A natural Epidote crystal specimen displaying multiple well-developed prismatic crystals forming a compact cluster. The crystals exhibit the typical elongated prism habit of epidote and a deep green to almost black coloration. Several crystal faces are visible with natural luster, giving the specimen a strong mineralogical character. The cluster shows good natural crystal growth and structural texture, making it an attractive piece for mineral collectors and display. Epidote is a calcium aluminum iron sorosilicate mineral often formed in metamorphic and hydrothermal environments. This specimen highlights the mineral's classic crystal structure and natural geological formation. Photos were taken under controlled lighting; slight color variation may occur due to light reflection.