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Also with galena.","Crystals frequently thin to thick tabular {001}, commonly with {210}, {101} and rhomboidal in outline. Also extended [100] or [010] at times. Prismatic [001] with large {210} and vertically striated; prismatic [100], with large {011}; stout prismatic [010], with {101}, {102}; tabular {100}; equant or pyramidal with {111}, {211} or otherwise. {100} and {210} commonly striated [001]. Massive; granular to compact; nodular; stalactitic.",2.5,3,"6.37","6.39","6.36","Adamantine to resinous, or vitreous.","Adamantine,Vitreous,Resinous","Transparent,Translucent,Opaque","Colorless","Colorless to white, often tinted grey, yellow, green or  blue; colourless in transmitted light.",[60,61,62,63,64,65],"colorless","white","gray","yellow","green","blue",[60],"Often flouresces yellow under LW UV.","Shades of yellow and golden-yellow (UV).","Good on {001}, distinct on {201}; on {010} in traces.","Distinct\u002FGood","Conchoidal","brittle","Biaxial","+","1.878","1.883","1.895","68","75",1.878,1.895,"relatively strong","Inverts to a monoclinic polymorph at about 864°C. Decomposes between 900°C and 1000°C.","Ore of lead.","Baryte Group.\r\n\r\nAlong with cerussite, the most common secondary lead mineral.","Named \"vitriol of lead\" in 1783 by William Withering (1741-1799) in his \"Outlines of Mineralogy\" (a translation of the original by Torbern Bergman (1735-1784)).\r\n\r\nNamed \"anglésine\" in 1832 by François Sulpice Beudant (1787-1850) for the type locality, the Parys Mine on the Island of Anglesey (Ynys Môn) in Wales, U.K.\r\n\r\nLater renamed to anglesite.","2026-03-23 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Mountain Mines, Amlwch, Isle of Anglesey, Wales, UK",53.3869444,-4.3444444,"UK",2804,[340,343,347,351,355,359,363,367,371,375,379,383,388,391,396,400,403,408,413,416,420,425,429,434,437,442,445,449,453,457,461,466,470,474,478,482,486,489,494,497,501,506,510,513,517,521,525,529,533,537,542,546,551,556,560,565,569,574,579,584],{"id":341,"year":11,"html":342,"doi":11},19420729,"Sella, Q. (1878) Delle forme cristalline dell'anglesite di Sardegna. Transunti della Regia Accademia dei Lincei: 3, serie III: 150-158.",{"id":344,"year":345,"html":346,"doi":11},16100562,1779,"Monnet (1779) System of Mineralogy: 371. [as Vitriol de Plomb]",{"id":348,"year":349,"html":350,"doi":11},16520514,1783,"Bergman, Torbern (1783) \u003Ci>Sciagraphia Regni Mineralis Secundum Principia Proxima Digesti [Sketch of the Mineral Kingdom According to the Proximate Principles of Digestion]\u003C\u002Fi>. Apud Johannem Murray, Londini. 165pp. \u003Ca target='_blank' href='https:\u002F\u002Farchive.org\u002Fdownload\u002Fb33021491\u002Fb33021491.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":352,"year":353,"html":354,"doi":11},16100564,1787,"Proust (1787) Lettre de M. Proust a M. De La Métherie, sur le borax. Journal de Physique - Observations sur la Physique, sur L'Histoire Naturelle, et sur les Arts, Paris: 30: 393-396. [as Vitriol de Plomb]",{"id":356,"year":357,"html":358,"doi":11},16100565,1789,"Lasius (1789) Beob. Harzgeb.: 2: 355. [as Bleiglas]",{"id":360,"year":361,"html":362,"doi":11},16129826,1791,"Karsten, D.L.G. (1791) \u003Ci>Tabellarische Übersicht der mineralogisch-einfachen Fossilien\u003C\u002Fi> (1st ed.). Heinrich August Rottmann.",{"id":364,"year":365,"html":366,"doi":11},16772235,1802,"Klaproth, M. H. (1802) LXXXVIII. Untersuchung der schwefelsauren Bleierze I. von Anglesea. In \u003Ci>Beiträge zur chemischen Kenntniss der Mineralkörper\u003C\u002Fi> Vol. 3. Rottmann. p.162-164. \u003Ca target='_blank' href='https:\u002F\u002Fwww.e-rara.ch\u002Fdownload\u002Fpdf\u002F12724692.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":368,"year":369,"html":370,"doi":11},18530121,1832,"Beudant, François-Sulpice (1832) \u003Ci>Traité élémentaire de minéralogie. Deuxiéme Edition [Elementary Treatise on Mineralogy. Second Edition]\u003C\u002Fi> (2nd ed.) Vol. 2 - Tome II [Volume  II]. Chez Verdière. \u003Ca target='_blank' href='https:\u002F\u002Farchive.org\u002Fdownload\u002Fbub_gb_XSRCAAAAcAAJ\u002Fbub_gb_XSRCAAAAcAAJ.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":372,"year":373,"html":374,"doi":11},12986374,1853,"Koksharov, Nikolai (1853) \u003Ci>Materialien zur Mineralogie Russlands\u003C\u002Fi> Vol. 1. Carl Kray. \u003Ca target='_blank' href='https:\u002F\u002Farchive.org\u002Fdownload\u002Fbub_gb_o8IJAAAAIAAJ\u002Fbub_gb_o8IJAAAAIAAJ.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":376,"year":377,"html":378,"doi":11},16100570,1859,"Lang (1859) Königliche Akademie der Wissenschaften, Sitzungsberichte, Vienna: 36: 241.",{"id":380,"year":381,"html":382,"doi":11},16100571,1873,"Brush, G.J. (1873) On a compact Anglesite from Arizona. American Journal of Science and Arts: 5(30): 421.",{"id":384,"year":385,"html":386,"doi":387},101204,1877,"Arzruni, A. (1877) Ueber den Einfluss der Temperatur auf die Brechungsexponenten der natürlichen Sulfate des Baryum, Strontium und Blei. \u003Ci>Zeitschrift für Kristallographie - Crystalline Materials\u003C\u002Fi>,  1 (1) 165-192 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1524\u002Fzkri.1877.1.1.165'>doi:10.1524\u002Fzkri.1877.1.1.165\u003C\u002Fa>","10.1524\u002Fzkri.1877.1.1.165",{"id":389,"year":385,"html":390,"doi":11},16100573,"Krenner, J.A. (1877) Ueber Ungarns Anglesite (On Hungary's Anglesite). Zeitschrift für Kristallographie-Crystalline Materials: 1(1-6): 321-334.",{"id":392,"year":393,"html":394,"doi":395},5326,1886,"Solly, R. H. (1886) Anglesite from Portugal. \u003Ci>Mineralogical Magazine and Journal of the Mineralogical Society\u003C\u002Fi>,  7 (33) 61-62 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.1886.007.33.04'>doi:10.1180\u002Fminmag.1886.007.33.04\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002FMinMag\u002FVolume_7\u002F7-33-61.pdf' class='refpdflink'>\u003C\u002Fa>","10.1180\u002Fminmag.1886.007.33.04",{"id":397,"year":398,"html":399,"doi":11},1118647,1892,"Dana, Edward Salisbury; Dana, James Dwight (1892) \u003Ci>A System of Mineralogy\u003C\u002Fi> (6th ed.). John Wiley & Sons, Inc.",{"id":401,"year":398,"html":402,"doi":11},16100575,"Cumenge (1892) in: Lacroix Bull. Muséum national d’histoire naturelle: 42. [as Bouglisite]",{"id":404,"year":405,"html":406,"doi":407},4552,1897,"Spencer, L. J. (1897) The Crystallography of Plagionite: New Crystal Forms on Stephanite, Enargite and Anglesite. \u003Ci>Mineralogical Magazine and Journal of the Mineralogical Society\u003C\u002Fi>,  11 (52) 192-197 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1180\u002Fminmag.1897.011.52.07'>doi:10.1180\u002Fminmag.1897.011.52.07\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002FMinMag\u002FVolume_11\u002F11-52-192.pdf' class='refpdflink'>\u003C\u002Fa>","10.1180\u002Fminmag.1897.011.52.07",{"id":409,"year":410,"html":411,"doi":412},102797,1904,"Hermann, P. (1904) XXIX. Ueber Anglesit von Monteponi (Sardinien). \u003Ci>Zeitschrift für Kristallographie - Crystalline Materials\u003C\u002Fi>,  39 (1) 463-504 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1524\u002Fzkri.1904.39.1.463'>doi:10.1524\u002Fzkri.1904.39.1.463\u003C\u002Fa>","10.1524\u002Fzkri.1904.39.1.463",{"id":414,"year":410,"html":415,"doi":11},16100579,"Samoiloff (1904) Zeitschrift für Kristallographie, Mineralogie und Petrographie, Leipzig: 45: 122.",{"id":417,"year":418,"html":419,"doi":11},16100580,1907,"Kolbeck (1907) Plattner's Probierk. m.d. Lötr., 7th edition, Leipzig: 241, 253. [as Weisbachit]",{"id":421,"year":422,"html":423,"doi":424},103021,1908,"Barker, Th. V. (1908) I. Untersuchungen über regelmäßige Verwachsungen. \u003Ci>Zeitschrift für Kristallographie - Crystalline Materials\u003C\u002Fi>,  45 (1) 1-59 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1524\u002Fzkri.1908.45.1.1'>doi:10.1524\u002Fzkri.1908.45.1.1\u003C\u002Fa>","10.1524\u002Fzkri.1908.45.1.1",{"id":426,"year":427,"html":428,"doi":11},16100582,1909,"Kruse (1909) Neues Jahrbuch für Mineralogie, Geologie und Paleontologie, Beil.