Crystal habit

Mineralogical term for the visible shape of a mineral From Wikipedia, the free encyclopedia

Crystal habit

In mineralogy, crystal habit is the characteristic external shape of an individual crystal or aggregate of crystals. The habit of a crystal is dependent on its crystallographic form and growth conditions, which generally creates irregularities due to limited space in the crystallizing medium (commonly in rocks).[1][2]

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Smoky quartz with spessartine on top of feldspar matrix, featuring different crystal habits (shapes)

Crystal forms

Recognizing the habit can aid in mineral identification and description, as the crystal habit is an external representation of the internal ordered atomic arrangement.[1] 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;
  • Subhedral: 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.

Altering factors

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Goethite replacing pyrite cubes

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.

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 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

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Perspective

[3][better source needed][4][better source needed][5][better source needed][6]

Aggregate habits

More information Habit, Image ...
Habit Image Description Common example(s)
Acicular
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Needle-like, slender, and end-tapered prisms growing in a radial/globular fashion. natrolite, scolecite, yuanfuliite
Arborescent
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Tree-like crystals growing similar to branches. copper, gold, silver
Capillary/Filiform
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Hair-like or thread-like, extremely fine byssolite, millerite
Colloform/Nodular/Tuberose
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Rounded, finely banded deposits with irregular concentric protuberances agate, baryte, sphalerite
Concentric
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Circular ring aggregates around a center. This habit is found in cross-sections from reniform/mamillary habits, and also from elongated stalactites of amethyst (quartz), malachites, rhodocrosite, and others agate, quartz, malachite, rhodocrosite
Dendritic
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Root-like, branching in one or more direction from central point copper, gold, romanechite, magnesite, silver
Druse/Encrustation
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Aggregate of crystals coating a surface or cavity, usually found in geodes and some fossils azurite, celestine, calcite, uvarovite, malachite, quartz
Fibrous/Asbestiform
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Extremely slender prisms forming muscle-like fibers actinolite, asbestos, baryte, kyanite, gypsum, nitratine, stilbite, serpentine group
Foliated/Micaceous/Lamellar
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Layered crystal planes, parting into thin sheets biotite, hematite, muscovite, lepidolite, molybdenite
Granular
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Aggregates of diminute anhedral crystals in matrix or other surface andradite, bornite, scheelite, quartz, uvarovite
Hopper
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Outer portions of cubes grow faster than inner portions, creating a concavity similar to that of a hopper bismuth (artificial), halite, galena
Oolithic
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Small spheres or grains (commonly flattened) that resemble eggs aragonite, calcite
Pisolitic
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Rounded concentric nodules often found in sedimentary rocks. Much larger than oolithic aragonite, bauxite, calcite, pisolite
Platy/Tabular/Blocky
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Flat, tablet-shaped, prominent pinnacoid baryte, feldspar, topaz, vanadinite, wulfenite
Plumose
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Fine, feather-like scales aurichalcite, okenite, mottramite
Radial/Radiating/Divergent
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Radiating outward from a central point without producing a star (crystals are generally separated and have different lengths). aenigmatite, atacamite, epidote, pyrophyllite, stibnite
Reticulated
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Crystals forming triangular net-like intergrowths. cerussite, rutile
Rosette/Lenticular
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Platy, radiating rose-like aggregate (also lens shaped crystals) gypsum, baryte, calcite
Stalactitic
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Forming as stalactites or stalagmites; cylindrical or cone-shaped. Their cross-sections often reveal a "concentric" pattern calcite, chalcedony, chrysocolla, goethite, malachite, romanechite
Stellate
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Star-like, radial fibers found inside spherical habits, such as mamillary or reniform. hematite, pectolite, shattuckite, wavellite
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Asymmetrical/Irregular habits

More information Habit, Image ...
Habit Image Description Common example(s)
Amygdaloidal
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Like embedded almonds heulandite, stilbite, zircon
Hemimorphic
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Doubly terminated crystal with two differently shaped ends elbaite, hemimorphite, olivine
Massive/Compact
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Shapeless, no distinctive external crystal shape limonite, turquoise, cinnabar, quartz, realgar, lazurite
Sceptered
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Crystal growth stops and continues at the top of the crystal, but not at the bottom. Exceptional aggregates of this habit (such as quartz) are often referred as "Elestial". baryte, calcite, marcasite, quartz
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Symmetrical habits

More information Habit, Image ...
Habit Image Description Common example(s)
Cubic
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Cube-shaped fluorite, pyrite, galena, halite
Dodecahedral
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Dodecahedron-shaped, 12-sided. Central facet can vary. garnet, pyrite
Enantiomorphic
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Mirror-image habit (i.e. crystal twinning) and optical characteristics; right- and left-handed crystals aragonite, gypsum, quartz, plagioclase, staurolite
Hexagonal
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Hexagonal prism (six-sided) beryl, galena, quartz, hanksite, vanadinite
Icositetrahedral
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Icositetrahedron-shaped, 24-faced analcime, spessartine
Octahedral
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Octahedron-shaped, square bipyramid (eight-sided) diamond, fluorine, fluorite, magnetite, pyrite
Prismatic
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Elongate, prism-like: may or not present well-developed crystal faces parallel to the vertical axis beryl, tourmaline, vanadinite
Rhombohedral
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Rhombohedron-shaped (six-faced rhombi) calcite, magnesite, rhodochrosite, siderite
Scalenohedral
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Scalenohedron-shaped, pointy ends calcite, rhodochrosite, titanite
Tetrahedral
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Tetrahedron-shaped, triangular pyramid (four-sided) chalcopyrite, tetrahedrite, sphalerite, magnetite
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Rounded/Spherical habits

More information Habit, Image ...
Habit Image Description Common example(s)
Botryoidal
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Grape-like, large and small hemispherical masses, nearly differentiated/separated from each other calcite, chalcedony, halite, plumbogummite, smithsonite
Globular
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Isolated hemispheres or spheres calcite, fluorite, gyrolite
Mammillary
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Breast-like: surface formed by intersecting partial spherical shapes, larger version of botryoidal and/or reniform, also concentric layered aggregates. chalcedony, hematite, malachite
Reniform
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Irregular kidney-shaped spherical masses cassiterite, chalcedony, chrysocolla, hematite, hemimorphite fluorite, goethite, greenockite, malachite, rhodochrosite, smithsonite, mottramite, wavellite
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See also

References

Bibliography

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