Editing Hematite

{{Short description|Common iron oxide mineral}}
{{About|the mineral|other uses}}
{{Infobox mineral
|boxtextcolor=#FFFFFF|boxbgcolor=#0e0d0b| name          = Hematite
| category      = [[Oxide minerals]]
| image         = WLA hmns Hematite.jpg
| imagesize     = 260
| caption       = Hematite crystals from Brazil
| formula       = [[iron(III) oxide]], Fe<sub>2</sub>O<sub>3</sub>, α-Fe<sub>2</sub>O<sub>3</sub><ref>{{cite book |last1=Dunlop |first1=David J. |last2=Özdemir |first2=Özden |title=Rock Magnetism: Fundamentals and Frontiers |date=2001 |publisher=Cambridge University Press |location=Cambridge |isbn=9780521000987 |page=73}}</ref>
| IMAsymbol   = Hem<ref>{{Cite journal|last=Warr|first=L.N.|date=2021|title=IMA–CNMNC approved mineral symbols|journal=Mineralogical Magazine|volume=85|issue=3|pages=291–320|doi=10.1180/mgm.2021.43|bibcode=2021MinM...85..291W|s2cid=235729616|doi-access=free}}</ref>
| strunz        = 4.CB.05
| dana          = 4.3.1.2
| symmetry      = ''R{{overline|3}}c'' (no. 167)
| unit cell     = ''a'' = 5.038(2)&nbsp;Å; <br />''c'' = 13.772(12)&nbsp;Å; Z&nbsp;=&nbsp;6
| color         = Metallic grey, dull to bright "rust-red" in earthy, compact, fine-grained material, steel-grey to black in crystals and massively crystalline ores
| habit         = Tabular to thick crystals; micaceous or platy, commonly in rosettes; radiating fibrous, reniform, botryoidal or stalactitic masses, columnar; earthy, granular, oolitic
| system        = [[Trigonal crystal system|Trigonal]]
| class         = Hexagonal scalenohedral ({{overline|3}}m) <br />[[H–M symbol]]: ({{overline|3}} 2/m)
| twinning      = Penetration and lamellar 
| cleavage      = None, may show partings on {0001} and {10{{overline|1}}1}
| fracture      = Uneven to subconchoidal
| tenacity      = Brittle
| mohs          = 5.5–6.5
| luster        = Metallic to splendent
| streak        = Bright red to dark red
| diaphaneity   = Opaque
| gravity       = 5.26
| density       = 5.26 - 5.3
| opticalprop   = Uniaxial (−)
| refractive    = ''n''<sub>ω</sub> = 3.150–3.220, ''n''<sub>ε</sub> = 2.870–2.940 
| birefringence = ''δ'' = 0.280
| pleochroism   = O: brownish red; E: yellowish red
| references    =<ref name=HBM>{{cite book |editor1-last=Anthony |editor1-first=John W. |editor2-last=Bideaux |editor2-first=Richard A. |editor3-last=Bladh |editor3-first=Kenneth W. |editor4-last=Nichols |editor4-first=Monte C. |title=Handbook of Mineralogy |publisher=Mineralogical Society of America |place=Chantilly, VA |chapter-url=http://rruff.geo.arizona.edu/doclib/hom/hematite.pdf |chapter=Hematite |date=1990 |access-date=December 22, 2018 |isbn=978-0962209727 |volume=III}}</ref><ref>{{cite web |url=http://webmineral.com/data/Hematite.shtml |title=Hematite Mineral Data |website=WebMineral.com |access-date=December 22, 2018}}</ref><ref>{{cite web |url=https://www.mindat.org/min-1856.html |title=Hematite |website=Mindat.org |access-date=December 22, 2018}}</ref>
}}

'''Hematite''' ({{IPAc-en|ˈ|h|iː|m|ə|ˌ|t|aɪ|t|,_|ˈ|h|ɛ|m|ə|-}}), [[American and British English spelling differences#ae and oe|also spelled as]] '''haematite''', is a common [[iron oxide]] compound with the formula, [[Iron(III) oxide|Fe<sub>2</sub>O<sub>3</sub>]] and is widely found in [[Rock (geology)|rocks]] and [[soil]]s.<ref name="TheIronOxides">{{cite book |title=The Iron Oxides |last1=Cornell |first1=Rochelle M. |last2=Schwertmann |first2=Udo |publisher=Wiley |location=Germany |year=1996 |isbn=9783527285761 |lccn=96031931 |url=https://books.google.com/books?id=R8SxQgAACAAJ |pages=4, 26 |access-date=December 22, 2018}}</ref> Hematite crystals belong to the [[Hexagonal crystal family|rhombohedral lattice system]] which is designated the [[Iron(III) oxide#Alpha phase|alpha polymorph]] of {{Chem|Fe|2|O|3}}. It has the same [[crystal structure]] as [[corundum]] ({{Chem|Al|2|O|3}}) and [[ilmenite]] ({{Chem|Fe||Ti||O|3}}). With this it forms a complete [[solid solution]] at temperatures above {{convert|950|C|F}}.