-Bd., Heidelberg, Stuttgart: 27: 541.",{"id":430,"year":431,"html":432,"doi":433},103208,1911,"Kolb, R. (1911) IV. Vergleich von Anhydrit, Cölestin, Baryt und Anglesit in bezug auf die Veränderung ihrer geometrischen und optischen Verhältnisse mit der Temperatur. \u003Ci>Zeitschrift für Kristallographie - Crystalline Materials\u003C\u002Fi>,  49 (1) 14-61 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1524\u002Fzkri.1911.49.1.14'>doi:10.1524\u002Fzkri.1911.49.1.14\u003C\u002Fa>","10.1524\u002Fzkri.1911.49.1.14",{"id":435,"year":431,"html":436,"doi":11},16100584,"Tacconi (1911) Instituto Lombardo di Scienze e Lettere, Milan, Rendus.",{"id":438,"year":439,"html":440,"doi":441},103280,1912,"Dürrfeld, V. (1912) XXXIX. Mitteilungen aus dem mineralogischen Institut der Universität Straßburg. \u003Ci>Zeitschrift für Kristallographie - Crystalline Materials\u003C\u002Fi>,  50 (1) 582 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1524\u002Fzkri.1912.50.1.582'>doi:10.1524\u002Fzkri.1912.50.1.582\u003C\u002Fa>","10.1524\u002Fzkri.1912.50.1.582",{"id":443,"year":439,"html":444,"doi":11},16100585,"Cesaro, G. (1912) L'Anglesite de Sardaigne. Mémoires Société géologique de Belgique, Liége, 39, 239—268.",{"id":446,"year":447,"html":448,"doi":11},4468623,1913,"(1913) \u003Ci>Atlas Der Krystallformen\u003C\u002Fi> Vol. 1 - Text - Band I - Adamin-Buntkupfererz. Carl Winters Universitätsbuchhandlung, Heidelberg.",{"id":450,"year":451,"html":452,"doi":11},16100588,1916,"Kraus, Peck (1916) Neues Jahrbuch für Mineralogie, Geologie und Paleontologie, Heidelberg, Stuttgart: II: 17.",{"id":454,"year":455,"html":456,"doi":11},16100589,1919,"Shannon, E.V. (1919) Anglesite from the Coeur d'Alene district, Idaho. American Journal of Science: 47(280): 287-292.",{"id":458,"year":459,"html":460,"doi":11},16100590,1920,"Shannon, E.V. (1920) Notes on anglesite, anthophyllite, calcite, datolite, sillimanite, stilpnomelane, tetrahedrite and triplite. Proceedings of the United States National Museum: 58(2345): 437–453.",{"id":462,"year":463,"html":464,"doi":465},103606,1923,"Ungemach, Μ. Η. (1923) VIII. Sur les formes cristallines de notation compliquée. \u003Ci>Zeitschrift für Kristallographie - Crystalline Materials\u003C\u002Fi>,  58 (1) 150-171 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1524\u002Fzkri.1923.58.1.150'>doi:10.1524\u002Fzkri.1923.58.1.150\u003C\u002Fa>","10.1524\u002Fzkri.1923.58.1.150",{"id":467,"year":463,"html":468,"doi":469},103625,"Ehringhaus, A., Rose, H. (1923) XXV. Über die Abhängigkeit der relativen Dispersion der Doppelbrechung vom Atomgewicht. \u003Ci>Zeitschrift für Kristallographie - Crystalline Materials\u003C\u002Fi>,  58 (1) 460-477 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1524\u002Fzkri.1923.58.1.460'>doi:10.1524\u002Fzkri.1923.58.1.460\u003C\u002Fa>","10.1524\u002Fzkri.1923.58.1.460",{"id":471,"year":463,"html":472,"doi":473},103636,"Maier, Adolf (1923) III. Kristallographische Beschreibung einiger Mineralien von der Eisenbläue bei Schönau im Wiesental (Baden) \u003Ci>Zeitschrift für Kristallographie - Crystalline Materials\u003C\u002Fi>,  58 (1) 75-107 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1524\u002Fzkri.1923.58.1.75'>doi:10.1524\u002Fzkri.1923.58.1.75\u003C\u002Fa>","10.1524\u002Fzkri.1923.58.1.75",{"id":475,"year":463,"html":476,"doi":477},103649,"(1923) XIV. Auszüge: Besprechungen von P. Niggli unter Mitwirkung von Κ. Faesy. \u003Ci>Zeitschrift für Kristallographie - Crystalline Materials\u003C\u002Fi>,  59 (1) 251 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1524\u002Fzkri.1923.59.1.251'>doi:10.1524\u002Fzkri.1923.59.1.251\u003C\u002Fa>","10.1524\u002Fzkri.1923.59.1.251",{"id":479,"year":480,"html":481,"doi":11},16100595,1924,"Billows (1924) Atti. Accad. Ven.-Trent.-Istr., Padova: 14: 82.",{"id":483,"year":484,"html":485,"doi":11},16100596,1925,"Hlawatsch (1925) Annalen des kaiserlich-königlichen naturhistorischen Hofmuseums Wien: 38: 19.",{"id":487,"year":484,"html":488,"doi":11},16100597,"James, R.W., Wood W.A. (1925) The crystal structure of barytes, celestine and anglesite. Proceedings of the Royal Society of London: 109A: 598-620.",{"id":490,"year":491,"html":492,"doi":493},103832,1926,"Basche, W., Mark, H. (1926) I. Über die Struktur von Verbindungen des Typus MeXO4. \u003Ci>Zeitschrift für Kristallographie - Crystalline Materials\u003C\u002Fi>,  64 (1) 1-70 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1524\u002Fzkri.1926.64.1.1'>doi:10.1524\u002Fzkri.1926.64.1.1\u003C\u002Fa>","10.1524\u002Fzkri.1926.64.1.1",{"id":495,"year":491,"html":496,"doi":11},16100599,"Shannon, S. (1926) National Museum Bulletin: 131: 444.",{"id":498,"year":499,"html":500,"doi":11},16100600,1929,"Hintze, C. (1929) Handbuch der Mineralogie. Berlin and Leipzig. 6 volumes: 1(3B): 3962.",{"id":502,"year":503,"html":504,"doi":505},104457,1931,"Heide, F. (1931) Über Deformationen an Kristallen bei erhöhtem Druck und erhöhter Temperatur. \u003Ci>Zeitschrift für Kristallographie - Crystalline Materials\u003C\u002Fi>,  78 (1) 257-278 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1524\u002Fzkri.1931.78.1.257'>doi:10.1524\u002Fzkri.1931.78.1.257\u003C\u002Fa>","10.1524\u002Fzkri.1931.78.1.257",{"id":507,"year":508,"html":509,"doi":11},520086,1933,"Swartzlow, Carl (1933) Note on the alteration of galena to anglesite to cerussite. \u003Ci>American Mineralogist\u003C\u002Fi>,  18 (4) 174-175 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM18\u002FAM18_174.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":511,"year":508,"html":512,"doi":11},16100602,"Nisi, H. (1933) The Raman Spectra of Anhydrite and Anglesite. Proceedings of the Physico-Mathematical Society of Japan. 3rd Series: 15(12): 463-469.",{"id":514,"year":515,"html":516,"doi":11},16100604,1935,"Himmel, Schroeder (1935) Centralblatt für Mineralogie, Geologie und Paleontologie, Stuttgart: 114.",{"id":518,"year":519,"html":520,"doi":11},16100605,1938,"Saldanha (1938) Bol. Univ. São Paulo: 8, no. 1.",{"id":522,"year":523,"html":524,"doi":11},16100606,1947,"Ramdohr (1947) Abh. deutsch. Ak. Wiss. Berlin, no. 4: 1. [Barytoanglesite]",{"id":526,"year":527,"html":528,"doi":11},1118652,1951,"Palache, Charles; Berman, Harry; Frondel, Clifford (1951) \u003Ci>The System of Mineralogy\u003C\u002Fi> (7th ed.) Vol. 2 - Halides, Nitrates, Borates, Carbonates, Sulfates, Phosphates, Arsenates, Tungstates, Molybdates, Etc. John Wiley and Sons.",{"id":530,"year":531,"html":532,"doi":11},526378,1974,"Blount, Charles W. (1974) Synthesis of barite, celestite, anglesite, witherite, and strontianite from aqueous solutions. \u003Ci>American Mineralogist\u003C\u002Fi>,  59 (11-12) 1209-1219 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM59\u002FAM59_1209.