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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. Terminology and basic principles [ edit ] Magma binds several hosts interconnected by a TCP/IP network to form a common storage space called a lava ring .

4. Sill (geology) - Wikipedia

   en.wikipedia.org/wiki/Sill_(geology)

   A sill is a concordant intrusive sheet, meaning that it does not cut across preexisting rock beds. Stacking of sills builds a sill complex [1] and a large magma chamber at high magma flux. [2] In contrast, a dike is a discordant intrusive sheet, which does cut across older rocks.

5. 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.

6. Volcanic and igneous plumbing systems - Wikipedia

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

   When magma stops ascending, the freezing of magma bodies or the arrest of magma supply lead to the formation of magma reservoirs. Magma emplacement can take place at any depth above the source rock. Magma emplacement is primarily controlled by the internal forces of magma including buoyancy and magma pressure.

7. Igneous differentiation - Wikipedia

   en.wikipedia.org/wiki/Igneous_differentiation

   Igneous differentiation. In geology, igneous differentiation, or magmatic differentiation, is an umbrella term for the various processes by which magmas undergo bulk chemical change during the partial melting process, cooling, emplacement, or eruption.

8. Magma - Wikipedia

   en.wikipedia.org/wiki/Magma

   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] Besides molten rock, magma may also contain suspended crystals and gas bubbles.