Cubic
The cube is composed of 6 square faces at 90 degree angles to each other. Each face intersects one of the crystallographic axes and is parallel to the other two.
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Diamond
Garnet
Rhodolite
Spinel
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Tetragonal
The tetragonal system also has three axes that all meet at 90°. It differs from the isometric system in that the C axis is longer than the A and B axis which are the same length.
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Zircon |
Hexagonal
In the hexagonal system we have an additional axes, which gives the crystals six sides. Three of these are equal in length and meet at 60° to each other. The C or vertical axis is at 90° to the shorter axes.
Mineralogists sometimes divide this into two systems, the hexagonal and the trigonal, based on their external appearance, as follows:
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Trigonal
Again, the trigonal system is a subsystem of the hexagonal. Most gem references will list these as hexagonal.
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Amethyst
Citrine
Corundum
Ruby
Sapphire
Tourmaline
Eudialyte
Quartz
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Orthorhombic
In this system there are three axes, all of which meet at 90° to each other. However, all the axes are a different length.
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Monoclinic
. The above crystal systems all have axes sides that meet at 90°. In the monoclinic system all the axes are different lengths. Two of them, the A and C axes, meet at 90°, but the third one does not.
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Triclinic
In this system all the axes are different lengths and none of them meet at 90°.
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Turquoise |