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":534,"year":535,"html":536,"doi":11},527050,1978,"Miyake, Michihiro, Minato, Ichiro, Morikawa, Hideki, Iwai, Shin-ichi (1978) Crystal structures and sulphate force constants of barite, celestite, and anglesite. \u003Ci>American Mineralogist\u003C\u002Fi>,  63 (5-6) 506-510 \u003Ca target='_blank' href='http:\u002F\u002Fwww.minsocam.org\u002Fammin\u002FAM63\u002FAM63_506.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":538,"year":539,"html":540,"doi":541},16384739,1996,"Nikolić, P.M., Mihajlović, P., Todorović, D.M. (1996) Far infrared and infrared properties of single crystal anglesite. \u003Ci>Spectrochimica Acta Part A: Molecular and Biomolecular Spectroscopy\u003C\u002Fi>, 52 (2) 131-137 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1016\u002F0584-8539(95)01530-2'>doi:10.1016\u002F0584-8539(95)01530-2\u003C\u002Fa>","10.1016\u002F0584-8539(95)01530-2",{"id":543,"year":544,"html":545,"doi":11},16104975,1998,"Jacobsen, Steven D., Smyth, Joseph R., Swope, R. Jeffrey, Downs, Robert T. (1998) Rigid-Body Character of the SO4 Groups in Celestine, Anglesite and Barite. \u003Ci>The Canadian Mineralogist\u003C\u002Fi>,  36 (4) 1053-1060 \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fuploads\u002FCM36_1053.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":547,"year":548,"html":549,"doi":550},348420,2002,"Majzlan, J., Navrotsky, A., Neil, J.M. (2002) Energetics of anhydrite, barite, celestine, and anglesite: a high-temperature and differential scanning calorimetry study. \u003Ci>Geochimica et Cosmochimica Acta\u003C\u002Fi>,  66 (10) 1839-1850 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1016\u002Fs0016-7037(01)00881-x'>doi:10.1016\u002Fs0016-7037(01)00881-x\u003C\u002Fa>","10.1016\u002Fs0016-7037(01)00881-x",{"id":552,"year":553,"html":554,"doi":555},149444,2003,"Frost, Ray L., Kloprogge, J. Theo, Williams, Peter A. (2003) Raman spectroscopy of lead sulphate-carbonate minerals – implications for hydrogen bonding. \u003Ci>Neues Jahrbuch für Mineralogie - Monatshefte\u003C\u002Fi>,  2003 (12) 529-542 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1127\u002F0028-3649\u002F2003\u002F2003-0529'>doi:10.1127\u002F0028-3649\u002F2003\u002F2003-0529\u003C\u002Fa>","10.1127\u002F0028-3649\u002F2003\u002F2003-0529",{"id":557,"year":558,"html":559,"doi":11},16962896,2005,"(2005) Anglesite. \u003Ci>Handbook of Mineralogy\u003C\u002Fi>. Mineralogical Society of America \u003Ca target='_blank' href='https:\u002F\u002Fwww.handbookofmineralogy.org\u002Fpdfs\u002Fanglesite.pdf' class='refpdflink'>\u003C\u002Fa>",{"id":561,"year":562,"html":563,"doi":564},395626,2007,"Lane, M. D. (2007) Mid-infrared emission spectroscopy of sulfate and sulfate-bearing minerals. \u003Ci>American Mineralogist\u003C\u002Fi>,  92 (1) 1-18 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam.2007.2170'>doi:10.2138\u002Fam.2007.2170\u003C\u002Fa> \u003Ca target='_blank' href='https:\u002F\u002Frruff.info\u002Fdoclib\u002Fam\u002Fvol92\u002FAM92_1.pdf' class='refpdflink'>\u003C\u002Fa>","10.2138\u002Fam.2007.2170",{"id":566,"year":562,"html":567,"doi":568},11619775,"Wolthoorn, Anke, Kuitert, Simon, Dijkman, Henk, Huisman, Jacco L. (2007) Application of Sulfate Reduction for the Biological Conversion of Anglesite to Galena. \u003Ci>Advanced Materials Research\u003C\u002Fi>, 20. 197-200 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.4028\u002Fwww.scientific.net\u002Famr.20-21.197'>doi:10.4028\u002Fwww.scientific.net\u002Famr.20-21.197\u003C\u002Fa>","10.4028\u002Fwww.scientific.net\u002Famr.20-21.197",{"id":570,"year":571,"html":572,"doi":573},7889386,2008,"Schröder-Wolthoorn, Anke, Kuitert, Simon, Dijkman, Henk, Huisman, Jacco L. (2008) Application of sulfate reduction for the biological conversion of anglesite (PbSO4) to galena (PbS). \u003Ci>Hydrometallurgy\u003C\u002Fi>, 94 (1). 105-109 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1016\u002Fj.hydromet.2008.05.025'>doi:10.1016\u002Fj.hydromet.2008.05.025\u003C\u002Fa>","10.1016\u002Fj.hydromet.2008.05.025",{"id":575,"year":576,"html":577,"doi":578},2430223,2009,"Jehlička, J., Vítek, P., Edwards, H.G.M., Hargreaves, M. D., Čapoun, T. (2009) Fast detection of sulphate minerals (gypsum, anglesite, baryte) by a portable Raman spectrometer. \u003Ci>Journal of Raman Spectroscopy\u003C\u002Fi>, 40 (8). 1082-1086 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.1002\u002Fjrs.2246'>doi:10.1002\u002Fjrs.2246\u003C\u002Fa>","10.1002\u002Fjrs.2246",{"id":580,"year":581,"html":582,"doi":583},396956,2012,"Antao, S. M. (2012) Structural trends for celestite (SrSO4), anglesite (PbSO4), and barite (BaSO4): Confirmation of expected variations within the SO4 groups. \u003Ci>American Mineralogist\u003C\u002Fi>,  97 (4) 661-665 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam.2012.3905'>doi:10.2138\u002Fam.2012.3905\u003C\u002Fa>","10.2138\u002Fam.2012.3905",{"id":585,"year":586,"html":587,"doi":588},397872,2015,"Keim, Maximilian F., Markl, Gregor (2015) Weathering of galena: Mineralogical processes, hydrogeochemical fluid path modeling, and estimation of the growth rate of pyromorphite. \u003Ci>American Mineralogist\u003C\u002Fi>,  100 (7) 1584-1594 \u003Ca target='_blank' href='https:\u002F\u002Fdoi.org\u002F10.2138\u002Fam-2015-5183'>doi:10.2138\u002Fam-2015-5183\u003C\u002Fa>","10.2138\u002Fam-2015-5183",[590,600,607,612,620,630,639,646,655,663,670,677,686,693,698,706,713,721,729,735,744,751,758,764,772,780,787,792,797,805,813,822,829,837,845,850,856,861],{"id":591,"source_url":592,"license_code":593,"credit_html":594,"title":595,"description":596,"author":597,"original_width":598,"original_height":599},1430,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=8762982","CC BY-SA 3.0","Didier Descouens, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=8762982\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Anglésite-touizit Monocristal.jpg","Anglesite - Touissit, Touissit District, Oujda-Angad Province, Oriental Region, Morocco - 4.7x2.3cm","Didier Descouens",4375,2645,{"id":601,"source_url":602,"license_code":603,"credit_html":604,"title":7,"description":11,"author":11,"original_width":605,"original_height":606},29093,"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F65184","CC BY-SA 4.0","Photo: Unknown author — http:\u002F\u002Fcreativecommons.org\u002Flicenses\u002Fby-sa\u002F4.0\u002F, courtesy of \u003Ca href=\"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F65184\" rel=\"noopener\">The Estonian Museum of Natural History\u003C\u002Fa> via