Earth's magnetic field is generated by the churn of its liquid nickel-iron outer core, but it is not a constant feature.

All around the world, from the Red Sea to the deep ocean ridges of the Atlantic, lurk more than a dozen geological misfits.

It turns out that continental breakups are just as messy as human ones, with the events leaving fragments scattered far from home ...

A study on tectonic plates that converge on the Tibetan Plateau has shown that Earth's fault lines are far weaker and the ...

Intelligent technology is allowing organizations to move from episodic transformation to continuous evolution by shrinking the coordination and experimentation costs that once made change slow and ...

This Production Update reports operational progress since April 2025, following bridge loan funding provided by ASP Isotopes Inc. (“ASPI”) (prior ...

Soil erosion is a key hydro-geological hazard and a primary cause of land degradation around the world, and it is increasing due to the combined pressures ...

Erosion is a geological process in which surface materials like soil, soil parent material, and rock are worn away and transported to new locations. Carbon elements are widely found in the Earth’s ...

Abstract: The shaping of transient processes in dynamic systems, although often overlooked, constitutes a critical research concern. This paper introduces a model predictive controller that addresses ...

A series of slowly widening fissures in southern Ethiopia once again drew the attention of scientists and authorities to one of the most significant geological processes on the planet: the progressive ...

Deep beneath our feet, colossal explosions in the mantle have, at times, blasted diamonds toward the surface in violent jets that scientists now liken to “fountains.” These eruptions, triggered when ...