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  2. Submarine volcano - Wikipedia

    en.wikipedia.org/wiki/Submarine_volcano

    Submarine volcanoes are underwater vents or fissures in the Earth 's surface from which magma can erupt. Many submarine volcanoes are located near areas of tectonic plate formation, known as mid-ocean ridges. The volcanoes at mid-ocean ridges alone are estimated to account for 75% of the magma output on Earth. [1]

  3. 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 ...

  4. Nef (metalwork) - Wikipedia

    en.wikipedia.org/wiki/Nef_(metalwork)

    Some nefs had wheels to allow them to be rolled from one end of the table to the other, but most had legs or pedestals. The nef was placed in front of the most important person at table as a mark of their status. The equivalent in religious plate is a navicula, Latin for small ship, and also a term in English for a boat-shaped incense-holder. [3]

  5. Laccolith - Wikipedia

    en.wikipedia.org/wiki/Laccolith

    A laccolith is a type of igneous intrusion, formed when magma forces its way upwards through the Earth's crust but cools and solidifies before reaching the surface. Laccoliths are distinguished from other igneous intrusions by their dome-shaped upper surface and level base. They are assumed to be fed by a conduit from below, though this is ...

  6. 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 ...

  7. 1902 eruption of Mount Pelée - Wikipedia

    en.wikipedia.org/wiki/1902_eruption_of_Mount_Pelée

    The tsunamis swept along the coast, damaging buildings and boats. The explosions resumed the night of 5 May. The following morning, parts of the eruption plume became incandescent, signifying that the character of the eruption had changed. The phreatic eruptions had finally given way to magmatic eruptions as magma reached the surface. These ...

  8. Magmatism along strike-slip faults - Wikipedia

    en.wikipedia.org/wiki/Magmatism_along_strike...

    Strike-slip faults have a direct effect on magmatism. They can either induce magmatism, act as a conduit to magmatism and magmatic flow, or block magmatic flow. [3][4] In contrast, magmatism can also directly impact on strike-slip faults by determining fault formation, propagation and slip. [5] Both magma and strike-slip faults coexist and ...

  9. Ocean island basalt - Wikipedia

    en.wikipedia.org/wiki/Ocean_island_basalt

    Ocean island basalt (OIB) is a volcanic rock, usually basaltic in composition, erupted in oceans away from tectonic plate boundaries. Although ocean island basaltic magma is mainly erupted as basalt lava, the basaltic magma is sometimes modified by igneous differentiation to produce a range of other volcanic rock types, for example, rhyolite in ...

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