4.A recent study has found that a sinking oceanic slab beneath the Zagros Mountains in northern Iraq is pulling the region downward.
The Neotethys oceanic slab, which formed over 66 million years ago, is splitting and sinking into the Earth's mantle, influencing the region's topography.
About: The Zagros Mountains are a major mountain range extending from southeastern Turkey to northwestern Iran, with parts in northern Iraq.
The sinking of the region is due to plate tectonics, specifically a growing tear in the Neotethys oceanic slab between the Arabian and Eurasian plates. The process is extremely slow and occurs over millions of years.
The depression surrounding the Zagros Mountains is deeper than expected, suggesting a significant impact of tectonic plate interactions.
By studying rock records, sediments, and deep-earth imaging, researchers confirmed the sinking of the Neotethys slab, which is gradually pulling northern Iraq downward.