yvlog

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olivine

[ ol-uh-veen, ol-uh-veen ]

noun

  1. Mineralogy. any of a group of magnesium iron silicates, (Mg,Fe) 2 SiO 4 , occurring in olive-green to gray-green masses as an important constituent of basic igneous rocks.


olivine

/ ˌɒlɪˈviːn; ˈɒlɪˌviːn /

noun

  1. an olive-green mineral of the olivine group, found in igneous and metamorphic rocks. The clear-green variety (peridot) is used as a gemstone. Composition: magnesium iron silicate. Formula: (MgFe) 2 SiO 4 . Crystal structure: orthorhombic Also calledchrysolite
  2. any mineral in the group having the general formula (Mg,Fe,Mn,Ca) 2 SiO 4
“Collins English Dictionary — Complete & Unabridged” 2012 Digital Edition © William Collins Sons & Co. Ltd. 1979, 1986 © HarperCollins Publishers 1998, 2000, 2003, 2005, 2006, 2007, 2009, 2012

olivine

/ ŏə-ŧ′ /

  1. An olive-green to brownish-green orthorhombic mineral. Olivine is a common mineral in the igneous rocks, such as basalt and gabbro, that make up most of the Earth's crust beneath the oceans. Chemical formula: (Mg,Fe) 2 SiO 4 .
  2. ◆ Olivine in which the mafic component consists entirely of magnesium is called forsterite . Chemical formula: Mg 2 SiO 4 .
  3. ◆ Olivine in which the mafic component consists entirely of iron is called fayalite . Chemical formula: Fe 2 SiO 4 .
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Other yvlog Forms

  • DZ··· [ol-, uh, -, vin, -ik], DZ···· [ol-, uh, -vi-, nit, -ik], adjective
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yvlog History and Origins

Origin of olivine1

1785–95; < German Olivin, equivalent to Olive olive + -in -ine 2
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yvlog History and Origins

Origin of olivine1

C18: from German, named after its colour
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Example Sentences

Examples have not been reviewed.

On Earth, basalts are a main component of the planet's crust, especially under the oceans, while olivines are abundant in its mantle.

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They are produced in a number of ways but the main process involves the interaction of ground water with iron-rich minerals such as olivine.

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One, Project Vesta, in 2022 spread an alkaline mineral called olivine on a Long Island beach to test whether that would result in more alkaline waters as waves wash the material out to sea.

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Analysis of Phaethon's infrared spectrum showed that the asteroid was composed of at least olivine, carbonates, iron sulfides, and oxide minerals.

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However, in those cases they had been more complex, magnesium-rich crystals of olivine and pyroxene.

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