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![Misteri Pembentukan Lubang Gravitasi Terbesar di Bumi yang Luasnya Mencapai Negara India, Akhirnya Terungkap](https://cdns.klimg.com/mav-prod-resized/480x/ori/feedImage/2024/4/8/1712578317858-bfbpu.jpeg)
Dream - Since its discovery in 1948, the gravitational hole at the bottom of the Indian Ocean has remained a perplexing mystery for scientists. Many theories have been proposed by scientists to unravel the mystery of the largest gravitational hole on Earth. Now, a team of researchers from the Indian Institute of Science (IIS) believes they have found the answer to this mystery.
The hole in the Indian Ocean is formed by sunken fragments of the ocean or other much older ocean floors. This gravitational hole is the largest and deepest gravitational anomaly in the world known as the Indian Ocean Geoid Low (IOGL).
Called as an anomaly, because in that mysterious part of the Indian Ocean the gravitational pull is much weaker compared to other places on Earth.
The gravitational hole is centered around 1,200 km southwest of Kanyakumari (Cape Comorin), the southernmost tip of the Indian subcontinent. This circular depression in the ocean has an area of approximately 3 million square kilometers, which is nearly as large as the country of India itself.
The sea surface in the IOGL is lower by up to 106 meters compared to the global average due to lower local gravity. This fact increases the volume of air significantly in a place where there should be water.
The calculation shows that as a result of the anomaly, approximately 100 cubic kilometers of water experienced displacement. The anomaly was discovered by Felix Andries Vening Meinesz, a Dutch geophysicist.
Vening Meinesz discovered a tool to measure gravity at sea. The tool is called Golden Calf and is always carried on a submarine that must remain stationary during the measurement.
As a pioneer in submarine gravimetry, Vening Meinesz spent most of his life exploring the oceans in submarines and research vessels. During his explorations, he discovered several anomalies in the Earth's gravitational field that he associated with tectonic plates. However, he was puzzled because there was nothing larger or stronger than what occurred in the Indian Ocean.
"Unfortunately, Vening Meinesz's theory on the cause of IOGL did not receive much support because at that time there was no computational technology to strengthen his findings. Until finally, the true cause of IOGL was discovered in May 2024 after the journal Geophysical Research Letters published the IIS research."
Using a period 140 million years ago as its basis, the IIS team conducted various simulations through a supercomputer by exploring how tectonic and volcanic forces shaped the world we now know. It turns out that the model produced gravity anomalies that are very similar to IOGL, and they all have one similarity. Low-density magma rises to the surface to replace materials with higher density, thus weakening the gravitational force in that area.
While in a clearer scenario, the IIS team used a period of about 120 million years ago. At that time, the Indian plate separated from the Gondwana supercontinent and collided with the Eurasian plate. The collision resulted in what is now known as the Himalayan Mountains.
However, before that, the Indian Plate passed through the Tethys Plate, so it is called the Tethyan Plate. The fragments of the plate called the Tethyan plate are pushed deeper into the Earth's mantle. They shift some of the material trapped in the 'African blob', which is a continent-sized magma bubble located about 1,000 km below East Africa.
About 20 million years ago, the relatively light substance rose to the surface in the form of a lump and formed a Geoid. Along with the mantle structure near the lower layer of the Geoid, the lump caused gravity anomalies at the southern tip of India.
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