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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. 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.

5. Magmatism - Wikipedia

   en.wikipedia.org/wiki/Magmatism

   Magmatism is the emplacement of magma within and at the surface of the outer layers of a terrestrial planet, which solidifies as igneous rocks. It does so through magmatic activity or igneous activity , the production, intrusion and extrusion of magma or lava .

6. 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.

7. Retrospektïẁ (Parts I+II) - Wikipedia

   en.wikipedia.org/wiki/Retrospektïẁ_(Parts_I+II)

   Retrospektïẁ (Parts I+II) is a live album by French rock band Magma. Released in 1981, it documents live recordings from a series of Magma reunion shows in Paris on 9, 10 and 11 June 1980. It was originally released on RCA, and has been re-released on Seventh Records .

8. 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.