The global mid-ocean ridge, with a total length over 65,000 km, is the longest volcanic chain on Earth. Hot magmas are extracted from the upwelling asthenosphere beneath the ridge axis to produce ...

The global mid-ocean ridge, with a total length over 65,000 km, is the longest volcanic chain on Earth. Hot magmas are extracted from the upwelling asthenosphere beneath the ridge axis to produce ...

"It's tearin' up my heart when I'm with you, but when we are apart, I feel it, too." Sure, it's a great opener to a pop song, but it also briefly describes what's happening to Africa. The continent is ...

There’s a giant blob of incredibly hot rock beneath New Hampshire — and it may be part of the reason the Appalachian Mountains are still standing tall, according to new research. It has, however, been ...

Too deep to see or reach via drilling, the Moho (crust-mantle transition) remains something of a mystery more than a hundred years after its discovery. This insightful, multidisciplinary volume ...

ABSTRACT: The current magma formation theory has many shortcomings and is unable to address issues such as the origin of granites and the source of oceanic seamount magmas, and its evolution is ...

ABSTRACT: The current magma formation theory has many shortcomings and is unable to address issues such as the origin of granites and the source of oceanic seamount magmas, and its evolution is ...

The Earth’s interior is far more complex than what we are taught in school. Instead of just three layers- crust, mantle, and core- the Earth is made up of multiple intricate layers, each with its own ...

The interplay between the lithosphere and the asthenosphere is central to the science of plate tectonics and greatly influences the geological processes and features we observe on the Earth’s surface.

The mechanism facilitating the smooth movement of the oceanic lithosphere over the underlying asthenosphere (upper mantle) remains poorly understood. Recently, researchers from Japan investigated the ...

Planet Earth consists of a crust, a mantle, and a core — so then what’s the asthenosphere? Wait, there’s something called a lithosphere too? What gives?! Schematic of the layers and sub-layers of ...