edenite
{{short description|Amphibole, double chain inosilicate mineral}}
{{Infobox mineral
| name = Edenite
| category = Amphibole mineral
| boxwidth =
| boxbgcolor =
| image = Edenite-188165.jpg
| imagesize =
| caption = Edenite crystal from Bancroft District, Ontario
| formula = NaCa2Mg5(Si7Al)O22(OH)2
| molweight = 834.25 g/mol
| strunz = 9.DE.15
| system = Monoclinic
| class = Prismatic (2/m)
(same H-M symbol)
| symmetry = C2/m
| unit cell = a = 9.83, b = 17.95
c = 5.3 [Å], β = 105.18°; Z = 2
| color = White to gray, pale to dark green, also brown and pale pinkish-brown
| habit = Prismatic crystals, fibrous, as reaction rims on pyroxenes
| twinning = Simple or multiple parallel to {010}
| cleavage = Good on (110)
| fracture = Conchoidal
| tenacity = Brittle
| mohs = 5–6
| luster = Vitreous
| refractive = nα = 1.606 – 1.649, nβ = 1.617 – 1.660, nγ = 1.631 – 1.672
| opticalprop = Biaxial (+)
| 2V = 50–82°
| birefringence = δ = 0.025
| pleochroism = Distinct, greens, blue-greens, and yellow-browns
| streak = White
| gravity = 3.05–3.37
| density =
| melt =
| fusibility =
| diagnostic =
| solubility =
| diaphaneity = Semitransparent
| other =
| references = [http://www.handbookofmineralogy.org/pdfs/edenite.pdf Edenite Handbook of Mineralogy][http://www.mindat.org/min-1351.html Edenite on Mindat.org][http://webmineral.com/data/Edenite.shtml Edenite on Webmineral][http://pubsites.uws.edu.au/ima-cnmnc/ IMA Master List]
}}
Edenite or edenitic hornblende is a double chain silicate mineral of the amphibole group with the general chemical composition NaCa2Mg5(Si7Al)O22(OH)2. Edenite is named for the locality of Edenville, Orange County, New York, where it was first described.
Occurrence
Edenite has been found primarily in metamorphic rocks, occurring in pods of other magnesium-rich minerals within a marble formation or with garnet-rich lherzolites from deep within the Earth's crust.{{cite journal|author1=Oberti, R. |author2=Cámara, F. |author3=Della Ventura, G. |author4=Iezzi, G. |author5= Benimoff, A.I. |name-list-style=amp|year=2006|title= Parvo-mangano-edenite, parvo-manganotremolite, and the solid solution between Ca and Mn2+ at the M4 site in amphiboles|journal= American Mineralogist|volume= 91|pages= 526–532|doi=10.2138/am.2006.1905|url=http://rruff.geo.arizona.edu/doclib/am/vol91/AM91_526.pdf|issue=4|bibcode=2006AmMin..91..526O |s2cid=55824304 }}{{cite journal|author=Yang, J. |year=2003 |title=Relict edenite in a garnet lherzolite from the Chinese Su-Lu UHP metamorphic terrane: Implications for metamorphic history |url=http://www.igcas.ac.cn/admin/uploadfiles/20041028175038_Yang-AM-03.pdf |journal=American Mineralogist |volume=88 |issue=1 |pages=180–188 |doi=10.2138/am-2003-0121 |bibcode=2003AmMin..88..180Y |s2cid=133200002 |url-status=dead |archiveurl=https://web.archive.org/web/20120329105748/http://www.igcas.ac.cn/admin/uploadfiles/20041028175038_Yang-AM-03.pdf |archivedate=2012-03-29 }} Thus, finding edenite in the field can indicate high-temperature regional metamorphism of the surrounding rocks.
Uses and importance
While edenite is not important for commercial or industrial applications, it is often studied because of its unique chemical substitution properties. Results from research performed on amphiboles have shown that edenite is particularly suited for fitting chloride anions into its chemical framework.{{cite journal|author1=Oberti, R. |author2=Hawthorne, F.C. |author3=Cannillo, E. |author4=Cámara, F. |name-list-style=amp|year=2007|title= Long-Range Order in Amphiboles|journal= Reviews in Mineralogy and Geochemistry|volume= 67|issue=1 |pages= 125–171|doi=10.2138/rmg.2007.67.4|bibcode=2007RvMG...67..125O }} This makes edenite a good candidate for use in chlorine isotope fractionation in amphibole-bearing rocks. Many synthetic variations of edenite are also used in geochemical research to produce a boron analogue of fluoroedenite.{{cite journal|author1=Oberti, R. |author2=Della Ventura, G. |author3=Cámara, F. |name-list-style=amp|year=2007|title= New Amphibole Compositions: Natural and Synthetic|journal= Reviews in Mineralogy and Geochemistry|volume= 67|issue=1 |pages= 89–124|doi=10.2138/rmg.2007.67.3|bibcode=2007RvMG...67...89O }}
Crystal habit
Edenite is a member of the monoclinic crystal system and is in the crystal class 2/m (space group C2/m). This means crystalline edenite is symmetrical around a two-fold rotation axis that is then reflected across a mirror plane perpendicular to the long axis of the mineral.Klein, C., and Dutrow, B. (2007) The 23rd Edition of the Manual of Mineral Science, John Wiley and Sons, Inc. Hoboken, New Jersey, U.S.
Optical properties
Edenite is a biaxial positive mineral. When viewed in thin section with a petrographic microscope, it is white-gray with pale green pleochroism in plane-polarized light. Under crossed polars, its interference colors range from first order gray to first order blue.