Produced & Designed by: Manoj Kumar
Scientists have discovered remnants of a 120-million-year-old tectonic plate, now called Pontus, hidden beneath Borneo. This ancient piece of Earth’s crust dates back to the time when supercontinent Pangaea began breaking apart.
The discovery of Pontus was made by Suzanna van de Lagemaat, a geologist at Utrecht University, and her supervisor. They analyzed rock formations in northern Borneo, leading to the identification of this long-lost plate.
Van de Lagemaat initially thought she was studying remnants of a known lost plate. But magnetic research on Borneo rocks revealed signs of a previously unknown tectonic plate—Pontus—originating much farther north.
Researchers estimate that the Pontus plate, now swallowed by other plates, once stretched beneath an ocean separating Eurasia and Australia. It was about a quarter of the size of today’s Pacific Ocean, based on reconstructions.
Pontus existed before the breakup of Pangaea. As this ancient landmass split, Pontus gradually disappeared under other plates, contributing to the tectonic shifts that moved regions like Borneo and the Philippines.
Van de Lagemaat’s study centered on the Junction Region—a hotspot of tectonic activity stretching from Japan to New Zealand. This complex area holds clues to the ancient movements that shaped Earth’s current geography.
Through magnetic lab research, the team discovered that the rocks from Borneo carried a distinct magnetic signature, indicating their origins in a much older and distant part of the Earth’s crust.
Using geological data, Van de Lagemaat reconstructed a video clip that tracks the movement of tectonic plates from the dinosaur age to today. It visualizes Pontus’ journey as it vanished beneath shifting continents.
This discovery is part of a larger effort to understand hidden parts of our planet’s history, including submerged oceans and lost continents, revealing how Earth’s surface has changed over millions of years.