The change of rock composition most responsible for the creation of magma is the addition of water.
Other mechanisms, such as melting from a meteorite impact, are less important today, but impacts during the accretion of the Earth led to extensive melting, and the outer several hundred kilometers of our early Earth was probably an ocean of magma. The molten rock, with or without suspended crystals and gas bubbles, is called magma. Volcanic rocks are named after Vulcan, the Roman name for the god of fire. The mineral grains in such rocks can generally be identified with the naked eye. Experimental studies of appropriate peridotite samples document that the solidus temperatures increase by 3 °C to 4 °C per kilometer.
Ridley, W. I., 2012, Petrology of Igneous Rocks, Volcanogenic Massive Sulfide Occurrence Model, USGS Scientific Report 2010-5070-C, Chapter 15.
Synonyms for Intrusive Rock in Free Thesaurus.
These are the elements that combine to form the silicate minerals, which account for over ninety percent of all igneous rocks.
There, it is variously attributed either to the rise of mantle plumes (the "Plume hypothesis") or to intraplate extension (the "Plate hypothesis").[11]. If crystals separate from the melt, then the residual melt will differ in composition from the parent magma. When magma reaches the surface from beneath water or air, it is called lava.
Igneous rocks are classified according to mode of occurrence, texture, mineralogy, chemical composition, and the geometry of the igneous body. The chemistry of igneous rocks is expressed differently for major and minor elements and for trace elements.
Fine volcanic ash is also erupted and forms ash tuff deposits, which can often cover vast areas. Decompression melting occurs because of a decrease in pressure.[10].
Igneous rocks are classified on the basis of texture and composition. This information should not be considered complete, up to date, and is not intended to be used in place of a visit, consultation, or advice of a legal, medical, or any other professional. In rare cases, melts can separate into two immiscible melts of contrasting compositions. Such magmas, and those derived from them, build up island arcs such as those in the Pacific Ring of Fire. Volcanoes with rhyolitic magma commonly erupt explosively, and rhyolitic lava flows are typically of limited extent and have steep margins because the magma is so viscous. For example, at a depth of about 100 kilometers, peridotite begins to melt near 800 °C in the presence of excess water, but near or above about 1,500 °C in the absence of water.
Two important variables used for the classification of igneous rocks are particle size, which largely depends on the cooling history, and the mineral composition of the rock. Igneous and metamorphic rocks make up 90–95% of the top 16 km of the Earth's crust by volume. Kanaga volcano in the Aleutian Islands with a 1906 lava flow in the foreground, A "skylight" hole, about 6 m (20 ft) across, in a solidified lava crust reveals molten lava below (flowing towards the top right) in an eruption of Kīlauea in Hawaii, Devils Tower, an eroded laccolith in the Black Hills of Wyoming, A cascade of molten lava flowing into Aloi Crater during the 1969-1971 Mauna Ulu eruption of Kilauea volcano, Columnar jointing in the Alcantara Gorge, Sicily, A laccolith of granite (light-colored) that was intruded into older sedimentary rocks (dark-colored) at Cuernos del Paine, Torres del Paine National Park, Chile, An igneous intrusion cut by a pegmatite dike, which in turn is cut by a dolerite dike. Explosively erupted pyroclastic material is called tephra and includes tuff, agglomerate and ignimbrite.
Mineralogical classification is most often used to classify plutonic rocks.
Basalt is a common extrusive igneous rock and forms lava flows, lava sheets and lava plateaus. Generally speaking, phaneritic implies an intrusive origin; aphanitic an extrusive one. The most important criterion is the phenocryst species, followed by the groundmass mineralogy. The magma, which is brought to the surface through fissures or volcanic eruptions, solidifies at a faster rate.
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