Scientists have made a groundbreaking discovery that has been hidden beneath the Earth's surface for millions of years. Two colossal, ultrahot structures, known as large low-shear-velocity provinces (LLSVPs), have been found to be responsible for shaping the planet's magnetic field.
The two massive structures are estimated to be comparable in size to Africa and remain buried at a depth of 2,900 kilometers beneath the Earth's surface. Low-lying surface vertical velocity (LLVV) regions are irregular areas of the mantle where the material is hotter, denser, and chemically different from the surrounding material.
Researchers have long suspected the existence of these anomalies, first proposing them in the late 1970s. However, it wasn't until two decades later that they were able to confirm their presence, followed by another decade of research that led to a direct link between the LLSVPs and the magnetic field.
The study published this week in Nature Geoscience, led by researchers at the University of Liverpool, found that temperature differences between LLSVPs and surrounding mantle material alter the flow of liquid iron in the core. This movement of iron is responsible for generating the Earth's magnetic field.
When analyzing how the magnetic field should look if the mantle were uniform versus how it behaves when including these heterogeneous regions with structures, researchers compared their findings to real magnetic field data. The model that incorporated LLSVPs replicated the observed irregularities and patterns in the magnetic field.
These findings have significant implications for understanding ancient continental configurations, climate, paleobiology, and natural resources. It has been assumed for a long time that Earth's magnetic field behaves as a perfect bar magnet aligned with the planet's rotational axis. However, this study suggests otherwise, providing new insights into the complex dynamics of our planet.
The research was conducted by a team led by Professor Andy Biggin, who stated that "the current model of the geodynamo is no longer valid." The discovery has sparked excitement among scientists and shed light on the intricate mechanisms driving the Earth's magnetic field.
The two massive structures are estimated to be comparable in size to Africa and remain buried at a depth of 2,900 kilometers beneath the Earth's surface. Low-lying surface vertical velocity (LLVV) regions are irregular areas of the mantle where the material is hotter, denser, and chemically different from the surrounding material.
Researchers have long suspected the existence of these anomalies, first proposing them in the late 1970s. However, it wasn't until two decades later that they were able to confirm their presence, followed by another decade of research that led to a direct link between the LLSVPs and the magnetic field.
The study published this week in Nature Geoscience, led by researchers at the University of Liverpool, found that temperature differences between LLSVPs and surrounding mantle material alter the flow of liquid iron in the core. This movement of iron is responsible for generating the Earth's magnetic field.
When analyzing how the magnetic field should look if the mantle were uniform versus how it behaves when including these heterogeneous regions with structures, researchers compared their findings to real magnetic field data. The model that incorporated LLSVPs replicated the observed irregularities and patterns in the magnetic field.
These findings have significant implications for understanding ancient continental configurations, climate, paleobiology, and natural resources. It has been assumed for a long time that Earth's magnetic field behaves as a perfect bar magnet aligned with the planet's rotational axis. However, this study suggests otherwise, providing new insights into the complex dynamics of our planet.
The research was conducted by a team led by Professor Andy Biggin, who stated that "the current model of the geodynamo is no longer valid." The discovery has sparked excitement among scientists and shed light on the intricate mechanisms driving the Earth's magnetic field.