Hematite occurs naturally in black to steel or silver-gray, brown to reddish-brown, or red colors. It is [[Mining|mined]] as an important [[Iron ore#Hematite|ore mineral of iron]]. It is electrically conductive.<ref name=":0">{{Cite book|last=Morgenthau|first=Mengo L.|url=https://books.google.com/books?id=TgXbAAAAMAAJ&pg=PA33|title=Minerals and Cut Stones: Reference Book Containing Condensed and Simplified Descriptions from Standard Works on Mineralogy|year=1923|pages=23|language=en}}</ref> Hematite varieties include ''kidney ore'', ''martite'' ([[pseudomorph]]s after [[magnetite]]), ''iron rose'' and ''specularite'' ([[Specular reflection|specular]] hematite). While these forms vary, they all have a rust-red [[streak (mineralogy)|streak]]. Hematite is not only [[Mohs scale of mineral hardness|harder]] than pure iron, but also much more [[Brittleness|brittle]]. The term ''kidney ore'' may be broadly used to describe [[Crystal habit|botryoidal, mammillary, or reniform]] hematite.<ref>{{cite web | url=https://www.mindat.org/min-5576.html | title=Kidney Ore }}</ref> [[Maghemite]] is a polymorph of hematite (γ-{{Chem|Fe|2|O|3}}) with the same chemical formula, but with a [[spinel structure]] like magnetite.

Large deposits of hematite are found in [[banded iron formation]]s. Gray hematite is typically found in places that have still, standing water, or mineral [[hot spring]]s, such as those in [[Yellowstone National Park]] in [[North America]]. The mineral may [[Precipitation (chemistry)|precipitate]] in the water and collect in layers at the bottom of the lake, spring, or other standing water. Hematite can also occur in the absence of water, usually as the result of [[Volcano|volcanic]] activity.

[[Clay]]-sized hematite crystals also may occur as a secondary mineral formed by [[weathering]] processes in [[soil]], and along with other iron oxides or [[oxyhydroxide]]s such as [[goethite]], which is responsible for the red color of many [[tropical]], ancient, or otherwise highly weathered soils.

==Etymology and history==
{{Main|Ochre}}
The name hematite is derived from the [[Greek language|Greek]] word for blood, {{lang|grc|[[wikt:αἷμα|αἷμα]]}} ''(haima)'', due to the red coloration found in some varieties of hematite.<ref name="TheIronOxides" /> The color of hematite is often used as a [[pigment]]. The English name of the stone is derived from [[Middle French]] ''hématite pierre'', which was taken from [[Latin]] ''lapis haematites'' {{circa}} the 15th century, which originated from [[Ancient Greek]] {{lang|grc|αἱματίτης λίθος}} (''haimatitēs lithos'', "blood-red stone").

[[Ochre]] is a clay that is colored by varying amounts of hematite, varying between 20% and 70%.<ref name="MZ">{{cite web |title=Ochre |work=Industrial Minerals |publisher=Minerals Zone |url=http://www.mineralszone.com/minerals/ochre.html |access-date=December 22, 2018 |url-status=dead |archive-url=https://web.archive.org/web/20161115190309/http://www.mineralszone.com/minerals/ochre.html |archive-date=November 15, 2016}}</ref> Red ochre contains unhydrated hematite, whereas yellow ochre contains [[hydrate]]d hematite ([[Iron|Fe]]<sub>2</sub>[[Oxygen|O]]<sub>3</sub>&nbsp;·&nbsp;[[Hydrogen|H]]<sub>2</sub>[[Oxygen|O]]). The principal use of ochre is for tinting with a permanent color.<ref name="MZ" />

