Scientists have uncovered evidence of two colossal, deep-Earth "blobs" that have significantly shaped the planet's magnetic field over millions of years. These massive rock formations, roughly 1,864 miles beneath Africa and the Pacific Ocean, are thought to be solid, superheated material, creating a significant temperature gradient in the rocky mantle.
According to researchers, these blobs, or basal structures, play a crucial role in sustaining Earth's fluid outer core, known as the geodynamo. By generating electric currents through the motion of extremely hot iron and nickel, the blobs help maintain the planet's magnetic field. Without this internal heat transfer from the core to the mantle and ultimately to the surface, scientists believe that Earth would be devoid of its magnetic properties.
The discovery was made possible by studying the magnetic records contained in rocks, which provide a record of the direction of Earth's magnetic field at different times and locations. Researchers noticed distinct patterns in these records, particularly among rocks up to 250 million years old. These findings suggested a correlation between magnetic directions and geographical coordinates.
To test their hypothesis, the researchers developed advanced simulations that mapped out Earth's magnetic field based on varying heat profiles for the core, mantle, and blobs. The results showed that including strong variations in heat transfers – characteristic of active blob movement – most accurately depicted the planet's actual magnetic field.
According to lead author Andrew Biggin, the presence of these blobs contributes to the overall stability of the magnetic field, with certain sections remaining stagnant for hundreds of millions of years. He posits that the blobs are insulating the liquid metal beneath them, preventing heat loss that would otherwise cause it to contract and sink into the core.
However, scientists remain unsure about the true origin and nature of these enigmatic blobs. The discovery highlights their significance in maintaining Earth's magnetic field, which is essential for our planet's climate regulation and navigation systems.
According to researchers, these blobs, or basal structures, play a crucial role in sustaining Earth's fluid outer core, known as the geodynamo. By generating electric currents through the motion of extremely hot iron and nickel, the blobs help maintain the planet's magnetic field. Without this internal heat transfer from the core to the mantle and ultimately to the surface, scientists believe that Earth would be devoid of its magnetic properties.
The discovery was made possible by studying the magnetic records contained in rocks, which provide a record of the direction of Earth's magnetic field at different times and locations. Researchers noticed distinct patterns in these records, particularly among rocks up to 250 million years old. These findings suggested a correlation between magnetic directions and geographical coordinates.
To test their hypothesis, the researchers developed advanced simulations that mapped out Earth's magnetic field based on varying heat profiles for the core, mantle, and blobs. The results showed that including strong variations in heat transfers – characteristic of active blob movement – most accurately depicted the planet's actual magnetic field.
According to lead author Andrew Biggin, the presence of these blobs contributes to the overall stability of the magnetic field, with certain sections remaining stagnant for hundreds of millions of years. He posits that the blobs are insulating the liquid metal beneath them, preventing heat loss that would otherwise cause it to contract and sink into the core.
However, scientists remain unsure about the true origin and nature of these enigmatic blobs. The discovery highlights their significance in maintaining Earth's magnetic field, which is essential for our planet's climate regulation and navigation systems.