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  2. Felsic - Wikipedia

    en.wikipedia.org/wiki/Felsic

    Felsic refers to silicate minerals, magma, and rocks which are enriched in the lighter elements such as silicon, oxygen, aluminium, sodium, and potassium. Felsic magma or lava is higher in viscosity than mafic magma/lava, and have low temperatures to keep the felsic minerals molten. Felsic rocks are usually light in color and have specific ...

  3. Magma - Wikipedia

    en.wikipedia.org/wiki/Magma

    Magma can be found in the mantle or molten crust. Magma ... Felsic or silicic magmas have a silica content greater than 63%. They include rhyolite and dacite magmas.

  4. Igneous intrusion - Wikipedia

    en.wikipedia.org/wiki/Igneous_intrusion

    In geology, an igneous intrusion (or intrusive body[1] or simply intrusion[2]) is a body of intrusive igneous rock that forms by crystallization of magma slowly cooling below the surface of the Earth. Intrusions have a wide variety of forms and compositions, illustrated by examples like the Palisades Sill of New York and New Jersey; [3] the ...

  5. Silicic - Wikipedia

    en.wikipedia.org/wiki/Silicic

    Silicic is an adjective to describe magma or igneous rock rich in silica. The amount of silica that constitutes a silicic rock is usually defined as at least 63 percent. [ 1] Granite and rhyolite are the most common silicic rocks . Silicic is the group of silicate magmas which will eventually crystallise a relatively small proportion of ...

  6. Lava - Wikipedia

    en.wikipedia.org/wiki/Lava

    Lava domes are formed by the extrusion of viscous felsic magma. They can form prominent rounded protuberances, such as at Valles Caldera. As a volcano extrudes silicic lava, it can form an inflation dome or endogenous dome, gradually building up a large, pillow-like structure which cracks, fissures, and may release cooled chunks of rock and rubble.

  7. Large igneous province - Wikipedia

    en.wikipedia.org/wiki/Large_igneous_province

    A large igneous province (LIP) is an extremely large accumulation of igneous rocks, including intrusive (sills, dikes) and extrusive (lava flows, tephra deposits), arising when magma travels through the crust towards the surface. The formation of LIPs is variously attributed to mantle plumes or to processes associated with divergent plate ...

  8. Effusive eruption - Wikipedia

    en.wikipedia.org/wiki/Effusive_eruption

    Effusive eruptions are most common in basaltic magmas, but they also occur in intermediate and felsic magmas. These eruptions form lava flows and lava domes, each of which vary in shape, length, and width. [2] Deep in the crust, gasses are dissolved into the magma because of high pressures, but upon ascent and eruption, pressure drops rapidly ...

  9. Ancient ocean of magma found on Moon south pole

    www.aol.com/ancient-ocean-magma-found-moon...

    August 21, 2024 at 11:31 AM. India's lunar mission found remnants of a magma ocean on the south pole [ISRO] The Moon’s south pole was once covered in an ocean of liquid molten rock, according to ...