Europeana",945,1000,{"id":608,"source_url":609,"license_code":603,"credit_html":610,"title":7,"description":11,"author":11,"original_width":606,"original_height":611},29094,"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F65181","Photo: Unknown author — http:\u002F\u002Fcreativecommons.org\u002Flicenses\u002Fby-sa\u002F4.0\u002F, courtesy of \u003Ca href=\"https:\u002F\u002Fgeocollections.info\u002Ffile\u002F65181\" rel=\"noopener\">The Estonian Museum of Natural History\u003C\u002Fa> via Europeana",913,{"id":613,"source_url":614,"license_code":593,"credit_html":615,"title":616,"description":617,"author":597,"original_width":618,"original_height":619},33004,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=8762532","Didier Descouens, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=8762532\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Anglésite-touizit.jpg","Anglesite - Touissit, Touissit District, Oujda-Angad Province, Oriental Region, Morocco - 5x4cm",3823,2854,{"id":621,"source_url":622,"license_code":623,"credit_html":624,"title":625,"description":626,"author":627,"original_width":628,"original_height":629},1433,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=12432435","CC0 1.0","Géry PARENT, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=12432435\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Anglesite 1.jpg","anglesite : Bou Bekker (Bou Becker), Touissit, Touissit District, Oujda-Angad Province, Oriental Region, Morocco","Géry PARENT",4011,2577,{"id":631,"source_url":632,"license_code":593,"credit_html":633,"title":634,"description":635,"author":636,"original_width":637,"original_height":638},33005,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10138598","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10138598\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Anglesite-113492.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAnglesite\" class=\"extiw\" title=\"en:Anglesite\">Anglesite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FTouissit\" class=\"extiw\" title=\"en:Touissit\">Touissit\u003C\u002Fa>, Touissit District, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FOujda\" class=\"extiw\" title=\"en:Oujda\">Oujda-Angad Province\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FOrient_(disambiguation)\" class=\"extiw\" title=\"en:Orient (disambiguation)\">Oriental Region\u003C\u002Fa>, Morocco (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-2402.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 2.8 x 1.6 x 0.5 cm.\u003C\u002Fdd>\n\u003Cdd>A superb, gemmy crystal of Moroccan anglesite - complete all around, with a perfect termination - just a bit of edge wear on the sides.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","Robert M. Lavinsky",419,600,{"id":640,"source_url":641,"license_code":623,"credit_html":642,"title":643,"description":626,"author":627,"original_width":644,"original_height":645},1434,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=12432575","Géry PARENT, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=12432575\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Anglesite 2.jpg",2685,3977,{"id":647,"source_url":648,"license_code":603,"credit_html":649,"title":650,"description":651,"author":652,"original_width":653,"original_height":654},1436,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=113716238","Koreller, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=113716238\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Muséum de Nantes - 021 - Anglésite (Maroc).jpg","Anglésite, en provenance du Maroc, au Muséum de Nantes","Koreller",2116,1120,{"id":656,"source_url":657,"license_code":603,"credit_html":658,"title":659,"description":660,"author":652,"original_width":661,"original_height":662},33013,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=113721568","Koreller, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=113721568\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Muséum de Nantes - 282 - Anglésite (Italie).jpg","Anglésite, en provenance d'Italie, au Muséum de Nantes",2712,2552,{"id":664,"source_url":665,"license_code":603,"credit_html":666,"title":667,"description":660,"author":652,"original_width":668,"original_height":669},33014,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=113721570","Koreller, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=113721570\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Muséum de Nantes - 283 - Anglésite (Italie).jpg",2792,2728,{"id":671,"source_url":672,"license_code":603,"credit_html":673,"title":674,"description":660,"author":652,"original_width":675,"original_height":676},33015,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=113721571","Koreller, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=113721571\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Muséum de Nantes - 284 - Anglésite (Italie).jpg",4272,2848,{"id":678,"source_url":679,"license_code":593,"credit_html":680,"title":681,"description":682,"author":683,"original_width":684,"original_height":685},33017,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=163316697","HolDu, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=163316697\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Anglesit-38498.JPG","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAnglesite\" class=\"extiw\" title=\"en:Anglesite\">Anglesite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Weight: 174,2g\u003C\u002Fdd>\n\u003Cdd>Locality: Marienberg, Erzgebirge, Germany\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>","HolDu",4058,2091,{"id":687,"source_url":688,"license_code":593,"credit_html":689,"title":690,"description":682,"author":683,"original_width":691,"original_height":692},33018,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=163316718","HolDu, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=163316718\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Anglesit-38498 2.JPG",4735,2908,{"id":694,"source_url":695,"license_code":593,"credit_html":696,"title":697,"description":682,"author":683,"original_width":684,"original_height":685},33019,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=163316728","HolDu, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=163316728\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Anglesit-38498 1.jpg",{"id":699,"source_url":700,"license_code":593,"credit_html":701,"title":702,"description":703,"author":636,"original_width":704,"original_height":705},1431,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10150647","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10150647\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Anglesite-Duftite-174037.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAnglesite\" class=\"extiw\" title=\"en:Anglesite\">Anglesite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FDuftite\" class=\"extiw\" title=\"en:Duftite\">Duftite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Tsumeb Mine (Tsumcorp Mine), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FTsumeb\" class=\"extiw\" title=\"en:Tsumeb\">Tsumeb\u003C\u002Fa>, Otjikoto (Oshikoto) Region, Namibia (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-2428.