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Magma chambers form when molten rock, or magma, accumulates in underground reservoirs beneath the Earth's surface. This accumulation occurs as magma rises from the mantle due to pressure and temperature differences, often generated by tectonic processes such as subduction or rifting. Over time, as magma collects and cools, it may crystallize into igneous rock, but some remains in a liquid state, creating a chamber that can feed volcanic eruptions. Additionally, the presence of fractures and porous rock can facilitate the movement and storage of magma within these chambers.

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Yes. That is what the asthenosphere is.


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