The continent of Asia is being pulled apart from within

Nature · Published 22 October 2026 Swipe more like this →

In short: Geology often teaches us that tectonic movements are either successful—creating new oceans—or failed, becoming dormant. However, new research into the Gulf of Suez reveals a middle path. This rift never actually stopped; it simply decelerated, continuing to pull the landmass apart at a persistent, glacial pace.

Acting as a central example of 'failed' rifts, the Gulf of Suez separates parts of Asia and Africa. Conventional geological narratives suggested that the Arabian plate pulled away from the African plate 28 million years ago and then ceased its movement about 5 million years ago. However, recent findings by geoscientists, including David Fernández-Blanco, indicate that the rift is still active, widening by approximately 0.02 inches (0.5 millimeters) per year.

This discovery challenges the binary model of rift evolution. Instead of a complete halt, the tectonic action shifted 5 million years ago toward the Dead Sea, where a new plate boundary is forming. While the primary rifting slowed, it remains active enough to lift ancient coral reefs up to 60 feet (18.5 meters) above sea level and create unique river profiles that cannot be explained by erosion alone.

This movement is part of a broader, restless Asian landscape. The Himalayas and Tibetan Plateau are currently being warped by Asia's ongoing collision with India. Simultaneously, subduction beneath Japan and Indonesia feeds active volcanic systems. These forces—collisions, faulting, and rifting—demonstrate that the continent is not geologically settled but is constantly being reshaped by the churning currents of the molten mantle below.

The mechanism driving these changes lies in the lithosphere, the Earth's outer shell. Driven by convection cells in the mantle, plates move at rates of one to two inches per year. Whether they are crumpling into mountains like the Himalayas or pulling apart to create new terrain, these movements release 'elastic strain' energy, resulting in the earthquakes and volcanic activity that define the continent's ongoing evolution.

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