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 4.6 x 3.5 x 1.2 cm.\u003C\u002Fdd>\n\u003Cdd>A fine, well-terminated anglesite crystal with fine luster! The back of the crystal is coated with Duftite. Ex. Willy Israel Collection.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",400,339,{"id":707,"source_url":708,"license_code":593,"credit_html":709,"title":710,"description":711,"author":636,"original_width":712,"original_height":638},1432,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10453701","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10453701\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Anglesite-Cerussite-mun05-145c.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAnglesite\" class=\"extiw\" title=\"en:Anglesite\">Anglesite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FCerussite\" class=\"extiw\" title=\"en:Cerussite\">Cerussite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FTouissit\" class=\"extiw\" title=\"en:Touissit\">Touissit\u003C\u002Fa>, Touissit District, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FOujda\" class=\"extiw\" title=\"en:Oujda\">Oujda-Angad Province\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FOrient_(disambiguation)\" class=\"extiw\" title=\"en:Orient (disambiguation)\">Oriental Region\u003C\u002Fa>, Morocco (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-2402.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: cabinet, 11 x 5.3 x 3.8 cm\n\u003Cdl>\u003Cdt>Anglesite with Cerussite\u003C\u002Fdt>\u003C\u002Fdl>\u003C\u002Fdd>\n\u003Cdd>I cannot rave enough about this one! This is a very impressive matrix specimen which combines the best of two secondary lead minerals, anglesite and, to a lesser extent, cerussite. I have never seen, in all my years selling, such a fine matrix specimen of the lemony yellow anglesite from this mine for sale on the open market. I also haven't seen any of the lemony hue with cerussite in association. Now, I have seen the more typical, paler colored anglesite in both cases...but not anglesite with the top color as you see here. Gemmy, sulphur yellow, lustrous crystals of anglesite, with one monster 7 cm across, abound on this specimen. There is admittedly damage to some terminations on the periphery (and hence the price is not over 10k) but the display core of the piece is pristine and you see the COLOR and crystal form first, without the eye being drawn to the edges. Adding to the mix are gemmy, lustrous, slightly smoky, cerussite crystals, some, v-twinned, measuring 1.0 cm across. As you can imagine, for such soft minerals, there are minor contacts around the periphera, but this is still ONE major rock. THe elegance of the combination is really quite striking and as I have said above, I have never seen a similar specimen for sale in my time.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",384,{"id":714,"source_url":715,"license_code":593,"credit_html":716,"title":717,"description":718,"author":636,"original_width":719,"original_height":720},33006,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10145844","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10145844\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Linarite-Anglesite-Galena-149540.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FLinarite\" class=\"extiw\" title=\"en:Linarite\">Linarite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAnglesite\" class=\"extiw\" title=\"en:Anglesite\">Anglesite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FGalena\" class=\"extiw\" title=\"en:Galena\">Galena\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Blanchard Mine (Portalas-Blanchard Mine), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FBingham\" class=\"extiw\" title=\"en:Bingham\">Bingham\u003C\u002Fa>, Hansonburg District, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FSocorro_County,_New_Mexico\" class=\"extiw\" title=\"en:Socorro County, New Mexico\">Socorro County\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FNew_Mexico\" class=\"extiw\" title=\"en:New Mexico\">New Mexico\u003C\u002Fa>, USA (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-3993.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 2.6 x 2.1 x 2 cm.\u003C\u002Fdd>\n\u003Cdd>The true holy grail of the famous Blanchard Mine is the highly sought-after Linarite. The world’s greatest find of Linarite came from there in 1980, and it is been a target ever since. This Galena cube has a very rich coating of deep-blue Linarite on two of its faces, and one crystal is about .2-.3 cm in length. A lovely and choice thumbnail.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",500,404,{"id":722,"source_url":723,"license_code":593,"credit_html":724,"title":725,"description":726,"author":727,"original_width":728,"original_height":676},1435,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=33576765","Parent Géry, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=33576765\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Anglésite, galène, soufre 300-4-5394.JPG","crystals of anglesite, crystals of galena, crystals of sulfur : Touissit, Touissit District, Oujda-Angad Province, Oriental Region, Morocco","Parent Géry",4288,{"id":730,"source_url":731,"license_code":593,"credit_html":732,"title":733,"description":718,"author":636,"original_width":719,"original_height":734},33007,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10145845","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10145845\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Linarite-Anglesite-Galena-149541.jpg",401,{"id":736,"source_url":737,"license_code":603,"credit_html":738,"title":739,"description":740,"author":741,"original_width":742,"original_height":743},1437,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146206963","TomWG00, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=146206963\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Lapworth Museum of Geology - Anglesite on Galena.jpg","A specimen of Anglesite (lead sulphate) on Galena (lead sulphide)","TomWG00",3024,4032,{"id":745,"source_url":746,"license_code":593,"credit_html":747,"title":748,"description":749,"author":636,"original_width":750,"original_height":719},33008,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10154599","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10154599\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Linarite-Brochantite-Anglesite-187702.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FLinarite\" class=\"extiw\" title=\"en:Linarite\">Linarite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FBrochantite\" class=\"extiw\" title=\"en:Brochantite\">Brochantite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAnglesite\" class=\"extiw\" title=\"en:Anglesite\">Anglesite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FGalena\" class=\"extiw\" title=\"en:Galena\">Galena\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Blanchard Mine (Portalas-Blanchard Mine), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FBingham\" class=\"extiw\" title=\"en:Bingham\">Bingham\u003C\u002Fa>, Hansonburg District, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FSocorro_County,_New_Mexico\" class=\"extiw\" title=\"en:Socorro County, New Mexico\">Socorro County\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FNew_Mexico\" class=\"extiw\" title=\"en:New Mexico\">New Mexico\u003C\u002Fa>, USA (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-3993.