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The mysterious ‘gravity hole’ in the Indian Ocean that has baffled scientists for years

This hole was first discovered by Dutch geophysicist Felix Andries Vening Meinesz in 1948 and has remained a mystery, till now.

The mysterious ‘gravity hole’ in the Indian Ocean that has baffled scientists for years
Representative Cover Image Source: Pexels | Emiliano Arano

Unlike “black holes” that attract and swallow the surrounding cosmic matter, a “gravity hole” pushes away the surrounding material due to lack of gravitational force. When formed in an ocean, a gravity hole pushes away water and creates pockets of air where there should have been water, lowering the sea level. Take the instance of the world’s largest, and deepest gravity hole, discovered in the Indian Ocean. Causing the sea level to dip by 348 feet (106 meters), the hole perplexed geologists for decades, until 2023, when some researchers gave a potential explanation for it in a study published in the journal Geophysical Research Letters. The mystery lies in a sunken ancient Indian sea, reported CNN.

Representative Image Source: Cape Agulhas, the southern tip of the African continent. The official dividing line between the Atlantic and Indian Oceans. (Photo by David Silverman/Getty Images)
Representative Image Source: Cape Agulhas, the southern tip of the African continent. The official dividing line between the Atlantic and Indian Oceans. (Photo by David Silverman/Getty Images)

Called the “Indian Ocean geoid low (IOGL),” this gravity hole is located about 1,200 kilometers (750 miles) southwest of Kanyakumari, the southernmost tip of the Indian subcontinent. It is a 1.2 million-square-mile (3 million square kilometers) circular depression lurking in the ocean’s waters. Compared with its surroundings, the gravity is weaker in this area. “It is by far the biggest low in the geoid, and it hasn’t been explained properly,” said study co-author, Attreyee Ghosh, a geophysicist and associate professor at the Centre for Earth Sciences of the Indian Institute of Science.

Representative Image Source: A wave in the Pacific Ocean breaks along the shore of La Jolla's Windansea Beach. (Photo by Kevin Carter/Getty Images)
Representative Image Source: A wave in the Pacific Ocean breaks along the shore of La Jolla's Windansea Beach. (Photo by Kevin Carter/Getty Images)

Initially, a Dutch geophysicist, Felix Andries Vening Meinesz, discovered the hole, in 1948, during a gravity survey from a ship. Felix had invented a device called “Golden Calf” to measure gravity at seas, per Big Think. Since then, researchers have attempted to explain this oceanic abyss' existence. "The origin of this geoid low has been enigmatic. Different theories were put forward to explain this negative geoid anomaly," the researchers wrote in the study. In 2023, some researchers from the Indian Institute of Science, Bengaluru, proclaimed that they had found an explanation. Their hypothesis is, that the hole was formed as a result of an ancient ocean that no longer exists. They believe that plumes of magma rising from deep inside the planet are responsible for the existence of this gravity hole.

Representative Image Source: This National Oceanic and Atmospheric Association satellite image shows Hurricane Jeanne spinning in the Atlantic Ocean. (Photo by NOAA via Getty Images)
Representative Image Source: This National Oceanic and Atmospheric Association satellite image shows Hurricane Jeanne spinning in the Atlantic Ocean. (Photo by NOAA via Getty Images)

To establish the base for understanding, Ghosh explained that the secret lies in the geometry of Earth. Against what most people believe, Earth is not a perfect sphere. “The Earth is basically a lumpy potato,” she said, “So technically it’s not a sphere, but what we call an ellipsoid, because as the planet rotates the middle part bulges outward.”

Representative Image Source: Image supplied by the European Space Agency. Gravity Satellite Yields 'Potato Earth' View. The image shows how gravitational pull varies across the planet's surface.  (Photo illustration by ESA via Getty Images)
Representative Image Source: Image supplied by the European Space Agency. Gravity Satellite Yields 'Potato Earth' View. The image shows how gravitational pull varies across the planet's surface. (Photo illustration by ESA via Getty Images)

In addition to this, Earth is not even uniform in its density and properties. Some areas are denser than others, which affects Earth’s surface and its gravity, she explained, and added, “If you pour water on the surface of the Earth, the level that the water takes is called a geoid — and that is controlled by these density differences in the material inside the planet because they attract the surface in very different ways depending on how much mass there is underneath.” Live Science described this geometrical anomaly behind the geoid low as, “The low is a consequence of our surprisingly squidgy planet, which flattens at the poles, bulges at the equator and undulates between lumps and bumps across its surface.”

 

Ghosh, with her fellow researchers, took the whole story back to 140 million years ago. She said back then, “the continents and the oceans were in very different places, and the density structure was also very different.” Starting from that timescale, the team plotted 19 simulation models till the present day, recreating tectonic history and the behavior of magma inside the mantle. In six of the models, a geoid low similar to the one in the Indian Ocean formed.

Representative Image Source: Pexels | MD Didar Al Mahmud
Representative Image Source: Pexels | MD Didar Al Mahmud

In each of these six models, they observed the presence of plumes of magma around the geoid low, which they believed were responsible for the formation of the “gravity hole,” said Ghosh. They further suggested these plumes were formed when an ancient Indian ocean disappeared millions of years ago.

Representative Image Source: Pexels | Tyler Hendy
Representative Image Source: Pexels | Tyler Hendy

“India was in a very different place 140 million years ago, and there was an ocean between the Indian plate and Asia. India started moving north and as it did, the ocean disappeared and the gap with Asia closed,” she explained. As per the team, when the oceanic plate squished inside the mantle, it could have prompted the formation of the plumes, bringing low-density material closer to Earth’s surface, reducing the region’s mass and weakening the gravity. Over 100 million years ago, the Indian plate broke off from the supercontinent of Gondwana and smashed into the Eurasian plate. This collision eventually ended up forming the Himalayas, but before that happened, the Indian plate crossed over the Tethys plate, pushing it under the Indian plate.

It was shoved away into the mantle which is the present-day location near East Africa. Eventually, around 20 million years ago, the sinking Tethyan plates moved the African blob's trapped magma, leading to the formation of the plumes. "These plumes, along with the mantle structure in the vicinity of the geoid low, are responsible for the formation of this negative geoid anomaly," the researchers wrote in the study.



 

Discussing whether the gravity hole will stay or shift or disappear, Ghosh told CNN, “That all depends on how these mass anomalies in the Earth move around. It could be that it persists for a very long time. But it could also be that the plate movements will act in such a way to make it disappear, a few hundreds of millions of years in the future.”



 

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