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What (who) is gabbro - definition
![[[Photomicrograph]] of a [[thin section]] of gabbro](https://commons.wikimedia.org/wiki/Special:FilePath/Gabbro pmg ss 2006.jpg?width=200 "[[Photomicrograph]] of a [[thin section]] of gabbro")
![A gabbro landscape – the main ridge of the [[Cuillin]], [[Isle of Skye]], [[Scotland]]](https://commons.wikimedia.org/wiki/Special:FilePath/Main ridge of the cuillin in skye arp.jpg?width=200 "A gabbro landscape – the main ridge of the [[Cuillin]], [[Isle of Skye]], [[Scotland]]")
![[[Zuma Rock]], Nigeria, a massive, nearly uniform, intrusion of gabbro and [[granodiorite]].](https://commons.wikimedia.org/wiki/Special:FilePath/Zuma rock.jpg?width=200 "[[Zuma Rock]], Nigeria, a massive, nearly uniform, intrusion of gabbro and [[granodiorite]].")
Wikipedia
Gabbro () is a phaneritic (coarse-grained), mafic intrusive igneous rock formed from the slow cooling of magnesium-rich and iron-rich magma into a holocrystalline mass deep beneath the Earth's surface. Slow-cooling, coarse-grained gabbro is chemically equivalent to rapid-cooling, fine-grained basalt. Much of the Earth's oceanic crust is made of gabbro, formed at mid-ocean ridges. Gabbro is also found as plutons associated with continental volcanism. Due to its variant nature, the term gabbro may be applied loosely to a wide range of intrusive rocks, many of which are merely "gabbroic". By rough analogy, gabbro is to basalt as granite is to rhyolite.
