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- 20" Bait/Fillet Mate™ ...WestMarine$169.99
- 31" Bait/Fillet Mate™ ...WestMarine$209.99
- Magma Rectangle Party ...MyGreenOutdoors$359.99
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- Magma Products, T10-313B...Amazon.com$199.99
- Magma Bait/Filet Mate ...CampSaver.com$209.99
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- Magma Econo Mate Bait ...CampSaver.com$89.99
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- Magma Bait/Filet Mate ...Kesper Supply$129.99
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- Magma White/Black...The Twister Group$209.99
- Magma White/Black...The Twister Group$129.99
- Magma 16" X 20" White...eBay.com$148.99
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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.
A magma is a set M matched with an operation • that sends any two elements a, b ∈ M to another element, a • b ∈ M. The symbol • is a general placeholder for a properly defined operation. To qualify as a magma, the set and operation (M, •) must satisfy the following requirement (known as the magma or closure axiom):
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.
Magma is a computer algebra system designed to solve problems in algebra, number theory, geometry and combinatorics. It is named after the algebraic structure magma. It runs on Unix-like operating systems, as well as Windows .
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 .
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.