The following notes, in conjunction with a paper upon the

subject published in the proceedings of the Royal Society

of "Tasmania, 1897, embrace the work done to elucidate

the mineralogy of the State since the publication of the

"Minerals of Tasmania, 1896.

Petterd, William Frederick

University of Tasmania Open Access Repository

NOTES ON UNRECORDED AND OTHERMINERALS OCCURRING IN TASMANIA.7?// W. r. Petterd.The following notes, in conjunction with a paper upon thesubject published in the proceedings of the Royal Societyof "Tasmania, 1897, embrace the work done to elucidatethe mineralogy of the State since the publication of the"Minerals of Tasmania, 1896."They comprise many interesting substances of more recentdiscovery, including one, or perhaps two, which are quitenew to mineralogical science. It will be found that49 species hitherto iinknown as occurring in this Islandhave been added to the already voluminous catalogue, andadditional localities and associations are recorded for severalpreviously known. An important feature is the record ofseveral complete analyses of complex substances, for whichI am indebted to Mr. S. Pascoe, of the Magnet Silver MiningCompany, and Mr. O. E. White, of Hobart, to whom Ireturn my sincere thanks for their ready and valuable assist-ance. Such work is invariably a welcome addition tomineralogical investigation, and I am sure it will be dulyappreciated by those interested in this field of enquiry. Inmany cases it is only by such means, coupled with crystal-logi'aphic characters, that the specific identity can be attainedwith reasonable certainty. It is almost needless to say thatin this department much yet remains to be done before wecan possess a comprehensive knowledge of the mineralsknown to occur in this State.1 Analcite.—{Hydrous silicate of sodium and alu-minium.)Somewhat abundant in the haiiyne phonolite of PortCygnet.2 Anorthoclase.—(Triclinic soda-pofash-felspar.)In rhombic sections of a shining milky-white.Solvsbergites of Port Cygnet.ITNflECOEDED AND OTHEU MINEEALS IN TASMANIA. 198 Arsenopyrite.—(Sulph-a/}'senide of iron.)In peculiar minute crystal trillings implanted }ncavities in hard gossan. Magnet Mine.As minute needles abundantly scattered throughoutsiderite gangue. Block 291, E-ingville.Analysis of this Mineral.Fe = 32-95,As = 43-20,S = 21-48,97-63,with about 2 per cent, of antimony.4 AuGiTE.—(Variety of pyroxene.)The embedded crystals of the nephelinite of theShannon Tier are of a shining black colour, andoften of remarkably large dimensions, sometime*one inch and a half in length.5 Beresowite.—(Chromate and carbonate of lead.)Occurs as small, in many cases almost microscopic,lamellae implanted in gossan. The colour variesfrom pale yellow to orange-red. It is sometimeschanged to crocoisite. Magnet Mine.6 Beryl.—(Metasilicate of beryllium and alntninium.)At the Shepherd and Murphy Mine, Bell Mount,specimens have occurred several inches in length,wholly changed to gilbertite, fluor, and chlorite.At the same locality small slender crystals havebeen met with of a pale green colour, intermixedwith quartz, topaz, molybdenite, and cassiterite.The crystals are commonly embedded in a thinfilm of pyrite.7 BouRNONiTE.—(Sulphantimonite of lead- and copper.)In bright well-developed orthorhombic crystals, whichgave the following result upon analysis :—S = 13 62 per cent.Sb = 28-68Pb = 42-39Cu = 11-93Fe = 1-9798-40UNRECORDED AND OTHER MINERALS8 Brijcite.—(^Magnesium hydrate^Radiating, massive, and white, near the workings,Mt. Bischoff.9 Calcite.—(Carbonate of calcium.)Some remarkably fine crystals have been obtained atthe Mt. Lyell limestone flux quarry at Queens-town. (H. W. Judd.)10 Campylite.