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olivine

olivine

1 9.2
A green mineral in rocks formed by volcanoes that contains magnesium
  • noun
  • /ˈɑːlɪˌviːn/
  • Specialized
translation icon : olivino
  • Olivine is a common mineral found in many igneous rocks, giving them a distinct olivine color.
  • olivine crystals

Examples

  • Pallasites originate from the core-mantle boundary, where olivine crystals formed a lattice network with nickel-iron from the core.

    Academic text (2001)
  • The best pallasite samples, which are some of the most beautiful meteorite specimens, are made of 50% olivine and 50% nickel-iron.

    Academic text (2001)
  • The sand is sort of pea green, thanks to the high olivine content.

    Blog text (10)
  • It is made of glass and crystals of olivine and magnetite.

    Academic text (2001)
  • These meteorites are composed of a mixture of nickel-iron and olivine crystals.

    Academic text (2001)
  • Not as much platinum or rare earths as my piece, but some nice chunks of olivine and plenty of volatiles.

    Fiction book (2001)
  • Hike some more across not-too-onerous lava terrain to see remarkably large olivine crystals and arrive at a quiet, rocky pool (tabbies are a must, and a flotation device would probably make the experience more fun).

    Blog text (10)
  • Geologists often study olivine to understand the composition of the Earth's mantle and its volcanic activity.

  • On Mars, scientists have discovered olivine deposits that provide clues about the planet's geological history.

Surface Forms

olivine singular
olivines plural

Morphology

olivine = olive (semi-transparent) = olive + ine

The name evokes the olive (green) colour, but the specific meaning 'a magnesium-iron silicate mineral' (and the mineral-naming suffix '-ine') is specialized and not fully inferable by learners.

Etymology

The word olivine comes from the Latin oliva, 'olive', because the mineral is often olive-green in colour. So the name helps you remember it is a green mineral often found in volcanic rock and used as a source of magnesium.