2)
The
Tetragonal System
-
The crystals in this
system are referred to by 3 crystallographic axes which are perpendicular (90o)
to each other.
-
The two horizontal axes
are equal in length and labeled a1 a2 while
the third axis is either longer or shorter and labeled c. That is a = b≠ c
(a1 = a2 ≠ c)
-
Its axial angles are
such that α = β = γ = 90o
-
The unit form is a
system made up of straight prisms with square bases.
-
The diagnostic property
if this system is a unique 1iv
axis on the c crystallographic
axis.
The Tetragonal system has 7 classes as follows:
a) The
Tetragonal holosymmetric (Ditetragonal bipyramidal) class or the Zircon type.
b) The
Tetragonal hemimorphic (Tetragonal pyramidal) class
c) The
Tetragonal Sphenoidal Class
d) The
Tetragonal Bipyramidal class
e) The
Ditetragonal hemimorphic (Ditetragonal pyramidal) class
f) The
Tetragonal scalenohedral (tetragonal bisphenoidal) class
g) The
Tetragonal Trapezohedral class.
The holohedral class of the system is
the Tetragonal holosymmetric
(Ditetragonal bipyramidal) class or zircon type with the following elements
of symmetry:
-
A center of symmetry
-
5 planes of symmetry (3
axial and 2 diagonal)
-
5 axes of symmetry (1iv and 4ii)
Forms in the Tetragonal
System:
1. Basal pinacoid: It
is a form composed of 2 parallel faces perpendicular to the c crystallographic axis. The basal pinacoids exist in combination with
the various prisms of this system which include:
-
Tetragonal Prisms of
the 1st order {I I 0
} and
-
Tetragonal Prisms of
the 2nd order {0 I 0
}
NB:
Prisms of the 1st order
are those whose faces intersect one horizontal axis and are parallel to the
rest while Prisms of the 2nd
order are those whose faces intersect two horizontal axes and are
parallel to the rest.
2. Bipyramids {I I 0 },
which is a combination of prisms, bipyramids and pinacoids;
Tetragonal
bipyramids of 1storder whose faces intersect all 3 crystallographic
axes symbolized as {I I I }
Tetragonal bipyramids of 2nd
order whose faces intersect the vertical crystallographic axis and 1 other
horizontal crystallographic axis and is parallel to the other horizontal axis.
Examples
of some minerals with this form include: Idocrase, zircon, Rutile and Cassiterite. Of them all, Idocrase shows a combination of
all the forms in the tetragonal system.
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