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Formula | Pyrope: Mg3Al2(SiO4)3 |
Compositions can be expressed by the general formula A3B2(SiO4) A may be (Mg, Mn, Ca, Fe2+) |
Crystal System | Isometric | |
Crystal Habit | Rounded grains, massive granular (coarse or fine) | |
Hardness and Streak | H = 6.5-7.5 Streak: White |
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Cleavage | No distinct cleavage | Irregular or conchoidal fracture |
Color/Pleochroism | Pyrope: deep red to nearly black |
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Luster | Vitreous to greasy or silky | Different types of garnet may be translucent or slightly opaque, leading to variable lusters. |
Specific Gravity | G = 3.1-4.2 | Density varies depending on the type of garnet, with Ca and Mg rich garnets having lower density than the Fe and Mn garnets |
Refractive Index
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n = 1.714-1.887 | Refractive index varies depending on type of garnet |
Distinguishing Features | High relief in thin section. Color in thin section is a pale version of the hand sample color, and is often more lightly colored than spinel. | |
Occurrence | Pyrope: ultramafic igneous rocks |
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References | Nesse, W.D. (2012) “Garnet” in Introduction to Mineralogy 2nd ed. Oxford University Press, New York. p. 341-344. | |
Editors | Sarah Vorhies ('06), Kelsey Moore ('13), Emma Roth ('17) |