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نارى بركانى - ترجمة إلى إنجليزي
نارى بركانى
igneous (ADJ)
igneous
![Natural columns of igneous rock separated from each other by [[columnar joint]]s, in [[Madeira]]](https://commons.wikimedia.org/wiki/Special:FilePath/BasaltColumns PortoSanto.JPG?width=200 "Natural columns of igneous rock separated from each other by [[columnar joint]]s, in [[Madeira]]")
![Sample of basalt (an extrusive igneous rock), found in [[Massachusetts]]](https://commons.wikimedia.org/wiki/Special:FilePath/Basalt 36mw1041.jpg?width=200 "Sample of basalt (an extrusive igneous rock), found in [[Massachusetts]]")
![fractional crystallisation]] in a [[magma]]. While cooling, the magma evolves in composition because different minerals crystallize from the melt. '''1''': [[olivine]] crystallizes; '''2''': olivine and [[pyroxene]] crystallize; '''3''': pyroxene and [[plagioclase]] crystallize; '''4''': plagioclase crystallizes. At the bottom of the magma reservoir, a [[cumulate rock]] forms.](https://commons.wikimedia.org/wiki/Special:FilePath/Fractional crystallization.svg?width=200 "fractional crystallisation]] in a [[magma]]. While cooling, the magma evolves in composition because different minerals crystallize from the melt. '''1''': [[olivine]] crystallizes; '''2''': olivine and [[pyroxene]] crystallize; '''3''': pyroxene and [[plagioclase]] crystallize; '''4''': plagioclase crystallizes. At the bottom of the magma reservoir, a [[cumulate rock]] forms.")
![[[Gabbro]] specimen showing [[phaneritic]] texture, from Rock Creek Canyon, eastern [[Sierra Nevada]], California](https://commons.wikimedia.org/wiki/Special:FilePath/GabbroRockCreek1.jpg?width=200 "[[Gabbro]] specimen showing [[phaneritic]] texture, from Rock Creek Canyon, eastern [[Sierra Nevada]], California")
![Close-up of granite (an intrusive igneous rock) exposed in [[Chennai]], India](https://commons.wikimedia.org/wiki/Special:FilePath/IndianGranite.jpg?width=200 "Close-up of granite (an intrusive igneous rock) exposed in [[Chennai]], India")
![[[Lopolith]]
}}](https://commons.wikimedia.org/wiki/Special:FilePath/Intrusion types.svg?width=200 "[[Lopolith]]
}}")
![[[Volcanic eruptions]] of lava are major sources of igneous rocks. ([[Mayon]] volcano in the Philippines, erupting in 2009)](https://commons.wikimedia.org/wiki/Special:FilePath/Mayon 0021.jpg?width=200 "[[Volcanic eruptions]] of lava are major sources of igneous rocks. ([[Mayon]] volcano in the Philippines, erupting in 2009)")
![Kanaga]] volcano in the [[Aleutian Islands]] with a 1906 lava flow in the foreground](https://commons.wikimedia.org/wiki/Special:FilePath/Kanaga Volcano (22432739869).jpg?width=200 "Kanaga]] volcano in the [[Aleutian Islands]] with a 1906 lava flow in the foreground")
![m}} across, in a solidified lava crust reveals molten lava below (flowing towards the top right) in an eruption of [[Kīlauea]] in Hawaii](https://commons.wikimedia.org/wiki/Special:FilePath/Molten Lava in Pahoehoe Skylight.jpg?width=200 "m}} 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](https://commons.wikimedia.org/wiki/Special:FilePath/"This means something. This is important" (19967592275).jpg?width=200 "[[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](https://commons.wikimedia.org/wiki/Special:FilePath/Happy Anniversary Hawaii (14802198589).jpg?width=200 "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]]](https://commons.wikimedia.org/wiki/Special:FilePath/Columnar jointing in the Alcantara Gorge, Sicily.jpg?width=200 "[[Columnar jointing]] in the Alcantara Gorge, [[Sicily]]")
![A laccolith of granite (light-coloured) that was intruded into older sedimentary rocks (dark-coloured) at Cuernos del Paine, [[Torres del Paine National Park]], Chile](https://commons.wikimedia.org/wiki/Special:FilePath/Cretaceous sedimentary rocks intruded by a Miocene granite laccolith.jpg?width=200 "A laccolith of granite (light-coloured) that was intruded into older sedimentary rocks (dark-coloured) 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](https://commons.wikimedia.org/wiki/Special:FilePath/Multiple Igneous Intrusion Phases Kosterhavet Sweden.jpg?width=200 "An igneous intrusion cut by a [[pegmatite]] dike, which in turn is cut by a [[dolerite]] dike")
ONE OF THE THREE MAIN ROCK TYPES; FORMED THROUGH THE COOLING AND SOLIDIFICATION OF MAGMA OR LAVA
Igneous rocks; Igneous Rock; Magmatic rock; Igneous Rocks; Magmatic rocks; Igneous; Igneus rock; Instrusive Rock; Igneous deposition; Decompression melting; Igneous body; Igneous mineral
ADJ
نارى بركانى
نارى بركانى