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 4.3 x 4.0 x 2.4 cm.\u003C\u002Fdd>\n\u003Cdd>A classic and aesthetic Blanchard Mine pseudomorph and combination specimen. A 2.2 cm galena cube jauntily set in quartz matrix is altering to anglesite, which in turn is brilliantly coated with rich, royal-blue linarite and green brochantite.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",436,{"id":752,"source_url":753,"license_code":593,"credit_html":754,"title":755,"description":749,"author":636,"original_width":756,"original_height":757},33009,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10154600","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10154600\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Linarite-Brochantite-Anglesite-187703.jpg",486,459,{"id":759,"source_url":760,"license_code":593,"credit_html":761,"title":762,"description":763,"author":683,"original_width":691,"original_height":692},21991,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=163316509","HolDu, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=163316509\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Anglesit, Zdenekit, Segnitit, Skorodit-36740.JPG","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAnglesite\" class=\"extiw\" title=\"en:Anglesite\">Anglesite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FZden%C4%95kite\" class=\"extiw\" title=\"en:Zdenĕkite\">Zdenĕkite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FSegnitite\" class=\"extiw\" title=\"en:Segnitite\">Segnitite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FScorodite\" class=\"extiw\" title=\"en:Scorodite\">Scorodite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Weight: 365 g\u003C\u002Fdd>\n\u003Cdd>Locality: Mine Golosina, Villaricos, Almeria, Spain\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",{"id":765,"source_url":766,"license_code":593,"credit_html":767,"title":768,"description":769,"author":636,"original_width":770,"original_height":771},11817,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10174558","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10174558\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Hydrocerussite-Anglesite-290656.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FHydrocerussite\" class=\"extiw\" title=\"en:Hydrocerussite\">Hydrocerussite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAnglesite\" class=\"extiw\" title=\"en:Anglesite\">Anglesite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Tsumeb Mine (Tsumcorp Mine), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FTsumeb\" class=\"extiw\" title=\"en:Tsumeb\">Tsumeb\u003C\u002Fa>, Otjikoto (Oshikoto) Region, Namibia (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-2428.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 8.4 x 6.4 x 5.4 cm.\u003C\u002Fdd>\n\u003Cdd>A superb specimen from the Ed Swoboda Pseudomorph Collection. It has snow-white pseudomorphs of hydrocerussite after sharp blocky, pyramidal anglesite crystals from Tsumeb. The second is rare enough; the replacement I cannot say I have seen another as good in this style. It is so sharp it looks carved. The large crystal is 3.7 cm. Very rare in this size and quality. Probably one of the finest hydrocerussite pseudomorphs around. Ex. Rob Smith Collection.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",465,433,{"id":773,"source_url":774,"license_code":593,"credit_html":775,"title":776,"description":777,"author":683,"original_width":778,"original_height":779},15175,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=164380490","HolDu, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=164380490\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Mahnertit, Anglesit, Mimetesit, Segnitit, Skorodit-36-31 1.JPG","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMahnertite\" class=\"extiw\" title=\"en:Mahnertite\">Mahnertite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAnglesite\" class=\"extiw\" title=\"en:Anglesite\">Anglesite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMimetite\" class=\"extiw\" title=\"en:Mimetite\">Mimetite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FSegnitite\" class=\"extiw\" title=\"en:Segnitite\">Segnitite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FScorodite\" class=\"extiw\" title=\"en:Scorodite\">Scorodite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Weight: 14.3 g\u003C\u002Fdd>\n\u003Cdd>Locality: Golosina Mine, Villaricos, Almeria, Spain\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",2652,1950,{"id":781,"source_url":782,"license_code":593,"credit_html":783,"title":784,"description":777,"author":683,"original_width":785,"original_height":786},15176,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=164380551","HolDu, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=164380551\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Mahnertit, Anglesit, Mimetesit, Segnitit, Skorodit-36-31 2.JPG",5184,3888,{"id":788,"source_url":789,"license_code":593,"credit_html":790,"title":791,"description":777,"author":683,"original_width":785,"original_height":786},15177,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=164380619","HolDu, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=164380619\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Mahnertit, Anglesit, Mimetesit, Segnitit, Skorodit-36-31 3.jpg",{"id":793,"source_url":794,"license_code":593,"credit_html":795,"title":796,"description":763,"author":683,"original_width":691,"original_height":692},21992,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=163316540","HolDu, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=163316540\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Anglesit, Zdenekit, Segnitit, Skorodit-36740 2.JPG",{"id":798,"source_url":799,"license_code":593,"credit_html":800,"title":801,"description":802,"author":683,"original_width":803,"original_height":804},21993,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=168436351","HolDu, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=168436351\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Mimetesit, Segnitit, Anglesit, Jarosit-36733 2.JPG","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMimetite\" class=\"extiw\" title=\"en:Mimetite\">Mimetite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FSegnitite\" class=\"extiw\" title=\"en:Segnitite\">Segnitite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAnglesite\" class=\"extiw\" title=\"en:Anglesite\">Anglesite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FJarosite\" class=\"extiw\" title=\"en:Jarosite\">Jarosite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Mine Golosina, Villaricos, Almeria, Spain\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",3812,2829,{"id":806,"source_url":807,"license_code":593,"credit_html":808,"title":809,"description":810,"author":636,"original_width":811,"original_height":812},33982,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10153470","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10153470\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Arsentsumebite-Anglesite-181548.