Use of the [[Sanguine|red chalk]] of this iron-oxide mineral in writing, drawing, and decoration is among the earliest in human history. To date, the earliest known human use of the powdery mineral is 164,000 years ago by the inhabitants of the [[Pinnacle Point|Pinnacle Point caves]] in what now is South Africa, possibly for social purposes.<ref>{{cite press release |author=<!--Staff writer(s); no by-line.--> |title=Researchers find earliest evidence for modern human behavior in South Africa |url=https://www.eurekalert.org/news-releases/477500 |publisher=AAAS |agency=ASU News |date=October 17, 2007 |access-date=December 22, 2018}}</ref> Hematite residues are also found in graves from 80,000 years ago. Near [[Rydno]] in [[Poland]] and [[Lovas, Hungary|Lovas]] in [[Hungary]] red chalk mines have been found that are from 5000&nbsp;BC, belonging to the [[Linear Pottery culture]] at the [[Upper Rhine]].<ref>{{cite journal |last=Levato |first=Chiara |year=2016 |title=Iron Oxides Prehistoric Mines: A European Overview |url=http://biblio.naturalsciences.be/associated_publications/studia-praehistorica-belgica/8/haematite_pdf-rgb-600_vol2_201216_p/009-023_3-1_levato_ironoxydes_201016_rgb-600-p.pdf |journal=Anthropologica et Præhistorica |volume=126 |pages=9–23 |access-date=December 22, 2018}}</ref>

Rich deposits of hematite have been found on the island of [[Elba]] that have been mined since the time of the [[Etruscans]].<ref>{{cite journal |last1=Benvenuti |first1=M. |last2=Dini |first2=A. |last3=D'Orazio |first3=M. |last4=Chiarantini |first4=L. |last5=Corretti |first5=A. |last6=Costagliola |first6=P. |title=The tungsten and tin signature of iron ores from Elba Island (Italy) |journal=Archaeometry |date=June 2013 |volume=55 |issue=3 |pages=479–506 |doi=10.1111/j.1475-4754.2012.00692.x}}</ref>

Underground hematite mining is classified as a carcinogenic hazard to humans.<ref>{{cite web | url=https://monographs.iarc.who.int/list-of-classifications | title=List of Classifications }}</ref>

==Magnetism==
Hematite shows only a very feeble response to a [[magnetic field]]. Unlike magnetite, it is not noticeably attracted to an ordinary magnet. Hematite is an [[antiferromagnetic]] material below the [[Morin transition]] at {{cvt|250|K|C}}, and a [[spin canting|canted]] antiferromagnet or weakly [[ferromagnetic]] above the Morin transition and below its [[Néel temperature]] at {{cvt|948|K|C}}, above which it is [[paramagnetic]].

The magnetic structure of α-hematite was the subject of considerable discussion and debate during the 1950s, as it appeared to be ferromagnetic with a Curie temperature of approximately {{cvt|1000|K|C}}, but with an extremely small [[magnetic moment]] (0.002&nbsp;[[Bohr magneton]]s). Adding to the surprise was a transition with a decrease in temperature at around {{cvt|260|K|C}} to a phase with no net magnetic moment. It was shown that the system is essentially antiferromagnetic, but that the low symmetry of the [[Ion#Anions and cations|cation]] sites allows [[spin–orbit coupling]] to cause [[spin canting|canting of the moments]] when they are in the plane perpendicular to the ''c'' axis. The disappearance of the moment with a decrease in temperature at {{cvt|260|K|C}} is caused by a change in the [[anisotropy]] which causes the moments to align along the ''c'' axis. In this configuration, spin canting does not reduce the energy.<ref>{{cite journal |last=Dzyaloshinsky |first=I. E. | title=A thermodynamic theory of "weak" ferromagnetism of antiferromagnetics |journal=Journal of Physics and Chemistry of Solids |volume=4 |pages=241–255 |year=1958 |doi=10.1016/0022-3697(58)90076-3 |issue=4 |bibcode=1958JPCS....4..241D}}</ref><ref>{{cite journal |last=Moriya |first=Tōru |title=Anisotropic Superexchange Interaction and Weak Ferromagnetism |journal= Physical Review|volume=120 |page=91 |issue=1 |year=1960 |doi=10.1103/PhysRev.120.91 |bibcode=1960PhRv..120...91M|url=https://hal-cea.archives-ouvertes.fr/cea-01550620/file/PhysRevB.93.214414.pdf }}</ref> The magnetic properties of bulk hematite differ from their nanoscale counterparts. For example, the Morin transition temperature of hematite decreases with a decrease in the particle size. The suppression of this transition has been observed in hematite [[nanoparticles]] and is attributed to the presence of impurities, water molecules and defects in the crystals lattice. Hematite is part of a complex solid solution oxyhydroxide system having various contents of H2O (water), hydroxyl groups and vacancy substitutions that affect the mineral's magnetic and crystal chemical properties.<ref>{{cite journal |last1=Dang |first1=M.-Z. |last2=Rancourt |first2=D. G. |last3=Dutrizac |first3=J. E. |last4=Lamarche |first4=G. |last5=Provencher |first5=R. |title=Interplay of surface conditions, particle size, stoichiometry, cell parameters, and magnetism in synthetic hematite-like materials |journal=Hyperfine Interactions |volume=117 |issue=1–4 |year=1998 |pages=271–319 |doi=10.1023/A:1012655729417 |bibcode=1998HyInt.117..271D|s2cid=94031594 }}</ref> Two other end-members are referred to as protohematite and hydrohematite.

