Difference between revisions of "Crystal Systems"

Crystal Systems & Forms

Crystal System Diagram Examples
Cubic

The cube is composed of 6 square faces
at 90° angles to each other. Each
face intersects one of the crystallographic
axes and is parallel to the other two.

Diamond
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
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.

Zircon
Hexagonal

In the hexagonal system, we have an additional axis,
giving 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:

Aquamarine
Trigonal

Again, the trigonal system is a subsystem of the
hexagonal. Most gem references will list these as
hexagonal.

Amethyst
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.

Alexandrite
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.

Azurite
Triclinic

In this system all the axes are different
lengths and none of them meet at 90°.

Turquoise