Page 4: Research news on magma

Magma is a high-temperature, silicate-dominated molten or partially molten substance generated within Earth’s crust and mantle by decompression melting, flux melting, or heat transfer. It consists of a continuous liquid phase containing dissolved volatiles (e.g., H₂O, CO₂, SO₂), suspended crystals, and sometimes entrained xenoliths. Its physicochemical properties—temperature, viscosity, density, and volatile content—are governed by bulk composition (mafic to felsic), pressure, and crystallinity. Magma behaves as a complex multiphase fluid, undergoing differentiation by fractional crystallization, assimilation, and mixing, and on ascent can evolve into eruptible magma that degasses and solidifies to form igneous rocks.

Matching magma dikes may have different flow patterns

Hundreds of millions of people live in areas that could be affected by volcanic eruptions. Fortunately, clues at the surface, such as earthquakes and ground deformation, can indicate movement within underground magma dikes—sheets ...

Using vibrations to see into Yellowstone's magma reservoir

Beneath Yellowstone lies a magma reservoir, pulsing with molten and superheated rock and exsolved gases. Scientists have long known about the chamber's existence, but have yet to precisely locate its uppermost boundary and ...

Kitchen experiments shed light on Mars's volcanic rootless cones

Rootless cones are small volcanic landforms ranging from several to several hundred meters in diameter, formed by continuous explosions resulting from the interaction between surface lava and water bodies like lakes and rivers. ...

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