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Crystal habit

In mineralogy, shape and size give rise to descriptive terms applied to the typical appearance, or habit of crystals.


The many terms used by mineralogists to describe crystal habits are useful in communicating what specimens of a particular mineral often look like. Recognizing numerous habits helps a mineralogist to identify a large number of minerals. Some habits are distinctive of certain minerals, although most minerals exhibit many differing habits (the development of a particular habit is determined by the details of the conditions during the mineral formation/crystal growth). Crystal habit may mislead the inexperienced as a mineral's internal crystal system can be hidden or disguised.

Factors influencing a crystal's habit include: a combination of two or more forms; trace impurities present during growth; crystal twinning and growth conditions (i.e., heat, pressure, space). 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.

Some minerals may replace other existing minerals while preserving the original's habit: this process is called pseudomorphous replacement. A classic example is tiger's eye quartz, crocidolite asbestos replaced by silica. While quartz typically forms euhedral (well-formed), prismatic (elongate, prism-like) crystals, in tiger's eye the original fibrous habit of crocidolite is preserved.

List of crystal habits

Habit: Description: Example:
Acicular Needle-like, slender and/or tapered Rutile in quartz
Amygdaloidal Almond-shaped Heulandite
Anhedral Poorly formed, external crystal faces not developed Olivine
Bladed Blade-like, slender and flattened Kyanite
Botryoidal or globular Grape-like, hemispherical masses Smithsonite
Columnar Similar to fibrous: Long, slender prisms often with parallel growth Calcite
Coxcomb Aggregated flaky or tabular crystals closely spaced. Barite
Dendritic or arborescent Tree-like, branching in one or more direction from central point Magnesite in opal
Dodecahedral Dodecahedron, 12-sided Garnet
Drusy or encrustation Aggregate of minute crystals coating a surface Uvarovite
Enantiomorphic Mirror-image habit and optical characteristics; right- and left-handed crystals Quartz
Equant, stout, stubby or blocky Length, width, and breadth roughly equal Zircon
Euhedral Well-formed, external crystal faces developed Spinel
Fibrous or columnar Extremely slender prisms Tremolite
Filiform or capillary Hair-like or thread-like, extremely fine Natrolite
Foliated or micaceous Layered structure, parting into thin sheets Mica
Granular Aggregates of anhedral crystals in matrix Scheelite
Hemimorphic Doubly terminated crystal with two differently shaped ends. Hemimorphite
Mamillary Breast-like: surface formed by intersecting partial spherical shapes Malachite
Massive or compact Shapeless, no distinctive external crystal shape Serpentine
Nodular or tuberose Deposit of roughly spherical form with irregular protuberances Geodes
Octahedral Octahedron, eight-sided (two pyramids base to base) Diamond
Plumose Fine, feather-like scales Mottramite
Prismatic Elongate, prism-like: crystal faces parallel to c-axis well-developed Tourmaline
Pseudo-hexagonal hexagonal appearance due to cyclic twinning Aragonite
Pseudomorphous Occurring in the shape of another mineral through pseudomorphous replacement Tiger's eye
Radiating or divergent Radiating outward from a central point Pyrite suns
Reniform or colloform Similar to mamillary: intersecting kidney-shaped masses Hematite
Reticulated Acicular crystals forming net-like intergrowths Cerussite
Rosette Platy, radiating rose-like aggregate Gypsum
Sphenoid Wedge-shaped Sphene
Stalactitic Forming as stalactites or stalagmites; cylindrical or cone-shaped Rhodochrosite
Stellate Star-like, radiating Pyrophyllite
Striated/striations Surface growth lines parallel or perpendicular to a crystallographic axis Chrysoberyl
Subhedral External crystal faces only partially developed
Tabular or lamellar Flat, tablet-shaped, prominent pinnacoid Ruby
Wheat sheaf Aggregates resembling hand-reaped wheat sheaves Zeolites
This article is licensed under the GNU Free Documentation License. It uses material from the Wikipedia article "Crystal_habit". A list of authors is available in Wikipedia.
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