Giant regions of the mantle where seismic waves slow down may have formed from subducted ocean crust, a new study finds.

Giant regions of the mantle where seismic waves slow down may have formed from subducted ocean crust, a new study finds.

Yellowstone and Hawaiʻi. These systems a well known for producing large volumes of magma through time and leaving chains of volcanic features in their wake, although they do so in very different ways.

The ground beneath your feet may feel solid, but Earth is constantly shifting. While we have mapped the surface in detail, ...

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The main place to find these types of volcanoes is the ... occur in the middle of continents. Hot mantle plumes sit in one place for long periods of time while the crust slowly creeps over ...

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“I was able to find out a lot more ... under both her own name and the nom de plume Zhemyna Jurate. Her reporting beats include Gardiner and Rosendale, the arts and a bit of local history. In 2011 she ...

A breakthrough study has provided the most detailed 3D look yet at the inner workings of the Tonga Subduction Zone, where ...

High-Resolution Anisotropic Tomography Reveals Mantle Flow Complexity and Slab-Plume Interactions, Redefining Subduction Zone ...

Conducted by researchers from Ocean University of China and Tohoku University, Japan, the work combines innovative seismic methodologies to map mantle flow patterns, slab-plume interactions ...

Continent-size islands deep inside Earth's mantle could be more than a billion years old, a new study finds. Known as large low-seismic-velocity provinces (LLSVPs), these blobs are both hotter and ...