral chimneys here, as they survive in conditions similar to those on Mars. These findings contribute to understanding where else life might exist in the universe.
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