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Where is Olivine found?

(Mg,Fe)2SiO4

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Olivine occurs in specific geological environments. Knowing where to look, and in what kind of rock, is the difference between going home empty-handed and finding a great specimen.

Where to find Olivine

San Carlos Apache Reservation, Arizona, USA

World-renowned locality for gem-quality peridot (olivine) found in basaltic lava flows and volcanic bombs.

Zabargad Island (St. John's Island), Red Sea, Egypt

Historical source of large, fine-quality peridot crystals, often found in peridotite xenoliths within basalt.

Kilauea Volcano, Hawaii, USA

Olivine is a common phenocryst in Hawaiian basalts, and small crystals can be found in volcanic sands (e.g., Papakolea Green Sand Beach).

Norway

Significant industrial deposits of olivine, particularly for refractory uses, found in large dunite bodies.

Pakistan

Produces high-quality peridot, often from peridotite xenoliths in volcanic rocks.

Collecting tips

  1. Look in Volcanic Rocks. Search for olivine in basaltic lava flows, volcanic bombs, and tuffs, especially in areas with recent volcanic activity. It often appears as small, green, glassy grains.
  2. Examine Ultramafic Intrusions. Explore outcrops of peridotite, dunite, and gabbro. Olivine is a primary constituent of these rocks and can form large, granular masses.
  3. Check for Mantle Xenoliths. In some volcanic areas, look for xenoliths (rock fragments) of mantle material brought to the surface by magma. These often contain abundant olivine.
  4. Observe Color and Luster. The characteristic olive-green color and vitreous to greasy luster are key identifiers. Fresh surfaces are best for observation.
  5. Consider Associated Minerals. Olivine is commonly found with pyroxenes (augite), plagioclase feldspar, and magnetite in mafic rocks. In ultramafic rocks, it may be associated with chromite and serpentine.

Quick Check

Color:
Olive-green to yellowish-green
Luster:
Vitreous to greasy
Streak:
White

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