Enhanced [[Magnetic coercivity|magnetic coercivities]] for hematite have been achieved by dry-heating a two-line ferrihydrite precursor prepared from solution. Hematite exhibited temperature-dependent magnetic coercivity values ranging from {{convert|289|to(-)|5,027|Oe|0|lk=in}}. The origin of these high coercivity values has been interpreted as a consequence of the subparticle structure induced by the different particle and [[crystallite]] size growth rates at increasing annealing temperature. These differences in the growth rates are translated into a progressive development of a subparticle structure at the nanoscale (super small). At lower temperatures (350–600&nbsp;°C), single particles crystallize. However, at higher temperatures (600–1000&nbsp;°C), the growth of crystalline aggregates, and a subparticle structure is favored.<ref>{{cite journal|last1=Vallina|first1=B.|last2=Rodriguez-Blanco|first2=J. D.|last3=Brown|first3=A. P.|last4=Benning|first4=L. G.|last5=Blanco|first5=J. A.|year=2014|title=Enhanced magnetic coercivity of α-Fe<sub>2</sub>O<sub>3</sub> obtained from carbonated 2-line ferrihydrite|journal=Journal of Nanoparticle Research|volume=16|issue=3|pages=2322|bibcode=2014JNR....16.2322V|doi=10.1007/s11051-014-2322-5|s2cid=137598876|url=http://eprints.whiterose.ac.uk/78765/19/Vallina%20et%20al%20JNR%20-%20final%20version%202014_with_coversheet.pdf}}</ref>

<gallery widths="200px" heights="200px" class="center">
File:Hematite - Titanomagnitite.jpg|A microscopic picture of hematite
File:Hematite structure.jpg|Crystal structure of hematite
</gallery>

==Mine tailings==
Hematite is present in the waste [[tailings]] of [[iron mines]]. A recently developed process, [[magnetation (iron ore)|magnetation]], uses magnets to glean waste hematite from old mine tailings in [[Minnesota]]'s vast [[Mesabi Range]] iron district.<ref>{{cite web |last=Redman |first=Chris |date=May 20, 2009 |url=https://money.cnn.com/2009/05/19/magazines/fortune/redman_iron.fortune/index.htm |title=The next iron rush |website=Money.cnn.com |access-date=December 22, 2018}}</ref> [[Falu red]] is a pigment used in traditional Swedish house paints. It is made from tailings of the [[Falun Mine]].<ref>{{cite web |url=http://falurodfarg.com/falu-rodfarg-original/ |title=Sveriges mest beprövade husfärg |trans-title=Sweden's most proven house color |language=sv |access-date=December 22, 2018}}</ref>

==Mars==
[[File:07-ml-3-soil-mosaic-B019R1 br.jpg|thumb|Image mosaic from the Mars Exploration Rover Microscopic Imager shows hematite [[Martian spherules|spherules]] partly embedded in rock at the Opportunity landing site. Image is around {{cvt|5|cm|0}} across.]]

