Stellerite

{{Short description|Zeolite mineral}}

{{Infobox mineral

| name = Stellerite

| category = Tectosilicate minerals, zeolite group, stilbite subgroup

| boxwidth =

| boxbgcolor =

| image = Stellerite - Takat, Imilchil, Midelt Province, Drâa-Tafilalet Region, Morocco.jpg

| imagesize = 270px

| caption =

| formula = Ca(Al2Si7O18)·7H2O

| IMAsymbol = Ste{{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}}

| molweight =

| strunz = 9.GE.15

| system = Orthorhombic

| class = Dipyramidal (mmm)
H-M symbol: (2/m 2/m 2/m)

| symmetry = Fmmm

| unit cell =

| color = Colorless to white, pink, orange

| habit = Spherical, Stellate, Tabular

| twinning =

| cleavage = Perfect on {010}

| fracture = Uneven

| tenacity =

| mohs = 4.5

| luster = Pearly

| refractive =

| opticalprop = Biaxial (-), a=1.4848, b=1.4864-1.4964, g=1.4979

| birefringence = δ = 0.013

| pleochroism =

| streak = white

| gravity = approximately 2.2

| density = 2.13 g/cm3

| melt =

| fusibility =

| diagnostic =

| solubility =

| diaphaneity = Transparent to translucent

| other =

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Stellerite is a rare mineral discovered by and named after Georg Wilhelm Steller, a German explorer and zoologist.{{cite journal |last1=Pabst |first1=Adolf |title=The relation of stellerite and epidesmine to stilbite |journal=Mineralogical Magazine and Journal of the Mineralogical Society |date=March 1939 |volume=25 |issue=164 |pages=271–276 |doi=10.1180/minmag.1939.025.164.06|bibcode=1939MinM...25..271P }} The mineral has a general formula of Ca[Al2Si7O18]·7H2O.{{Cite web |title=Stellerite |work=PubChem |publisher=National Library of Medicine |date= |access-date=19 October 2023 |url= https://pubchem.ncbi.nlm.nih.gov/compound/Stellerite#section=Synonyms}} Like most rare minerals, there are few commercial uses for stellerite. Mineral collectors are lucky to find it in good enough crystal form. Zeolites, including stellerite, have been studied using a dehydration process to gauge the potential use of their phases as molecular sieves, sorbents, and catalysts.{{cite journal |last1=Arletti |first1=R. |last2=Mazzucato |first2=E. |last3=Vezzalini |first3=G. |title=Influence of dehydration kinetics on T-O-T bridge breaking in zeolites with framework type STI: The case of stellerite |journal=American Mineralogist |date=1 April 2006 |volume=91 |issue=4 |pages=628–634 |doi=10.2138/am.2006.1966|bibcode=2006AmMin..91..628A |hdl=2318/80204 |s2cid=36048763 |hdl-access=free }} Its occurrences are in cavities of andesite as sheaf-like clusters of small crystals.

Crystal habit

Stellerite is part of the orthorhombic crystal system which means it has three axes of unequal length that intersect at 90° angles. Its crystal class is rhombic-dipyramidal which means it has three perpendicular two-fold rotational axes with perpendicular mirror planes.{{cite journal |last1=Miller |first1=S. A. |last2=Taylor |first2=J. C. |title=Neutron single crystal diffraction study of an Australian Stellerite |journal=Zeolites |date=1 January 1985 |volume=5 |issue=1 |pages=7–10 |doi=10.1016/0144-2449(85)90003-X}} Stilbite, another zeolite, is very similar to stellerite in both chemical composition and physical appearance. Stellerite is more commonly found in rounded radiating clusters or as single crystals and appears more transparent than stilbite does.

Optical properties

Stellerite is an anisotropic mineral, meaning that it has different properties in different directions-such as indices of refraction-when light passes through it. A refractive index (n) measures the speed of light in a substance—or in the case of mineralogy—in a mineral. It is expressed as a ratio of the speed of light in vacuum to that in a mineral."Index of Refraction." Encyclopedia Americana. Grolier Online http://ea.grolier.com/article?id=0213810-00 (accessed May 2, 2010) Stellerite has three indices of refraction because it is a biaxial mineral.

References