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  2. Central Atlantic magmatic province - Wikipedia

    en.wikipedia.org/wiki/Central_Atlantic_magmatic...

    Last eruption. Hettangian. The Central Atlantic magmatic province ( CAMP) is the Earth's largest continental large igneous province, covering an area of roughly 11 million km 2. It is composed mainly of basalt that formed before Pangaea broke up in the Mesozoic Era, near the end of the Triassic and the beginning of the Jurassic periods.

  3. Magmatism - Wikipedia

    en.wikipedia.org/wiki/Magmatism

    Not to be confused with Magnetism. 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. Volcanism is the surface expression of magmatism.

  4. Magmatic water - Wikipedia

    en.wikipedia.org/wiki/Magmatic_water

    Magmatic water, also known as juvenile water, is an aqueous phase in equilibrium with minerals that have been dissolved by magma deep within the Earth's crust and is released to the atmosphere during a volcanic eruption.

  5. 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] If the magma finds a path to the surface, then the result will be a volcanic eruption ...

  6. 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.

  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 .