Scientists have discovered a mysterious lost world deep in the Pacific Ocean. This unusual finding caused astonishment in the scientific world.
An international team of geophysics has discovered a mysterious discovery deep in the Pacific Ocean, thanks to a new imaging method they developed to measure the speed of seismic waves created by earthquakes. lost world discovered. These findings, which emerged as a result of the joint work of researchers from ETH Zurich and the California Institute of Technology (Cal Tech), astonished scientists. The new technique revealed previously unnoticed anomalies in the mantle layer beneath the ocean.
The Lost World Mysterious Regions in the Mantle
The researchers analyzed the earthquake waves using a method called “full waveform inversion.” By examining different types of waves simultaneously, this method allowed detecting regions called “subduction zones” located deep in the mantle. But this time, anomalies in the speed of seismic waves appeared in unexpected places. Researchers stated that these anomalies were found in regions that did not show any tectonic activity in the past geological history.
Thomas Schouten, a researcher at ETH Zurich, said: “We do not have precise information about the origin of these regions. “More data is needed to understand what kind of material the patterns we observe are made of,” he said. Scientists think these regions may be accumulations of ancient silica-rich materials or iron-rich rocks that have existed since the formation of the mantle.
Researchers stated that they will examine the speed of earthquake waves and the properties of matter in more detail to better understand the lost world. This will be an important step in understanding how different types of material in the mantle affect the speed of waves.
This discovery, which had a great impact in the scientific world, shows that there are still many mysteries waiting to be discovered deep within the Earth. This lost world beneath the Pacific Ocean looks set to pave the way for new research in geology and geophysics.