After decades of scientific speculation, geophysicists have made a breakthrough in understanding one of Earth’s most perplexing geophysical enigmas—a massive gravitational anomaly beneath the Indian Ocean. Often referred to as the “gravity hole,” this vast region exhibits significantly weaker gravitational pull compared to surrounding areas. Recent research combining advanced seismic modeling and geological data now points to ancient tectonic shifts and submerged mantle plumes as key drivers behind the anomaly.