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New research published in Nature Geoscience in June 2026 reconstructs how the Euphrates River formed millions of years ago, identifying two ancestral rivers in Anatolia that merged and were rerouted by tectonic activity.
Using seismic-reflection imaging, onshore geological mapping and computer modelling, the team—led in part by geologist Andrew Madof at Chevron—traced the Paleo‑Karasu and Paleo‑Murat systems which once drained into the then‑dried Mediterranean during the Messinian Salinity Crisis.
The analysis suggests the paleo‑rivers were gigantesque—estimates put the Paleo‑Karasu’s discharge larger than the Nile and the Paleo‑Murat greater than the modern Tigris and Euphrates combined—and that between roughly 3.6 million and 1.6 million years ago tectonic shifts on Anatolia’s faults swung their courses southeast, producing the single river system now known as the Euphrates.
Authors note remaining uncertainty because conclusions rely on remote seismic and modelling data; targeted field sampling would help corroborate channel pathways and timings.
The findings shed new light on landscape evolution that helped shape the Fertile Crescent and inform debates about regional paleoclimate and sedimentary basins.








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