—(Lead arsenate.)In very characteristic barrel-shaped crystals aggre-gated together. The colour is very pale, almostwhite. Britannia Mine, Zeehan.11 Carminite.—(Arsenate of lead and iron.)In minute orthorhombic groups of crystals coatingfractures and vughs in gossan. It is of a reddishcolour, and adamantine lustre. The MagnetSilver Mine.12 Cassiterite.—(Dioxide of tin.)Pseudomorphous after orthoclase. * Mt. Bex Mine,Ben Lomond.13 Cerussite.—(Carbonate of lead.)Analysis of the characteristic form of a yellowish-green colour from the Adelaide Proprietary Mine,Dundas, by Mr. J. C. H. Mingaye, F.C.S., ofSydney, N.S.W. :—PbOCO,c^o^GangueOCCURRING IN TASMANIA. 21In slugs up to many pounds in weight, associated withnative copper, at the King Lyell Mine. (H. W.Judd.)16 Clinochlore.—{Basic magnesium and aluminimnsilicate.)In large masses and occasionally crystalline bunchesof a pale metallic green colour. Near Mt.Heemskirk.Abundant in fine groups of hexagonal crystals of adark olive-green to black colour. The plates areoften over one inch in diameter. Near theHampshire Hills Silver Mine, Hampshire Hills.At Anderson's Creek in minute, almost microscopic,radiating bunches of a dark colour. (W. H.Twelvetrees.)17 Chlorite.—{Basic silicate of magnesium and alu-minium.)In schist, and as beautiful bright green fan-shapedcrystals in honey-combed quartz—Crown LyellMine—species undetermined. (H. W. Judd.)Occurs pseudomorphous after felspar—Block 4891-93m, Ben Lomond. (Waller, ''Report on the BenLomond District," 1901.)18 CopiAPiTE.—{Hydrous basic ferric sulphate.)Results from the decomposition of pyrites, ColebrookMine, Ringville, Khaki Mine, Whyte River, and atBarn Bluff. The rock from the last-named locality,when freshly broken out, soon becomes coated withthis and other sulphates.19 Crocoisite.—{Chromate of lead.)Rare as small crystals in gossan at the Silver QueenMine and at the Colonel North Mine, Zeehan. (H.W. Judd.)A full detailed description of the typical and well-known Dundas occurrence of this beautifulmineral, by C. Palache, may be found in the" American Journal of Science " for 1896, page389. ^^UNRECOKDKD AND OTHER MINERALS20 Deweylite.—{Hydrous basic iiiagnesiuni silicate.)In thin seams, sometimes reaching a foot in width,traversing serpentine. Harman's Rivulet, nearthe Parson's Hood Mountain.21 Dolomite.—{Carbonate of calcium and magnesium)Analysis of the pure white form from the MagnetMine. (F. O. Hill.)Ca 31 "72 per cent. = Ca Co 3 56*64 per cent.Mg O 15-60 „ = Mg C03 32-76Fe 3-92 ,. = Fe Co, 8*26Mn 1-80 „ = Mn C03 3-76101-4222 DuNDASiTE.—{Hydrous carbonate of lead and alu-minium.)" Minerals of Tasmania," 1896, page 33.Dana, " First Appendix to the Sixth Edition of theSystem of Mineralogy," page 23.The following is a complete analysis of this newspecies :—Pb = 38-84 per cent = Pb O 41-86AU O3 26-06Fe = 3-85 „ = Fe', O3 5-50H/O + Co^ 28-08101-50Mr. Pascoe states that the Fcg and O3, or a portionthereof, may be foreign to the substance, as it isnext to impossible to perfectly separate it, since italmost invariably occurs as an incrustation on themineral from the original locality at Dundas. Atrace of P 3 O 3 was also found ; this was certainlyobtained from an extremely thin coating or skinof pyromorphite, which is often present, and givesan external green colouration to the surface of themineral. At the Hercules Mine, Mt. Read, amass of snow-white cellular quartz has beenobtained, throughout which are scattered crystalsof cerussite, gibbsite, and numerous patches ofdundasite, the whole forming one of the mostattractive associations of minerals as yet obtainedin this State.OCCUERING IN TASMANIA. 2323 DuFREYNOYSiTE.—(Sulpharseuite of lead.)Analysis :—Pb24'INK'KOORDKl* AND OIHKH MINERALS28 GiBBSiTE.