Deep Earth Pulses Detected Beneath Africa
A Lancaster University statistician is part of a team uncovering evidence of rhythmic surges of molten mantle rock rising from deep within the Earth beneath Africa.
The Discovery: Rhythmic Mantle Surges
Researchers from Lancaster University and other institutions have detected pulses of molten mantle rock rising beneath Africa. These pulses are believed to be a key factor in the ongoing process of continental rifting.
Continental Rifting Explained
The surges of molten material contribute to the gradual tearing apart of the African continent. This geological process, known as continental rifting, is reshaping the landscape over millions of years.
Implications for Earth Sciences
Understanding these deep earth processes is crucial for advancing our knowledge of plate tectonics, volcanism, and the overall evolution of our planet. This discovery opens new avenues for research into the dynamics of the Earth's interior.
For more information on Earth Science Research, visit our dedicated page.
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