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3. MagmaFS - Wikipedia

   en.wikipedia.org/wiki/MagmaFS

   Magma is a distributed file system based on a distributed hash table, written in C, compatible with Linux and BSD kernels using FUSE .

4. Magma - Wikipedia

   en.wikipedia.org/wiki/Magma

   Magma (from Ancient Greek μάγμα (mágma) 'thick unguent ') [1] is the molten or semi-molten natural material from which all igneous rocks are formed. [2] Magma (sometimes colloquially but incorrectly referred to as lava by laypeople) is found beneath the surface of the Earth, and evidence of magmatism has also been discovered on other terrestrial planets and some natural satellites. [3 ...

5. Magma supply rate - Wikipedia

   en.wikipedia.org/wiki/Magma_supply_rate

   The magma supply rate measures the production rate of magma at a volcano. Global magma production rates on Earth are about 20–25 cubic kilometres per year (4.8–6.0 cu mi/a).

6. Volcanic and igneous plumbing systems - Wikipedia

   en.wikipedia.org/wiki/Volcanic_and_igneous...

   Volcanic and igneous plumbing systems. Schematic sketch of the volcanic and igneous plumbing systems (after Burchardt, 2018). [1] [2] Volcanic and igneous plumbing systems (VIPS) consist of interconnected magma channels and chambers through which magma flows and is stored within Earth's crust. [1] Volcanic plumbing systems can be found in all ...

7. Tholeiitic magma series - Wikipedia

   en.wikipedia.org/wiki/Tholeiitic_Magma_Series

   A magma series is a chemically distinct range of magma compositions that describes the evolution of a mafic magma into a more evolved, silica rich end member. Rock types of the tholeiitic magma series include tholeiitic basalt, ferro-basalt, tholeiitic basaltic andesite, tholeiitic andesite, dacite and rhyolite.

8. Magma chamber - Wikipedia

   en.wikipedia.org/wiki/Magma_chamber

   A magma chamber is a large pool of liquid rock beneath the surface of the Earth. The molten rock, or magma, in such a chamber is less dense than the surrounding country rock, which produces buoyant forces on the magma that tend to drive it upwards. [1]