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  2. Magmatism - Wikipedia

    en.wikipedia.org/wiki/Magmatism

    Magmatism. Geological map showing the Gangdese batholith, which is a product of magmatic activity about 100 million years ago. 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 ...

  3. Üdü Ẁüdü - Wikipedia

    en.wikipedia.org/wiki/Üdü_Ẁüdü

    Review scores. Source. Rating. Allmusic. [2] Üdü Ẁüdü is the sixth studio album by French rock band Magma, released on 10 September 1976. This album was first issued with a provisional sleeve, as Klaus Blasquiz's artwork was not finished on time. This art features in all later issues.

  4. Live/Hhaï - Wikipedia

    en.wikipedia.org/wiki/Live/Hhaï

    Live/Hhaï (also known as Magma Live, Live Köhntark, and Hhaï Live) is the first live album and fifth album in total by French rock group Magma. It was recorded in Paris between the 1st and 5 June 1975 at the Taverne de l'Olympia, [2] and was first released in 1975. The album has been re-released many times: in 1975 on Utopia Records, in 1978 ...

  5. 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 . Location of the concert Olympia music hall Paris (Photo 2009)

  6. Mantle plume - Wikipedia

    en.wikipedia.org/wiki/Mantle_plume

    Mantle plume. A superplume generated by cooling processes in the mantle (LVZ = low-velocity zone) [1] A mantle plume is a proposed mechanism of convection within the Earth's mantle, hypothesized to explain anomalous volcanism. [2] Because the plume head partially melts on reaching shallow depths, a plume is often invoked as the cause of ...

  7. Magma chamber - Wikipedia

    en.wikipedia.org/wiki/Magma_chamber

    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 ...

  8. Sill (geology) - Wikipedia

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

    Sill (geology) Illustration showing the difference between a dike and a sill. In geology, a sill is a tabular sheet intrusion that has intruded between older layers of sedimentary rock, beds of volcanic lava or tuff, or along the direction of foliation in metamorphic rock. A sill is a concordant intrusive sheet, meaning that it does not cut ...

  9. Pluton emplacement - Wikipedia

    en.wikipedia.org/wiki/Pluton_emplacement

    Pluton emplacement. The methods of pluton emplacement are the ways magma is accommodated in a host rock where the final result is a pluton. The methods of pluton emplacement are not yet fully understood, but there are many different proposed pluton emplacement mechanisms. Stoping, diapirism and ballooning are the widely accepted mechanisms.

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