—[Hydrate of ahnniniuin.')Apparently abundant in botryoidal masses, associatedwith native copper and earthy lode-material. Itvaries in colour from clear pellucid glassy to palegreen, and more rarely to golden yellow with abronze lustre. It decomposes to a white powder.Rio Tinto Mine, Savage River.29 Gmelinite.—{Hydrous sodium, calcium, and alu-miniuTn silicate.^3^ fine lot of perfect crystals of this zeolite have beenobtained loose and coating a vugli in Tertiarybasalt at Bell Mount. Middlesex.30 Hauynite.—{Sodiu7n, calcium, and aluminium or-thosilicate with sodium sidphate.)In micro-crystals sparingly in the fayalite-melilitebasalt f]'om One Tree Point, near flobart.31 Hematite.—{Sesquioxide of iron.)At Zeehan this occurs pseudomorphous after cubicalpyrites. (R. F. Waller.)32 Histeixite.—(Sulphide of antimony and bismuth.)An apparently new substance occurring in radiatinggroups of prismatic crystals, which are occasionallyin confused bunches, and commonly stained ex-ternally with a dark brown coating. The crystalsare orthorhombic, with acute but indistinct ter-minations, and striated longitudinally. Theysometimes reach over 2 in. in length by | in. inwidth. Slightly sectile, with a hardness of about2. Lustre eminently metallic, shining on freshcrystalline surfaces. Colour and streak, steel-grey.When massive, it presents a foliated structure, andtarnishes to blue and purple iridescent colouration.The crystals occurred interpenetrating a vughfrom a bedding of a mixture of iron and copperpyrites. It was found in a somewhat massivebody of tetrahedrite, with which were associatedbismuthinite and pyrites, and appeared to te ofvery exceptional occurrence.OCCURRING IN TASMANIA. 25Kesult of two analyses of the pure material: —S =2405 S =23-01Bi = 55-93 Bi = 56-08Sb = 10-08 Sb = 9-33Cu= 6-86 Cu= 6-12Fe = 5-18 Fe = 5-44102-10 99-98Answering to the formula—7 Bi^ S3 + 2 Sb, S3 + 5 Cu Fe S,(Locality, No. 1 Curtin-Davis Mine, Ringville.)33 HuASCOLiTE.—(Sulphide of lead and zinc.)A massive, fine-grained, dark-coloured and somewhatdull substance—Comstock Mine. Zeehan.34 HYDROMAGNES ITE.—(Basic carhonate of magnesium.)Occurs in solid, almost white, radiating bunches—Comstock Mine. Zeehan.35 Hypersthene.—(Magnesium and iron metasilicate.)In basalt. Circular Head; in granite, St. Mary'sPass.36 Jamiesonite.—(Sulfhantimonite of lead.)Analysis of a sample from the Magnet Mine :—= 0*12 per cent, = 39 ozs. 4 dwts. 10 grs. per ton.Ag26 UNRECORDED AND OTHEK MINERALSAnalysis of a columnar and striated sample from Mt.Bischoff :—Ag = 012Pb = 32-08As = traceSb = 26-74Fe = 5-56S = 17-82Si 02=14-28Al = trace96-6037 JoHNSTONOTiTE.—(A new mcmgancse garnet. Pro.Roy. Soc, Tas., 1898-99.)Occurs abundantly distributed in the mica-solvsber-gite of Port Cygnet. The cavities containing thegarnet are often lined with a thin coating ofpurple fluor and arsenical pyrites.38 Knoxvillite.—{Hydrous basic sulphate of chromium,iron, and aluminimn.)Occurs as a granular sugar-like substance of a palegreen colour. From adit at the Victoria GoldMine, Salisbury.Analysis :—OCCURRING IN TASMANIA. 27followingAn28 UNRECOHDRD AND OTHER .MINKRALS45 MiLLERiTE.—(Sulphide of 7iick(l.)In the characteristic capillary patches in quartz,with pentlandite—near the Colebrook Mine.Ringville.46 MONAZITE. (Phosphate of cerium metals.)This mineral has been obtained in a fine granularform in alluvial at the following localities, in ad-dition to those quoted in the " Minerals of Tas-mania " :—Stanley River, South Esk Tin Mine(Ben Lomond), Briseis Tin Mine (Derby), thePioneer Tin Mine (Mt. Stronach), and at theKhaki Mine at the foot of the Meredith Range).47 Natrolite.—(Hydrous sodium and aluminium sili-cate.)Somewhat abundant in massive pure white massesand pockets, which often exhibit distinct rhombiccrystals agglutinated together, Nephelinite,Shannon Tier.48 Nephelite.