Scientists have discovered a massive Pacific plateau, the Melanesian Border Plateau, larger than the US state of Idaho, that has been growing on the sea floor near Fiji since the age of dinosaurs. Research suggests it formed through four separate pulses of volcanism and continues to grow to this day. The plateau began forming 120 million years ago and its history is more complex than previously thought, shedding light on the poorly understood nature of underwater volcanic features.
Scientists have discovered a massive volcanic superstructure, the Melanesian Border Plateau, the size of Idaho beneath the Pacific Ocean, formed by four distinct periods of volcanic eruptions over 100 million years ago. This structure, larger than Idaho, is still growing and contains rare elements used in technology and medical devices. The research sheds light on the forces that shaped the Earth and may provide insight into its future, while also suggesting that similar oceanic mid-plate superstructures likely exist in the South Pacific.
Scientists have discovered a massive "superstructure" on the sea floor near Fiji, known as the Melanesian Border Plateau, which has been growing since the age of dinosaurs due to volcanic eruptions. Research suggests that the plateau formed through four separate pulses of volcanism and continues to grow to this day. This discovery sheds light on the complex history of underwater volcanic features and challenges previous assumptions about their formation.
A vast volcanic superstructure, the Melanesian Border Plateau, has been discovered in the Pacific Ocean, covering around 222,000 square kilometers. Research led by University of Nevada geoscientist Kevin Konrad has uncovered evidence of its formation, shedding light on the forces that shape our planet. The plateau's creation involved multiple volcanic structures over millions of years, influenced by hotspots in the mantle. Understanding the slow, complex formation of such superstructures could provide insights into climate change and past extinction events, and may lead to the discovery of similar formations in other parts of the world.
Scientists are unraveling the mystery of the Melanesian Border Plateau, a massive igneous rock superstructure beneath the Pacific Ocean, which is believed to have formed through four distinct episodes of volcanic activity over tens of millions of years. Unlike other major structures, this plateau's formation was not the result of a single event. Research suggests that such superstructures may have minimal environmental impacts and that further exploration of the world's oceans may reveal more complex ocean mid-plate superstructures.
Scientists have discovered a massive Pacific plateau, the Melanesian Border Plateau, that has been growing on the sea floor near Fiji since the age of dinosaurs. This underwater superstructure, larger than the US state of Idaho, began forming due to volcanic eruptions during the Cretaceous period and has continued to grow through four separate pulses of volcanism. The plateau's complex history, revealed in a new study, sheds light on the formation of underwater volcanic features and suggests it began forming 120 million years ago.
The Melanesian Border Plateau, an undersea plateau in the Pacific Ocean, has been growing since the dinosaur age through multiple volcanic events, according to new research. This plateau, larger than Idaho, formed over millions of years through different volcanic pulses, and its timeline is crucial for understanding similar features in the Pacific basin. The study's findings shed light on the complex formation of undersea features and may lead to the identification of similar structures in the South Pacific.
