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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. 1001° Centigrades - Wikipedia

    en.wikipedia.org/wiki/1001°_Centigrades

    1001° Centigrades, alternative title 2, is the second album by French rock band Magma, released on 5 October 1971. Future reissues use both titles as 2: 1001° Centigrades . The first track, "Rïah Sahïltaahk", was later re-recorded as a full-length studio album, Rïah Sahïltaahk, in 2014, as Christian Vander did not consider himself ...

  5. Ëmëhntëhtt-Ré - Wikipedia

    en.wikipedia.org/wiki/Ëmëhntëhtt-Ré

    Ëmëhntëhtt-Ré is the tenth studio album by French progressive rock band Magma. It was released on 20 October 2009. [2] Parts of it have been played live since 1975 and can be found on various albums as extracts or live versions. Included with the CD is a making-of DVD called "Phases". [3]

  6. There was once an ancient ocean filled with magma on the moon ...

    www.aol.com/once-ancient-ocean-filled-magma...

    There was once a magma-filled ocean on the south pole of the moon, scientists recently discovered after analyzing lunar soil that revealed ancient information about the moon's origin. The study of ...

  7. 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 ...

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