—(Orthosilicate of sodium, potassium, andaluminium..)In microscopic crystals, as an essential constituentin the nephelinite of the Shannon River.49 NoNTRONiTE.—(Hydrated iron silicate.)A green variety of chloropal. Occurs of a pale yel-low-green colour. Middlesex.50 OsMiRiDiUM. (Iridium and osmium in varying pro-portio7is.)A fine nugget of this substance was recently obtainedin the Whyte River, near its junction with thePieman. The specific gravity was 19-5, andweight 60 grains.51 Pectolite.—(Metasilicate of sodium and calcite.)Occurs in fibrous radiating bunches of a pure whitesilkv subvitreous lustre—Upper Emu River. W.R. Bell.52 Penninite.—(Basic silicate of magnesium, aluminium,and iron.)In dark, almost olive-green, masses and crystals, thelatter sometimes over |'/ across. It is invariablyassociated with quartz—Tharsis Copper Mine.Mt. Lyell.OCCURRING IN TASMANIA. 2953 Perofskite.—(Tifanite of calcium.)Microscopical crystals in the melilite basalt of theShannon Tier.54 Petterdite.—{A new oxychloride of lead. Fro.Royal Soc, Tas., 1901.)Occurs implanted and in bunches of pseudo-hexa-gonal crystals—Britannia Mine. Zeehan.55 Pharmacosiderite.—(Hydrous basic iron arsenate.)Found as coatings of microscopic cubic crystals of anintensely green colour and bright lustre—MagnetMine. (R. F. Waller.)56 Phosgenite.—(Chlorocarbonate of lead.)Some fine adamantine crystals of this somewhat raremineral have been obtained at the Comet Mine,Dundas, with anglesite and cerussite.57 PiCOTiTE.—(Aluminafe of inagnesium and chrome.)Chrome spinel is stated to occur in the vicinity ofZeehan. (Krause, "_ Mineralogy," p. 245.) Abun-dant in the alluvial of the Heazlewood River.58 Prosopite.—{Hydrous fluoride of aluminium andcalcium.)Occurs as a granular powder, and often kaolinised.It is associated with decomposed green tourmaline(zeuxite), which is so characteristic of Mt. BischoffTin Mine.59 Rhodonite.—{Metasilicate of manganese.)Massive^ in a somewhat impure form as a boulderin a large asbestos seam in serpentine on theground leased to the Australasian Asbestos Com-pany at Anderson's Creek, west of Beaconsfield.Called "red quartz" by the miners. (W. H.Twelvetrees.)60 Saponite.—(Hydrous magnesium and cduminiumsilicate.)Occurs in patches of a yellow to brown colour andglimmering lustre, with chrome ochre and quartzon the hanging-wall of a reef at the Duchess ofYork Mine, Salisbury.White and amorphous at Trial Harbour. WestCoast.30 UNRECORDED AND OTHER MINERALS61 ScAPOLiTE.— (Hydrous silicate of alu7ninium and cal-cium.^This mineral was found as loosened rounded bouldersin a seam of asbestos occurring in the serpentine atAnderson's Creek, near Beaconsfield. It was mis-taken by the miners for quartz, which it somewhatresembles. It has, however, a slightly greenishtinge, and its hardness is only between 5 and 6. Itis soluble with difficulty in HCl.Microscopical characters.—Confusedly crystalline,with the larger crystal faces obscurely divergent.The crystals often form rosettes. Double refrac-tion, strong ; interference colours higher thanquartz; extinction straight in longitudinal sec-tions; no sensible absorption.Scapolite is mostly found in schists and gneiss. Italso occurs in amphibolites and ophites. When itis found in gabbro, it has been derived fromfelspar, and this may have been the case here,though there is some reason to believe that theserpentine was originally pyroxenite. Scapolite isundeniably a secondary mineral, and was hereformed during the hydro-metamorphic process ofserpentinisation. (W. II. Twelvetrees.)62 ScHEELiTE.—(Tungstate of calcium.)Analysis of a sample of this mineral from Mt. Ram-say :—W O2 = 79-77M O3 = traceCa O = 19 6599-42(Dana, ' System, of Mineralogy," page 987.)63 ScHROTTERiTE.