
In
mineralogy
Mineralogy is a subject of geology specializing in the scientific study of the chemistry, crystal structure, and physical (including optical) properties of minerals and mineralized artifacts. Specific studies within mineralogy include the proces ...
, crystal habit is the characteristic external shape of an individual
crystal or crystal group. The habit of a crystal is dependent on its
crystallographic form
A crystal or crystalline solid is a solid material whose constituents (such as atoms, molecules, or ions) are arranged in a highly ordered microscopic structure, forming a crystal lattice that extends in all directions. In addition, macros ...
and growth conditions, which generally creates irregularities due to limited space in the
crystallizing medium (commonly in
rocks
In geology, rock (or stone) is any naturally occurring solid mass or aggregate of minerals or mineraloid matter. It is categorized by the minerals included, its chemical composition, and the way in which it is formed. Rocks form the Earth's ...
).
[Klein, Cornelis, 2007, ''Minerals and Rocks: Exercises in Crystal and Mineral Chemistry, Crystallography, X-ray Powder Diffraction, Mineral and Rock Identification, and Ore Mineralogy,'' Wiley, third edition, ][Wenk, Hans-Rudolph and Andrei Bulakh, 2004, ''Minerals: Their Constitution and Origin,'' Cambridge, first edition, ]
Recognizing the habit can aid in mineral identification and description, as the crystal habit is an external representation of the
internal ordered atomic arrangement.
Most natural crystals, however, do not display ideal habits and are commonly malformed. Hence, it is also important to describe the quality of the shape of a mineral specimen:
*
Euhedral: a crystal that is completely bounded by its characteristic faces, well-formed. Synonymous terms: idiomorphic, automorphic;
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Subhedral
Euhedral crystals (also known as idiomorphic or automorphic crystals) are those that are well-formed, with sharp, easily recognised faces. The opposite is anhedral (also known as ''xenomorphic'' or ''allotriomorphic''): a rock with an anhedral ...
: a crystal partially bounded by its characteristic faces and partially by irregular surfaces. Synonymous terms: hypidiomorphic, hypautomorphic;
*
Anhedral: a crystal that lacks any of its characteristic faces, completely malformed. Synonymous terms: allotriomorphic, xenomorphic.

Factors influencing habit include: a combination of two or more crystal forms; trace impurities present during growth;
crystal twinning and growth conditions (i.e., heat, pressure, space); and specific growth tendencies such as growth
striations. Minerals belonging to the same
crystal system do not necessarily exhibit the same habit. Some habits of a mineral are unique to its variety and locality: For example, while most
sapphires form elongate barrel-shaped crystals, those found in
Montana form stout ''tabular'' crystals. Ordinarily, the latter habit is seen only in
ruby. Sapphire and ruby are both varieties of the same mineral:
corundum
Corundum is a crystalline form of aluminium oxide () typically containing traces of iron, titanium, vanadium and chromium. It is a rock-forming mineral. It is a naturally transparent material, but can have different colors depending on the pres ...
.
Some minerals may replace other existing minerals while preserving the original's habit, i.e.
pseudomorphous replacement. A classic example is
tiger's eye quartz,
crocidolite asbestos
Asbestos () is a naturally occurring fibrous silicate mineral. There are six types, all of which are composed of long and thin fibrous crystals, each fibre being composed of many microscopic "fibrils" that can be released into the atmosphere b ...
replaced by
silica. While quartz typically forms ''prismatic'' (elongate, prism-like) crystals, in tiger's eye the original ''fibrous'' habit of crocidolite is preserved.
List of crystal habits
See also
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Abnormal grain growth
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Grain growth
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Crystal structure
References
{{ Mineral identification
Crystallography
Mineralogy concepts
Mineral habits