The spectral signature of hematite was seen on the planet [[Mars]] by the infrared [[spectrometer]] on the [[NASA]] ''[[Mars Global Surveyor]]''<ref>{{cite press release |publisher=NASA |date=May 27, 1998 |url=http://tes.asu.edu/webdata/hematitepr.html |title=Mars Global Surveyor TES Instrument Identification of Hematite on Mars |access-date=December 22, 2018 |url-status=dead |archive-url=https://web.archive.org/web/20070513161834/http://tes.asu.edu/webdata/hematitepr.html |archive-date=May 13, 2007}}</ref> and ''[[2001 Mars Odyssey]]''<ref>{{cite journal |last1=Christensen |first1=Philip R. |title=Formation of the hematite-bearing unit in Meridiani Planum: Evidence for deposition in standing water |journal=Journal of Geophysical Research |date=2004 |volume=109 |issue=E8 |pages=E08003 |doi=10.1029/2003JE002233|bibcode=2004JGRE..109.8003C |doi-access=free }}</ref> spacecraft in orbit around Mars. The mineral was seen in abundance at two sites<ref>{{cite journal |last=Bandfield |first=Joshua L.|title=Global mineral distributions on Mars |journal=Journal of Geophysical Research |volume=107 |issue=E6|page=E65042 |year=2002 |doi=10.1029/2001JE001510 |url=http://tes.asu.edu/mineral_map/bandfield_minmap.pdf |bibcode=2002JGRE..107.5042B|doi-access=free }}</ref> on the planet, the [[Terra Meridiani]] site, near the Martian equator at 0° longitude, and the [[Aram Chaos]] site near the [[Valles Marineris]].<ref>{{cite journal |last1=Glotch |first1=Timothy D. |last2=Christensen |first2=Philip R. |year=2005 |title=Geologic and mineralogic mapping of Aram Chaos: Evidence for a water-rich history |journal=Journal of Geophysical Research |volume=110 |issue=E9 |page=E09006 |doi=10.1029/2004JE002389 |bibcode=2005JGRE..110.9006G|s2cid=53489327 |doi-access=free }}</ref> Several other sites also showed hematite, such as [[Aureum Chaos]].<ref>{{cite journal |last1=Glotch |first1=Timothy D. |last2=Rogers |first2=D. |last3=Christensen |first3=Philip R. |url=https://www.lpi.usra.edu/meetings/lpsc2005/pdf/2159.pdf |title=A Newly Discovered Hematite-Rich Unit in Aureum Chaos: Comparison of Hematite and Associated Units With Those in Aram Chaos |journal=Lunar and Planetary Science |volume=36 |pages=2159 |year=2005 |bibcode=2005LPI....36.2159G}}</ref> Because terrestrial hematite is typically a mineral formed in aqueous environments or by aqueous alteration, this detection was scientifically interesting enough that the second of the two [[Mars Exploration Rover]]s was sent to a site in the Terra Meridiani region designated [[Meridiani Planum]]. In-situ investigations by the [[Opportunity rover|''Opportunity'' rover]] showed a significant amount of hematite, much of it in the form of small "[[Martian spherules]]" that were informally named "blueberries" by the science team. Analysis indicates that these [[spherule]]s are apparently [[concretion]]s formed from a water solution. "Knowing just how the hematite on Mars was formed will help us characterize the past environment and determine whether that environment was favorable for life".<ref>{{cite web |url=https://mars.nasa.gov/mer/spotlight/hematite01.html |title=Hematite |publisher=NASA |access-date=December 22, 2018}}</ref>
==Jewelry==
Hematite is often shaped into beads, tumbling stones, and other jewellery components.<ref>{{Cite web |title=Hematite: A primary ore of iron and a pigment mineral |url=https://geology.com/minerals/hematite.shtml |access-date=2023-09-07 |website=geology.com}}</ref> Hematite was once used as mourning jewelry.<ref>{{Cite book|last=Oldershaw|first=Cally|url=https://books.google.com/books?id=wm_X_LzoN-cC&pg=PA56|title=Firefly Guide to Gems|publisher=Firefly Books|year=2003|isbn=978-1-55297-814-6|pages=53|language=en}}</ref><ref name=":0" /> Certain types of hematite- or iron-oxide-rich clay, especially [[Armenian bole]], have been used in [[gilding]]. Hematite is also used in art such as in the creation of [[Engraved gem|intaglio engraved gems]]. [[Hematine]] is a synthetic material sold as ''magnetic hematite''.<ref>{{cite web |url=https://www.mindat.org/min-35948.html |title=Magnetic Hematite |website=Mindat.org |access-date=December 22, 2018}}</ref>

