The discovery of a gravity anomaly in the Indian Ocean, commonly referred to as the “gravity hole,” has intrigued geologists for decades. This enigmatic spot, where Earth’s gravitational pull is unusually weak, its mass lower than normal, and the sea level dips by over 328 feet (100 meters), has long posed a puzzle to scientists. Recent research by the Indian Institute of Science in Bengaluru, India, has shed new light on this phenomenon, attributing it to deep magma plumes akin to those that form volcanoes.
Understanding Earth’s Irregular Shape and Gravity Anomalies
Contrary to the common perception of Earth as a perfect sphere, our planet is more akin to a “lumpy potato,” as described by study coauthor Attreyee Ghosh, a geophysicist and associate professor at the Centre for Earth Sciences of the Indian Institute of Science. Earth is technically an ellipsoid, bulging at the equator due to its rotation. This irregular shape, combined with varying densities within the planet, affects gravity and the sea level.
The “gravity hole,” or the Indian Ocean geoid low, represents the lowest point in Earth’s geoid—a hypothetical sea level surface shaped by gravitational pull. This geoid low creates a circular depression starting just off India’s southern tip, covering approximately 1.2 million square miles (3 million square kilometers). Dutch geophysicist Felix Andries Vening Meinesz first discovered this anomaly in 1948 during a gravity survey from a ship.
The Role of Magma Plumes in Geoid Formation
To unravel the mystery of the Indian Ocean geoid low, Ghosh and her colleagues utilized supercomputers to simulate geological processes dating back 140 million years. Their research, published in the journal Geophysical Research Letters, suggests that the anomaly is a result of magma plumes originating from deep within the Earth. These plumes, which are columns of hot molten rock rising through the mantle, influence the planet’s density and gravitational field.
By running 19 different simulations, the researchers recreated the tectonic shifts and magma dynamics over millions of years. In six of these scenarios, a geoid low similar to the one in the Indian Ocean emerged, characterized by the presence of magma plumes. These plumes are thought to have formed due to the subduction of an ancient oceanic plate beneath the Indian plate as it drifted northward and collided with Asia.
The Disappearance of an Ancient Ocean
About 140 million years ago, the Indian subcontinent was positioned much further south, separated from Asia by an ocean. As the Indian plate moved northward, this ocean disappeared, causing the oceanic plate to subduct into the mantle. This process likely generated magma plumes, bringing low-density material closer to the Earth’s surface and contributing to the formation of the geoid low.
The simulations indicated that the geoid low formed around 20 million years ago. However, whether it will persist or eventually disappear remains uncertain. Plate movements and mantle dynamics could alter its characteristics over hundreds of millions of years.
Evaluating the Research Findings
While the study provides a compelling explanation for the Indian Ocean geoid low, some experts have noted limitations in the simulations. Dr. Alessandro Forte, a professor of geology at the University of Florida, pointed out that the models failed to reproduce the significant mantle plume that caused the Deccan Traps volcanic eruptions 65 million years ago. This plume, located under present-day Réunion Island, is a notable omission from the simulation.
Moreover, Forte highlighted discrepancies between the simulated geoid and the actual geoid, particularly in regions like the Pacific Ocean, Africa, and Eurasia. The study reported an 80% correlation between the predicted and observed geoids, suggesting room for improvement in the models.
The Future of Geoid Low Studies
Despite these challenges, the research marks a significant advancement in understanding the Indian Ocean’s gravity anomaly. It underscores the complexity of Earth’s internal processes and their impact on surface features. Further studies, incorporating more precise data and additional factors, will help refine these models and enhance our understanding of such anomalies.
Ghosh acknowledged the inherent uncertainties in simulating Earth’s geological past, especially as one goes further back in time. “We cannot take into account each and every possible scenario,” she said, “but we believe the overall reason for this low is sound.”
The investigation into the Indian Ocean’s gravity hole highlights the intricate interplay between geological processes and gravitational anomalies. By tracing the origins of this geoid low to ancient magma plumes and tectonic shifts, researchers have provided a plausible explanation for a long-standing geological mystery. This discovery not only enriches our understanding of Earth’s dynamic history but also opens new avenues for exploring the planet’s complex interior and its impact on surface phenomena. As science advances, the continuous refinement of these models promises to unravel even more secrets hidden beneath our planet’s surface.
