Geology of the Dead Sea region

The Dead Sea region's geology is shaped by its location along the Dead Sea Rift, a major fault line between the African and Arabian tectonic plates. This tectonic activity causes the land to sink, forming the deep, salt-rich basin known as the Dead Sea. Over millions of years, mineral-rich waters have evaporated, depositing thick layers of salt and minerals. The region's geology features rugged cliffs, fault lines, and sedimentary layers, reflecting ongoing tectonic processes and historical geological changes. This active geological environment creates the unique landscape and high mineral content that make the Dead Sea scientifically significant.