Research news on mantle plume

A mantle plume is a buoyant, localized upwelling of anomalously hot, partially molten or near-solid-state mantle material that rises from depth toward the lithosphere, driven primarily by thermal and compositional density contrasts. In geodynamic models, mantle plumes are often represented as narrow, cylindrical conduits with bulbous heads, capable of producing large magma volumes upon decompression melting in the upper mantle. They are invoked to explain intraplate magmatism, flood basalt provinces, and hotspot volcanism, and are studied through seismic tomography, geochemical tracers (e.g., isotopic signatures), and numerical or analogue convection experiments that constrain their temperature excess, geometry, and temporal evolution.

Study reveals Hawaiian hotspot is getting hotter

Contrary to conventional geological thinking, the Hawaiian mantle plume has gotten hotter by about 250°C (480°F) over the past 47 million years. This discovery, led by Earth scientists at the University of Hawai'i at Mānoa, ...

Expedition to Hess Rise in the Northwest Pacific begins

Located in the middle of the North Pacific, between Japan and Canada, lies one of the world's largest oceanic plateaus, the so-called Hess Rise. The plateau is roughly T-shaped and extends over a length of about 1,000 kilometers. ...

Bizarre Venus surface formations puzzle planetary scientists

Bizarre Venus surface formations (or coronae) are likely key to understanding our twin planet's heretofore inscrutable interior. Using NASA Magellan spacecraft data from decades past, Anna Gulcher, an Earth and planetary ...

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