== Pigment ==
Hematite has been sourced to make pigments since earlier origins of human pictorial depictions, such as on cave linings and other surfaces, and has been employed continually in artwork through the eras. In Roman times, the pigment obtained by finely grinding hematite was known as ''sil atticum''. Other names for the mineral when used in painting include ''colcotar'' and ''caput mortuum''. In Spanish, it is called ''almagre'' or ''almagra'', from the Arabic ''al-maghrah'', red earth, which passed into English and Portuguese. Other ancient names for the pigment include ''ochra hispanica'', ''sil atticum antiquorum'', and ''Spanish brown''.<ref>{{Cite book |last=Calvo Rebollar |first=Miguel |title=Minerales y Minas de España. Vol. 4. Óxidos e hidróxidos. |date=2009 |publisher=Escuela Técnica Superior de Ingenieros de Minas de Madrid. Fundación Gómez Pardo. |isbn=978-84-95063-99-1 |location=Madrid, Spain |language=es |trans-title=Minerals and mines of Spain Vol 4. Oxides and Hidroxides}}</ref> It forms the basis for red, purple, and brown iron-oxide pigments, as well as being an important component of ochre, sienna, and umber pigments.<ref>{{Cite web |title=Colors from the Earth: Violet Hematite |url=https://www.naturalpigments.com/artist-materials/violet-color-hematite-earth-pigments |access-date=2023-09-07 |website=www.naturalpigments.com |language=en}}</ref> The main producer of hematite for the pigment industry is India, followed distantly by Spain.

== Industrial purposes ==
As mentioned earlier, hematite is an important mineral for iron ore. The physical properties of hematite are also employed in the areas of medical equipment, shipping industries, and coal production. Having high density and capable as an effective barrier against X-ray passage, it often is incorporated into radiation shielding. As with other iron ores, it often is a component of ship ballasts because of its density and economy. In the coal industry, it can be formed into a high specific density solution, to help separate coal powder from impurities.<ref>{{Cite web |title=Hematite: A primary ore of iron and a pigment mineral |url=https://geology.com/minerals/hematite.shtml |access-date=2023-09-07 |website=geology.com}}</ref>

==Gallery==
<gallery widths="133" heights="130">
File:Hematite-LTH43A.JPG|A rare pseudo-scalenohedral crystal habit
File:Quartz-Hematite-113680.jpg|Three gemmy quartz crystals containing bright rust-red inclusions of hematite, on a field of sparkly black specular hematite
File:Rutile-Hematite-113489.jpg|Golden acicular crystals of [[rutile]] radiating from a center of platy hematite
File:Cylinder seal antelope Louvre AM1639.jpg|[[Cypro-Minoan syllabary|Cypro-Minoan]] [[cylinder seal]] (left) made from hematite with corresponding impression (right), approximately 14th century BC
File:Hematite-254990.jpg|A cluster of parallel-growth, mirror-bright, metallic-gray hematite blades from Brazil
File:Hematite.bear.660pix.jpg|Hematite carving, {{cvt|5|cm|0}} long
File:Hematit 2.jpg|Hematite, variant specularite (specular hematite), with fine grain shown
File:Hematite-rich BIF ventifact.jpg|Red hematite from [[banded iron formation]] in [[Wyoming]]
File:Hematite on mars.jpg|Hematite on Mars as found in form of "blueberries" (named by NASA)
File:Hematite streak plate.jpg|[[Streak (mineralogy)|Streak plate]], showing that hematite consistently leaves a rust-red streak
File:Hematite in Scanning Electron Microscope, magnification 100x.JPG|Hematite in scanning electron microscope, magnification 100x
File:Micaceous hematite.jpg|Micaceous hematite taken with permission from Kelly's Mine, Lustleigh, Devon UK
File:Hemacollage.png|[[Cumbria|Cumbrian]] [[botryoidal]] hematite under [[Hand lens|hand-lens]]. Despite all being present on the same sample, the botryoids themselves vary widely in diameter. 
</gallery>

==See also==
*[[Mill scale]]
*[[Mineral redox buffer]]
*[[Wüstite]]

==References==
{{Reflist}}

==External links==
{{Commons}}
*[https://www.mindat.org/min-1856.html MineralData.org]

{{Ores}}
{{Gemstones}}
{{Jewellery}}

{{Authority control}}

[[Category:Oxide minerals]]
[[Category:Iron(III) minerals]]
[[Category:Iron oxide pigments]]
[[Category:Hematite group]]
[[Category:Trigonal minerals]]
[[Category:Minerals in space group 167]]
[[Category:Iron ores]]
[[Category:Glances]]
[[Category:Magnetic minerals]]
[[Category:Jewellery components]]
[[Category:Symbols of Alabama]]