Crystals Can Grow
Virtual Geology Museum
Hall of Minerals
Geology Home Page
Roger Weller,
geology instructor ( wellerr@cochise.edu
)
last edited: 10/6/10
copyright 2010-R.Weller
Part 2-Crystal Systems
List of Topics
for Potato Crystallography Part 2:
Preparation and
Materials
The Six Crystal Systems
Isometric System
Tetragonal System
Orthorhombic System
Monoclinic System
Triclinic System
Hexagonal/Trigonal System
Preparation
and Materials
Materials needed: Several large potatoes, a large sharp knife, a small paring
knife,
and a bunch of round toothpicks.

It is much easier to demonstrate crystal shapes if you start with big potatoes
(Russet). Peel several potatoes and cut the largest cubes that you can
from each
potato. You will probably need at least twelve cubes. Try
to be as accurate as
possible to make perfect cubes, all the sides of equal
length and at right angles.
It might take a little practice.

The Six Crystal
Systems
Naturally occurring crystals have studied
for over two hundred years and all of
the shapes can be sorted out and placed
into 6 families (or systems) of symmetry.
Five of the systems of symmetry can be each defined by the orientation of 3
imaginary lines called axes that describe the type of symmetry along each axis;
the sixth system (#8 in the figure below) requires four axes.

Isometric System
The Isometric system is best described by a simple cube.

cut potato showing
basic form of the Isometric system
This system is described by 3 axes oriented at right angles to the other two.
Each of these axes has four-fold symmetry and has the same length. The best
example is a cube.
A toothpick stuck into the middle of any cube face will act as
an axis and will
show show four-fold symmetry. This system has the greatest
amount of
symmetry of the six crystal systems.

cut potato model with
toothpicks representing crystallographic axes

wooden model of cube
Tetragonal system
Take a potato cube and cut in half. The
resulting shape has a square top and
short sides.
potato-flattened Tetragonal form
The
tetragonal basic form can also be elongated in one direction

cut potato illustrating elongated central
axis

comparison between a cube (Isometric) and an elongated Tetragonal form
A toothpick stuck in the middle of the square face and then rotated shows that
this is an axis of four-fold symmetry. A toothpick inserted into the
middle of any
of the short sides will only be an axis of two-fold symmetry.
The Tetragonal
System is defined by three axes at right angles to each other;
one axis has
four-fold symmetry and the other two axes only have two-fold
symmetry. The two
axes of two-fold symmetry have the same length, while
the four-fold axis is either
longer or shorter than the other two.

cut potato with
elongated central axis

wooden model of simple
tetragonal form
Orthorhombic System
Take the leftover half of the potato cube that you created when you made to
Tetragonal form and cut off a small sliver parallel to one of the small faces.
You
should have a rectangular blow where the length, width, and height are all
different.

cut potato model of basic
orthorhombic form
A toothpick stuck in the middle of any one of the 6 faces will
turn out to be an
axis of two-fold symmetry. The Orthorhombic System is
defined by three axes at
right angles to each other and each axis only has
two-fold symmetry. All three
axes are of unequal length. The simplest Orthorhombic crystal is similar to
the
shape of a
breakfast cereal box.

cut potato model showing
relationship of Orthorhombic crystallographic axes

wooden model of basic
Orthorhombic shape
Monoclinic System
Cutting the potato is now going to become more difficult. First cut the
potato
into an Orthorhombic shape, a box-like shape where the length, width, and
height
are all different. Follow the diagram below and cut an inclined
slice off two
opposing sides so that the final form looks like a box leaning
over in one direction.

cut potato model of basic
Monoclinic shape

wooden model of basic
Monoclinic shape
The leaning in one direction is where this crystal gets its name. "Mono" means
one and "cline" means to lean. The Monoclinic System is defined by three
axes of
unequal length and where two axes are at right angles to each other and
the third
is at an angle other than 90 degrees.
cut potato model showing
relationship of Monoclinic crystallographic axes
Triclinic System
Cut another potato into a monoclinic shape of
a box leaning in one direction.
Following the diagram below, cut inclined
slices off two opposing sides that
were at right angles to the box. You
should now now have a shape that looks
like a box leaning in two directions.

cut potato model of basic
Triclinic shape

wooden model of basic
Triclinic shape
Even though the box looks like it is leaning in two directions, the name for
this
type of symmetry is Triclinic. The reasoning behind this name is that
the Triclinic
system is described by three axes of unequal length where none of
the axes makes
a right angle with the other two. In other words, all three
axes are leaning in some
direction.

Tricinic axes
Copper sulfate produces
Triclinic crystals.
Hexagonal/Trigonal System
For this crystal system, do not start out by
making a cube. The simplest way of
describing the shape you need to create
is a hexagonal column. Carefully study
the diagram below. The six
sides should be parallel to each other and of equal
length. The top and
bottom of the column should be flat.

cut potato model showing
basic Hexagonal shape

wooden model of basic
Hexagonal shape
The axes that describe the Hexagonal system
consist of one axis with six-fold
symmetry at right angles to the axes of equal
length oriented at 60 degree angles
to their neighboring axes.
In the Trigonal System the main axis has three-fold
symmetry instead of six-fold
symmetry. Some crystallographers treat the Trigonal
System as a separate
system, while others consider it a sub-category of the
Hexagonal System.

cut potato showing Hexagonal
crystallographic axes