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FArsentsumebite\" class=\"extiw\" title=\"en:Arsentsumebite\">Arsentsumebite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAnglesite\" class=\"extiw\" title=\"en:Anglesite\">Anglesite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Tsumeb Mine (Tsumcorp Mine), \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FTsumeb\" class=\"extiw\" title=\"en:Tsumeb\">Tsumeb\u003C\u002Fa>, Otjikoto (Oshikoto) Region, Namibia (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-2428.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 4.5 x 4.0 x 2.4 cm.\u003C\u002Fdd>\n\u003Cdd>A significantly rich specimen just loaded with arsentsumebite crystals on anglesite.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",800,734,{"id":814,"source_url":815,"license_code":623,"credit_html":816,"title":817,"description":818,"author":819,"original_width":820,"original_height":821},35295,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=163478482","Nessa Eull, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=163478482\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Corkite with beaverite and anglesite (GeoDIL number - 648).jpg","This sample contains green corkite, PbFe(PO4)(SO4)(OH)6, yellow-olive beaverite, PbCu(Fe,Al)2(SO4)2(OH)6, and gray-white anglesite, PbSO4.","Nessa Eull",2326,1914,{"id":823,"source_url":824,"license_code":593,"credit_html":825,"title":826,"description":827,"author":636,"original_width":811,"original_height":828},36404,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10137861","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10137861\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Boleite-Paratacamite-Anglesite-74813.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FBoleite\" class=\"extiw\" title=\"en:Boleite\">Boleite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FParatacamite\" class=\"extiw\" title=\"en:Paratacamite\">Paratacamite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAnglesite\" class=\"extiw\" title=\"en:Anglesite\">Anglesite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Amelia Mine, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FSanta_Rosal%C3%ADa\" class=\"extiw\" title=\"en:Santa Rosalía\">Santa Rosalía (El Boleo)\u003C\u002Fa>, Boleo District, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FMuleg%C3%A9_(municipality)\" class=\"extiw\" title=\"en:Mulegé (municipality)\">Municipio de Mulegé\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FBaja_California_Sur\" class=\"extiw\" title=\"en:Baja California Sur\">Baja California Sur\u003C\u002Fa>, Mexico (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-5565.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Boleite specimens are fairly common and most of them are on unattractive matrix. Not so for this specimen which has a thin, drusy, sparkling, crust of greenish-blue, paratacamite, acting as the host for several boleite crystals, to .6 cm across. The intensely colored boleite crystals are so blue, that the smaller ones appear as transparent sapphire-like gems. RARE on hard, anglesite=rich matrix! Not many were found that were on such matrix as opposed to the usual friable claylike material. Acquired from Arizona dealer Evan Jones personal collection. 6.9 x 5.7 x 3.5 cm\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",706,{"id":830,"source_url":831,"license_code":593,"credit_html":832,"title":833,"description":834,"author":636,"original_width":835,"original_height":836},56040,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10166822","Robert M. Lavinsky, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=10166822\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Anglesite-Galena-249200.jpg","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAnglesite\" class=\"extiw\" title=\"en:Anglesite\">Anglesite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FGalena\" class=\"extiw\" title=\"en:Galena\">Galena\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Locality: Monteponi Mine, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FIglesias\" class=\"extiw\" title=\"en:Iglesias\">Iglesias\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FProvince_of_Carbonia-Iglesias\" class=\"extiw\" title=\"en:Province of Carbonia-Iglesias\">Carbonia-Iglesias Province\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FSardinia\" class=\"extiw\" title=\"en:Sardinia\">Sardinia\u003C\u002Fa>, Italy (\u003Ca rel=\"nofollow\" class=\"external text\" href=\"http:\u002F\u002Fwww.mindat.org\u002Floc-2135.html\">Locality at mindat.org\u003C\u002Fa>)\u003C\u002Fdd>\n\u003Cdd>Size: 4.8 x 4.0 x 3.0 cm.\u003C\u002Fdd>\n\u003Cdd>Water-clear, glassy anglesite blades to 1.0 cm are attractively set in a vug of massive, specular galena on this showy old-time piece from a classic Italian locality - Monteponi in Sardinia. Highly representative of the species and historic locale. Accompanied by an expertly handwritten, faded label from an older collection. The collection this came out of was a museum stash dating to prior to World War I.\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",700,577,{"id":838,"source_url":839,"license_code":593,"credit_html":840,"title":841,"description":842,"author":683,"original_width":843,"original_height":844},78649,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=170619304","HolDu, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=170619304\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Schulenbergit, Anglesit-27773 1.JPG","\u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FSchulenbergite\" class=\"extiw\" title=\"en:Schulenbergite\">Schulenbergite\u003C\u002Fa>, \u003Ca href=\"https:\u002F\u002Fen.wikipedia.org\u002Fwiki\u002FAnglesite\" class=\"extiw\" title=\"en:Anglesite\">Anglesite\u003C\u002Fa>\n\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>\u003Cdl>\u003Cdd>Weight: 6,9 g\u003C\u002Fdd>\n\u003Cdd>Locality: Friedrichssegen Mine, Bad Ems, Rhineland-Palatinate, Germany\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>\u003C\u002Fdd>\u003C\u002Fdl>",3254,2580,{"id":846,"source_url":847,"license_code":593,"credit_html":848,"title":849,"description":842,"author":683,"original_width":785,"original_height":786},78650,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=170619362","HolDu, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=170619362\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Schulenbergit, Anglesit-27773 2.JPG",{"id":851,"source_url":852,"license_code":593,"credit_html":853,"title":854,"description":802,"author":683,"original_width":803,"original_height":855},78796,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=168436274","HolDu, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=168436274\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Mimetesit, Segnitit, Anglesit, Jarosit-36733 