Geologists drilled 4,160 feet into the Atlantic seabed and it changed our understanding of Earth

Earth was formed millions of years ago. Its structure has been a source of fascination for scientists for years. However, we haven't been able to explore the layers of our planet beyond its crust. Recently, scientists drilled a record-breaking 1,268 meters (4,160 feet) into Earth’s mantle. The drilling done in the volcanically active region of the mid-Atlantic ridge on the floor of the Atlantic Ocean allowed the scientists to get a glimpse into the inaccessible layer of the mantle, per IFL Science. The exact findings of the research have been published in the journal Science. 

Led by Professor Johan Lissenberg from Cardiff University’s School of Earth and Environmental Sciences, the experiment was conducted using an ocean-drilling vessel, JOIDES Resolution. While the attempts started as early as the 1960s, experts were finally able to recover rocks to understand the mantle’s history. “Our study begins to look at the composition of the mantle by documenting the mineralogy of the recovered rocks, as well as their chemical makeup,” Professor Lissenburg said, per a news release. He added that the findings were not just a record-breaking achievement but a profound source for further exploration. “Its value is in what the cores of mantle rocks could tell us about the makeup and evolution of our planet,” he remarked. 

Revealing what they found with their extensive drilling, it was mentioned that it was far different from what the researchers had predicted or expected. “Our results differ from what we expected. There is a lot less of the mineral pyroxene in the rocks, and the rocks have very high concentrations of magnesium, both of which result from much higher amounts of melting than what we would have predicted,” the professor highlighted. Going beyond the composition of the rocks and their changes over many years, there was also an understanding of how the rocks in the mantle melted over the years. 

“We also found channels through which melt was transported through the mantle, and so we can track the fate of magma after it is formed and travels upwards to the Earth’s surface,” Lissenburg explained. He added that this tracking can help provide insight into what feeds volcanoes, especially the ones on the surface of the Earth. “Having access to these mantle rocks will allow us to make the connection between the volcanoes and the ultimate source of their magma,” he pointed out. Dr Susan Q Lang, an associate scientist in Geology and Geophysics, said that the rocks found in the mantle closely resembled rocks present on the early Earth. Both seemed different from the rocks that today’s continents are composed of. 

This information allows the researchers to dive into what the compositions looked like millions of years ago. “Analyzing them gives us a critical view into the chemical and physical environments that would have been present early in Earth’s history and that could have provided a consistent source of fuel and favorable conditions over geologically long timeframes to have hosted the earliest forms of life,” Lang explained. 30 scientists who took part in the discovery are proud of their ground-breaking achievement and are hoping to open up several avenues for future study.