—{Hydfous aluminium silicate.)A soft brittle white to honey-yellow coloured gum-like substance, occurring as an incrustation andin patches in a fissure in Silurian slate. It decom-poses to a white powder. Occasionally it is stalac-titic or mamillated, and easily falls to pieces.Obtained near the Pieman River.OCCUKRING IN TASMANIA. 3164 SiEGENiTE.—{Sulphide of cobalt and nickel.)Occurs massive, of a steel-grey colour, intermixedwith magnetite, pyrite, and niccolite. RockyRiver Mine.65 SoDALiTE.—{GhiorOS Hicat e of sodium and aluminium.)In the elaeolite syenite of Port Cygnet, changed tonatrolite.66 Spodumene.—(^Aluminium and lithium metasilicate.)Variety, triphane.Several thin flakes of this substance have beenobtained in alluvial tin workings near Mt. Cameron,with quartz, topaz, and sapphire. It is of the verycharacteristic yellow-green colour, and quite indis-tinguishable from the clear samples found inBrazil. It might easily be mistaken for a varietyof corundum—Oriental topaz—or even quartz ; infact, it is highly probable that it is more abundantthan supposed, but has been overlooked from itsresemblance to the minerals mentioned. Someminute bright green specks in granite from Ring-arooma are probably the same mineral.67 Stilbite.—(Hydrous sodium, calcium, and aluminiumsilicate.)In large radiating masses of a yellow-brown colourimbedded in basalt vitrophyre. Bell Mount,Middlesex.68 Strigovite.—(A basic silicate of iron and aluminium:)A chlorite-like mineral consisting of a black shiningaggregate of minute plates, in the fractures decom-posed to brown. Occurs as a narrow band a fewinches wide in granite—near the Great RepublicTin Mine. Ben Lomond.69 Stromeyerite.—(Sulphide of copper and silver.)Analysis of an amorphous slug from the Mt. LyellMine :—Ag = 13-80 = 4507 ozs. 19 dwts. 23 s^rs. per tonPb = 1-60Cu32 UNRECORDED AND OTIIKR MINKRALS70 SuLPHcm.—(Native.)Found ill minute blebs on crystallised and othergalenite. Magnet Mine.71 Symplesite.—(Hydrous iron arsenate.)Occurs thickly coating gossan in small radiating blue-green tufts, of great attractiveness under the lens.Magnet Mine.72 Tennantite.—(Sulpharsenite of copjjer.)Analysis of a sample from No. 4 adit, Mt. LyellMine :—Ag-OCCUERING IN TASMANIA. 8376 Variscite.—(Hydrous phosphate of aluminhim.)As incrustations, often with a uniform surface.General character somewhat dull, but of a brightemerald-green colour, and thus sometimes mistakenfor an ore of copper.Associated with wavellite. Back Creek.Implanted in the cleavages of quartz. Lefroy.77 VoLTZiTE.—{Oxysulphide of zinc.)Formed as an incrustation of a thin lamellar struc-ture and globular; colour, clove-brown. Very-Rare. Silver Crown Mine, Zeehan.78 Wavellite.—{Hydrous basic phosphate of alu-?niniu7n.)Occurs in small white discs, with the characteristicradiating structure implanted in the cleavages ofsandstone. Ballast Quarry, Zeehan—ComstockLine.79 Wolfram.—(Tungstate of iron and manganese.)An unusual occurrence 'df this mineral is in smallpatches, associated with stannite and pyrite, at theOonah Mine. Zeehan.Occurs in the form of small brown crystals in quartz.Mt. Bischoff Mine.80 Zeuxite.—{A ferriferous tourmaline.)A peculiar variety of tourmaline of a dark greencolour, of remarkable habit. It is confined to andcharacteristic of the tin-deposits of Mt. Bischoff,where it occurs in great abundance, often formingrock masses of considerable size. Its common habitis in short acicular crystals, which are interlacedtogether into irregular bunches. Both colour andhabit are very constant.

Notes on unrecorded and other minerals occurring in Tasmania

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Notes on unrecorded and other minerals occurring in Tasmania

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