1.JPG",2564,{"id":857,"source_url":858,"license_code":593,"credit_html":859,"title":860,"description":802,"author":683,"original_width":785,"original_height":786},78797,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=168437406","HolDu, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=168437406\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Mimetesit, Segnitit, Anglesit, Jarosit-36733 5.JPG",{"id":862,"source_url":863,"license_code":593,"credit_html":864,"title":865,"description":802,"author":683,"original_width":866,"original_height":867},78798,"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=168450956","HolDu, via \u003Ca href=\"https:\u002F\u002Fcommons.wikimedia.org\u002F?curid=168450956\" rel=\"noopener\">Wikimedia Commons\u003C\u002Fa>","Mimetesit, Segnitit, Anglesit, Jarosit-36733 3.JPG",3949,2980,[869,875,879,883],{"id":870,"url":871,"label":872,"formula":873,"spacegroup":874,"year":581},595,"\u002Fcif\u002F595.cif","Antao 2012","Pb S O4","P b n m",{"id":876,"url":877,"label":878,"formula":873,"spacegroup":874,"year":544},596,"\u002Fcif\u002F596.cif","Jacobsen 1998",{"id":880,"url":881,"label":882,"formula":873,"spacegroup":874,"year":535},597,"\u002Fcif\u002F597.cif","Miyake 1978",{"id":884,"url":885,"label":886,"formula":887,"spacegroup":888,"year":484},598,"\u002Fcif\u002F598.cif","James 1925","Pb S","P n m a",[890,891,892,893,894,895,896,897,898,899,900,901],"Anglésine","Lead mineralized by vitriolic acid","Lead sulphate","Lead Vitriol","Plomb sulfaté","Plumbum acido vitriolico mineralisatum","Sardinian","Sulphate of Lead","Vitriol de Plomb","Vitriolbleierz","Vitriolo nativo de plomo","Weisbachit",[903,910,914,918,922,926,930,935,939,942,946,950,955,959,967,970,973,977,981,984,988,991,994,997,1001,1004,1008,1011,1014,1018,1023,1028,1031,1034,1038,1041,1044,1048,1051,1055,1059,1062,1065,1068,1071,1075,1078,1081,1084,1087],{"lang":904,"names":905},"ar",[906,907,908,909],"أنغلزيت","أنغليزيت","انجلزيت","انجليزيت",{"lang":911,"names":912},"az",[913],"Anqlezit",{"lang":915,"names":916},"be",[917],"Англезіт",{"lang":919,"names":920},"bg",[921],"Англезит",{"lang":923,"names":924},"ca",[925],"anglesita",{"lang":927,"names":928},"da",[929],"Anglesit",{"lang":931,"names":932},"de",[929,933,934,899],"Blei(II)-sulfat","Bleivitriol",{"lang":936,"names":937},"el",[938],"Αγγλεσίτης",{"lang":940,"names":941},"es",[925],{"lang":943,"names":944},"et",[945],"anglesiit",{"lang":947,"names":948},"eu",[949],"Anglesita",{"lang":951,"names":952},"fa",[953,954],"آنگلزیت","انگلزیت",{"lang":956,"names":957},"fi",[958],"Anglesiitti",{"lang":960,"names":961},"fr",[962,890,963,964,894,965,966],"7446-14-2","Anglésite","Barytoanglésite","Vitriol de plomb","Vitriol de plomb natif",{"lang":968,"names":969},"hr",[929],{"lang":971,"names":972},"hu",[929],{"lang":974,"names":975},"it",[976],"anglesite",{"lang":978,"names":979},"ja",[980],"硫酸鉛鉱",{"lang":982,"names":983},"kk",[921],{"lang":985,"names":986},"kk-arab",[987],"انگلەزىيت",{"lang":989,"names":990},"kk-cn",[987],{"lang":992,"names":993},"kk-cyrl",[921],{"lang":995,"names":996},"kk-kz",[921],{"lang":998,"names":999},"kk-latn",[1000],"Anglezït",{"lang":1002,"names":1003},"kk-tr",[1000],{"lang":1005,"names":1006},"ko",[1007],"황산연",{"lang":1009,"names":1010},"ky",[921],{"lang":1012,"names":1013},"mk",[921],{"lang":1015,"names":1016},"nb",[1017],"anglesitt",{"lang":1019,"names":1020},"nds",[929,1021,1022],"Blievitriol","Vitriolblieierz",{"lang":1024,"names":1025},"nl",[1026,1027],"anglesiet","Loodspaat",{"lang":1029,"names":1030},"nn",[1017],{"lang":1032,"names":1033},"oc",[949],{"lang":1035,"names":1036},"pl",[1037],"Anglezyt",{"lang":1039,"names":1040},"pt",[925,7],{"lang":1042,"names":1043},"ru",[921],{"lang":1045,"names":1046},"sh",[1047],"Anglezit",{"lang":1049,"names":1050},"sk",[929],{"lang":1052,"names":1053},"sl",[1054],"anglezit",{"lang":1056,"names":1057},"sr",[1058],"англезит",{"lang":1060,"names":1061},"sr-ec",[921],{"lang":1063,"names":1064},"sr-el",[1047],{"lang":1066,"names":1067},"sv",[929],{"lang":1069,"names":1070},"tg",[921],{"lang":1072,"names":1073},"th",[1074],"แองกลีไซต์",{"lang":1076,"names":1077},"tly",[1054],{"lang":1079,"names":1080},"uk",[921],{"lang":1082,"names":1083},"uz",[1047],{"lang":1085,"names":1086},"vi",[929],{"lang":1088,"names":1089},"zh",[1090,1091],"鉛礬","铅矾","Q156526",{"history":1094,"applications":1098},{"markdown":1095,"model_version":1096,"prompt_version":1097,"reviewed_at":11},"The mineral now called **anglesite** spent its first half-century under a chemist's name, not a geographic one. In 1783 the English physician William Withering described it as the *vitriol of lead* — *vitriol* being the old term for any sulfate[1]. The description appeared in his *Outlines of Mineralogy*, an expanded translation of work by the Swedish chemist Torbern Bergman[1]. Withering had recognised the species in specimens from the Parys copper mine on the island of Anglesey, in north-west Wales[1][2].\n\nThe lead-vitriol label survived in mineralogical literature into the early 19th century, in German as *Bleivitriol* and in French as *plomb vitriolé*[1]. It described the chemistry honestly — a sulfate of lead — but it did not single the species out from other sulfates in the way the science of the period was beginning to demand.\n\nThat separation came in 1832, when the French mineralogist François Sulpice Beudant renamed the species *anglésine* in his treatise on mineralogy, after the type locality on Anglesey[2]. The form was later anglicised to **anglesite** and is the name the International Mineralogical Association still recognises. The Parys Mountain workings on Anglesey — a vast open copper-and-lead pit worked heavily through the 18th century — remain the type locality.","claude-opus-4-7","1.7.0",{"markdown":1099,"model_version":1096,"prompt_version":1097,"reviewed_at":11},"Anglesite is heavy and easy to smelt — three-quarters of its weight is lead. Even so, it holds only a modest place in the modern lead supply. The metal industry runs almost entirely on galena, the lead sulfide from which anglesite is itself derived by weathering[1]. Anglesite earns its keep in the oxidised upper portions of lead deposits. Those are the zones where rainwater and air have worked on galena long enough to convert it[1][2].\n\nIn two parts of the world, those oxidised zones are rich enough to mine in their own right. Anglesite has been worked as an ore of lead in large masses at deposits in Australia and Mexico[2]. There it is recovered alongside the cerussite and galena that usually accompany it. In most other localities the mineral is too disseminated to bother with. It appears in small amounts on the rims of weathered galena. The smelter only collects it when it happens to come along with the primary ore.\n\nBeyond that ore role, anglesite finds an occasional second life as a cut gemstone[2]. The crystals are clear and take a high *adamantine* polish — the diamond-like lustre prized by collectors. They are also soft and easily cleaved, so the stones stay strictly the preserve of collectors rather than the jewellery trade."]