Peridot is primarily found in Arizona, United States. Other sources of peridot include Hawaii and New Mexico.
Peridot is not commonly found in California. The only known source of peridot in the United States is the San Carlos Apache Reservation in Arizona.
The Mantle
Yes.
Peridot is commonly found in countries such as the United States (Arizona and Hawaii), Pakistan, Myanmar, China, and Vietnam. It can also be found in some African countries like Egypt and Tanzania.
Peridot (or pridot) is found in many places all over the world.
Peridot is composed of the mineral olivine, which is formed from the mineral group of silicates. It gets its characteristic green color from the presence of iron. Peridot is usually found in volcanic rocks such as basalt and peridotite.
Peridot is typically found in igneous rocks, specifically in basaltic lava flows and in some metamorphic rocks. It is formed in the Earth's mantle and brought to the surface through volcanic activity.
Peridot is found in North Carolina, Arizona, Hawaii, Nevada, New Mexico, Australia, Brazil, China, Kenya, Mexico, Myanmar, Norway, Pakistan, Saudi Arabia, South Africa, Sri Lanka and Tanzania.
Peridot is olivine, which is a mineral, not a rock. It is found in both intrusive and extrusive rocks.
Peridot is formed deep within the Earth's mantle under high pressure and temperature conditions. It is created through volcanic activity, where it is brought to the surface through magma and can be found in volcanic rock such as basalt. Peridot can also be found in meteorites from outer space.
Peridot is typically found in small to medium sizes, with most gem-quality stones ranging from 1 to 10 carats. Larger sizes can be rare and more valuable. It's important to note that peridot can also be found in smaller sizes for jewelry like earrings and pendants.