Epidote
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Ca2(Al,Fe)3(SiO4)(Si2O7)O(OH)
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Distinguished by a distinctive pistachio-green color, epidote is a monoclinic sorosilicate with the formula Ca2(Al,Fe)3(SiO4)(Si2O7)O(OH). It forms during metamorphism and hydrothermal alteration across a wide range of rock types and is an important constituent of greenstone belts. The mineral is translucent with a vitreous luster, a gray streak, and perfect {001} cleavage, occurring as prismatic, columnar, or fibrous crystals. Its Mohs hardness is 6 to 7 and its specific gravity 3.25 to 3.50. Well-formed epidote crystals are collected as specimens, and the mineral's characteristic yellow-green hue makes it readily identifiable in the field. A specific gravity of 3.25 to 3.50 and a prismatic to fibrous habit round out its diagnostic profile.
Epidote is a common metamorphic and hydrothermal mineral recognizable by its distinctive pistachio-green color. It forms in a wide range of rock types during metamorphism and is an important constituent of greenstone belts.
| النظام البلوري | Monoclinic |
| صنف المعدن | 09 Silicates |
| صلادة موس | 6.0-7.0 |
| الكثافة النوعية | 3.25-3.50 |
| اللون | Pistachio green, yellowish-green, dark green |
| اللمعان | Vitreous |
| لون الخط | Gray |
| الانفصام | Perfect {001} |
| الكسر | Uneven |
| الشفافية | Translucent |
| الشكل البلوري | Prismatic, columnar, fibrous |
صلادة موس
| صلادة موس | Reference Mineral |
|---|---|
| 1 | Talc |
| 2 | Gypsum |
| 3 | Calcite |
| 4 | Fluorite |
| 5 | Apatite |
| 6 | Orthoclase |
| 7 | Quartz |
| 8 | Topaz |
| 9 | Corundum |
| 10 | Diamond |
النظام البلوري
| الخاصية | Value |
|---|---|
| النظام البلوري | Monoclinic |
| Axial Relationships | a ≠ b ≠ c, α = γ = 90°, β ≠ 90° |