Fracture is the characteristic
mark left when a mineral chips or breaks. Cleavage and fracture
differ in that cleavage is
the break of a crystal face where a new face (resulting in
a smooth
plane) is formed, whereas fracture is the "chipping" of
a mineral. All minerals exhibit a fracture, even those that
exhibit cleavage. If a mineral with cleavage is chipped a certain way,
it will fracture rather than cleave.
Various
types of mineral fractures include:
Conchoidal:
Fracture
resembling a semicircular shell, with a smooth, curved surface.
An good
illustration of a conchoidal
fracture is a large chip in a piece of glass. This fracture
is also known as "shelly" in some references.
Uneven:
Fracture that leaves a rough or irregular surface.
Hackly:
Fracture that
resembles broken metal, with rough, jagged, points. True
metals exhibit this fracture. This fracture is
also known as "jagged".
Splintery:
Fracture that forms elongated splinters. All fibrous
minerals fall into this category.
Crumbly:
Fracture of minerals that crumble when broken.
Even:
Fracture that forms a smooth surface.
Sub-Conchoidal:
Fracture that falls somewhere between conchoidal
and even; smooth with irregular rounded corners.
Some
references may describe additional fractures not mentioned
above, but those terms are either synonymous or simply used
as a verbal depiction of the authors inference.
Almost
all minerals have a characteristic fracture. Some
minerals of the same species may exhibit a different
fracture, but this
is rare.