How do I identify Eclogite?

Eclogite can be identified by its Brown color. Look for these key characteristics when examining specimens.

What color is Eclogite?

Eclogite typically appears in Brown, green, red, pink, black, gray, etc.. Color can vary depending on impurities and formation conditions.

Eclogite

A variety of Metamorphic

Rare

What is Eclogite?

Eclogite is a dense metamorphic rock that is formed at tremendous pressures and depths. The rock often sports a striking mix of colors, with green and pink being the predominant hues (caused by the minerals garnet and omphacite, respectively). This coloration can make eclogite attractive for decorative uses. Because it forms at such great depths, it is of even greater use to geologists, who study it to learn about certain aspects of plate tectonics.

Uses & Applications

Eclogite is commonly bright red and green, which make it a popular rock option in construction, particularly for countertops and other decorative elements. Unsurprisingly, it is a popular choice for jewelry, especially because eclogite often contains large garnets. It has also been used in cosmetics.

Healing Properties

Eclogite is believed to support spiritual growth, clearing the heart and solar plexus chakras. It is said to balance the emotions, relieving the user from negative feelings of guilt, fear and anger and replacing these with positive energy. Some say meditating with this stone will help to increase self-esteem and restore confidence and motivation.

Eclogite Market Value Calculator

Estimate the market value of Eclogite using size, quality, and finish. This preview calculator is for quick context and is not a formal appraisal.

Eclogite Localities Map

See where Eclogite is found with a localities map, collecting zones, and geology context. Generate a sample map preview below.

Map preview

North ZoneCentral RidgeSouth Basin

Associated Chakras

Solar Plexus

Key Characteristics

Formation of Eclogite

Eclogite typically result from high to ultrahigh pressure metamorphism of mafic rocks at low thermal gradients of <10 ℃/km as they were subducted to the lower crust to upper mantle depths in a subduction zone. They are generally formed from precursor mineral assemblages typical of blueschist-facies metamorphism.