Continent-sized structures of mineral protruding from the lower mantle towards Earth’s outer core may be contributing to an instability of our planet’s magnetic field.
The two odd formations – one under the Pacific and the other beneath…
Continent-sized structures of mineral protruding from the lower mantle towards Earth’s outer core may be contributing to an instability of our planet’s magnetic field.
The two odd formations – one under the Pacific and the other beneath…