Epidote

Epidote is a mineral with a characteristic color ranging from yellowish-green to dark green, often found in the form of elongated crystals or granular masses. Epidote is composed of calcium, aluminum, and iron silicate, noted for its significant double refraction. Its main deposits are found in Austria, Pakistan, and the United States. It was first discovered in the early 19th century. The often brilliant appearance and crystalline structure of epidote make it a popular choice for mineral collections and decorative objects.

This stone is sold individually and measures approximately 3 cm.