Colemanite

{{Short description|Borate mineral}}

{{for|the community in California formerly named Colemanite|Ryan, California}}

{{Infobox mineral

| name = Colemanite

| category = Inoborates

| image = Colemanite - USGS Mineral Specimens 096.jpg

| imagesize = 260px

| caption =

| formula = Ca2B6O11·5H2O

| IMAsymbol=Cole{{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}}

| strunz = 6.CB.10

| system = Monoclinic

| class = Prismatic (2/m)
(same H-M symbol)

| symmetry = P21/a

| unit cell = a = 8.712(2) Å,
b = 11.247(3) Å,
c = 6.091(1) Å;
β = 110.12°; Z = 4

| color = Colorless, white, yellowish, grey

| habit = Massive granular to coarsely crystalline, most commonly nodular.

| twinning =

| cleavage = [010] perfect, [001] distinct

| fracture = Brittle uneven to subconchoidal

| mohs = 4.5

| luster = Vitreous

| refractive = nα = 1.586 nβ = 1.592 nγ = 1.614

| opticalprop = Biaxial (+)

| birefringence = δ = 0.028

| pleochroism =

| streak = White

| gravity = 2.42

| density =

| melt =

| fusibility = 1.5

| diagnostic = Exfoliates on heating, produces a green flame

| solubility =

| diaphaneity = Transparent to translucent

| other = Bright pale yellow fluorescence, may phosphoresce pale green; pyroelectric and piezoelectric at very low temperature.

| references = {{cite web |first1=Stefan |last1=Schorn |display-authors=etal |title=Colemanit (Colemanite) |url=https://www.mineralienatlas.de/lexikon/index.php/MineralData?mineral=Colemanite |website=Mineralienatlas |year=2021}}{{cite book |last1=Klein |first1=Cornelis |last2=Hurlbut |first2=Cornelius S. Jr. |title=Manual of mineralogy: (after James D. Dana) |date=1993 |publisher=Wiley |location=New York |isbn=0-471-57452-X |edition=21st |page=422}}{{mindat |name=Colemanite |id=1108 |access-date=30 December 2021}}{{cite web |url=http://webmineral.com/data/Colemanite.shtml |website=Webmineral |title=Colemanite mineral data |access-date=30 December 2021}}{{cite web |url=http://rruff.geo.arizona.edu/doclib/hom/colemanite.pdf |website=Handbook of Mineralogy |year=2005 |title=Colemanite |first1=John W. |last1=Anthony |first2=Richard A. |last2=Bideaux |first3=Kenneth W. |last3=Bladh |first4=Monte C. |last4=Nichols}}

}}

Colemanite (Ca2B6O11·5H2O) or (CaB3O4(OH)3·H2O) is a borate mineral found in evaporite deposits of alkaline lacustrine environments. Colemanite is a secondary mineral that forms by alteration of borax and ulexite.

It was first described in 1884 for an occurrence near Furnace Creek in Death Valley and was named after William Tell Coleman (1824–1893), owner of the mine "Harmony Borax Works" where it was first found. At the time, Coleman had alternatively proposed the name "smithite" instead after his business associate Francis Marion Smith.Hildebrand, GH. (1982) Borax Pioneer: Francis Marion Smith. San Diego: Howell-North Books. p 31 {{ISBN|0-8310-7148-6}}

Uses

Colemanite is an important ore of boron, and was the most important boron ore until the discovery of kernite in 1926. It has many industrial uses, like the manufacturing of heat resistant glass.{{cite book |chapter=Nitrates |date=1977 |title=Simon & Schuster's Guide to Rocks and Minerals |publisher=Simon & Schuster |isbn=978-0-671-24417-0 |page=entry 111 |url=https://archive.org/details/isbn_9780671244170 }}

Occurrence

About 40% of the world's known colemanite reserves are at the Emet mine in western Turkey.{{cite web |title=Emet |url=https://www.etimaden.gov.tr/en/emet |website=Eti Maden |access-date=29 November 2024}} Other important sources in Turkey are found at Bigadiç and Kestelek.{{cite web |title=Country Profile – Boron Turkey |url=https://borates.today/country-profile-boron-turkey/ |website=Borates Today |access-date=29 November 2024}}

See also

References