New Evidence Reveals Ancient Earth Structures Altered Magnetic Field for Millions of Years
A groundbreaking study has discovered that two massive, continent-sized structures hidden deep beneath the Earth's surface have been shaping the planet's magnetic field for over 265 million years. The findings, published in Nature Geoscience, provide new insights into the dynamic processes that govern our planet's magnetic field and challenge current understanding of the Earth's interior.
Researchers at the University of Liverpool have identified two large low-shear-velocity provinces (LLSVPs), which are vast regions of hot, dense rock that extend from the Earth's mantle to a depth of approximately 2,900 kilometers. These massive structures are capable of modifying the flow of liquid iron in the core, responsible for generating the magnetic field.
The team's analysis and simulations revealed that temperature differences between LLSVPs and surrounding mantle material create an asymmetry, leading to unequal acceleration or deceleration of liquid iron movement. This results in an irregular shape for the magnetic field, which is currently observed on Earth.
The study's lead author, Professor Andy Biggin, noted that previous assumptions about the behavior of the Earth's magnetic field may be incorrect, citing the long-standing uncertainty surrounding ancient continental configurations and the formation of natural resources. The findings also shed light on the role of these structures in shaping the planet's climate and paleobiology.
This groundbreaking research highlights the complex dynamics at play within our planet's interior and underscores the importance of continued exploration and discovery into the Earth's structure and processes.
A groundbreaking study has discovered that two massive, continent-sized structures hidden deep beneath the Earth's surface have been shaping the planet's magnetic field for over 265 million years. The findings, published in Nature Geoscience, provide new insights into the dynamic processes that govern our planet's magnetic field and challenge current understanding of the Earth's interior.
Researchers at the University of Liverpool have identified two large low-shear-velocity provinces (LLSVPs), which are vast regions of hot, dense rock that extend from the Earth's mantle to a depth of approximately 2,900 kilometers. These massive structures are capable of modifying the flow of liquid iron in the core, responsible for generating the magnetic field.
The team's analysis and simulations revealed that temperature differences between LLSVPs and surrounding mantle material create an asymmetry, leading to unequal acceleration or deceleration of liquid iron movement. This results in an irregular shape for the magnetic field, which is currently observed on Earth.
The study's lead author, Professor Andy Biggin, noted that previous assumptions about the behavior of the Earth's magnetic field may be incorrect, citing the long-standing uncertainty surrounding ancient continental configurations and the formation of natural resources. The findings also shed light on the role of these structures in shaping the planet's climate and paleobiology.
This groundbreaking research highlights the complex dynamics at play within our planet's interior and underscores the importance of continued exploration and discovery into the Earth's structure and processes.