CORNERSTONE Journal of the Accredited Gemologists Association

Total Page:16

File Type:pdf, Size:1020Kb

Load more

SPRING 1 9 9 6 CORNERSTONE Journal of the Accredited Gemologists Association TUCSON REPORT by David Harris This year the Tucson conference with physical properties of miner- David Johnson was our instructor was presented by the University of als as a function of structure and the remainder of the second day Arizona Geoscience Department chemistry and lab exercises to which we spent in the Santa Rita and included lectures on the funda- determine the physical properties Mountains panning for minerals. mentals of crystallography and of crystals. The final lecture of the Minerals such as pyrite, garnet, mineralogy and a fortune hunting day was presented by noted dia- and gold were found during this field trip in the mountains. mond geologist, Dr. Tom McCand- exercise, however none of the finds less, on the location of gem was large enough to prevent the DAY ONE deposits worldwide from the view- return to regular employment. Conducted by Frank Mazdab, the point of a geologist. The day ended Special thanks to all the partic- first lectures on Day One reminded at 6:30 PM with everyone going to ipants and instructors who made us how long it had been since we their rooms to digest this enor- used the periodic table and dis- mous amount of information and this a learning experience so enjoy- cussed atomic structure. Frank prepare for a day in the mountains. able. Next year we are planning started the day by passing out a another "Learning Experience in 100 page workbook filled with won- DAY TWO Tucson" in conjunction with the drous charts and tables. As he On Day Two Dr. Peter Kresan lec- University of Arizona. started his lecture, we knew we tured on the movement of tecton- After the conference, Past Presi- would receive far more than our ics forming the mountains sur- dent Joe Tenhagen presented me "moneys worth". The first day rounding the Tucson basin and how with an article that better explains included lectures on basic crystal- the various mineral deposits the type of information we dis- lography and basic crystal struc- occurred in the area in a presenta- cussed during the conference. ture followed by a hands-on labora- tion entitled, "Geology of Arizona (See page 3.) Thank you Joe, for tory. After lunch we continued and the American Cordillera". sharing this information. TOWARD A issues about gem treatments, the officers and membership "in grading standards, appraising, step" working toward a common SHARED VISION new technology, and many, many goal and objective for any signifi- By Craig Lynch more. Our industry has resolved cant length of time. I tend to some of these issues, others believe that nobody is at fault for During the 10 years I've spent as still stand without agreement this short term success that is fol- a member of the Accredited or resolution. Even in these lowed with disorganization. I Gemologists Association I've seen unresolved issues, I've found that believe that this happens primarily great benefits from belonging to the open forum provided by AGA because of slightly differing the organization. I've made many has been of significant benefit. visions of our organization. This friends and benefited from the net- However, I have noticed an on is complicated by the fact that work of good gemologists. This going problem in AGA. For some in our small organization time, organization has successfully reason, it seems that it has been money, distances between addressed many controversial almost impossible to keep all of members and physical resources (continued on page 2) AGA • CORNERSTONE • 1 SPRING 1 9 9 6 IN MEMORIUM Antonio Bonanno, founder of the Accredited Gemologists Association, AGA is a nonprofit research, education and ethics died recently after a long illness. organization, benefiting professional and avocation- In addition to the AGA, Mr. Bonanno founded the Columbia School of al gemologists as well as the consumer interest. Gemology in Washington, DC., and the National Gem Appraising Membership programs include advanced gemo- logical education seminars, professional computer Laboratory. He was a Distinguished Fellow of the Gemological software reviews and workshops, and the AGA- Association of Great Britain and Master Gemologist Appraiser of the Certified Gemological laboratory Program. American Society of Appraisers. We are grateful for his mind, his talent and the creativity he brought to his life. Think About It "Never doubt that a small group of commit- ted people can change the world. Indeed, it is CORNERSTONE very often the only thing that does. is a quarterly publication of the Accredited Gemologists Association. Paid for through Margaret Mead membership dues, this publication may not be purchased commercially. The opinions expressed within are those of the individual authors. AGA can assume no liability for (continued from page 1) these statements, which are offered entirely are in very limited supply. These "The mission statement is intend- for the purposes of informed professional limited resources seem to magnify ed to serve leaders of organiza- discourse and education. the differences in shared vision. tions as an expression of their vision and sense of stewardship. Copyright 1996, Accredited Gemologists Associa- Just how important is it to have a , tion common shared vision in an orga- It attempts to encompass in one All Rights Reserved nization? brief paragraph, the core values of Let me paraphrase Dr. Stephen the organization; it creates context For information regarding Cornerstone, that gives meaning, direction, and contact Lorraine Lopezzo at: Covey from his book Principled coherence to everything else." 41 East Mill Road, Suite 2, Centered Leadership. Long Valley, NJ 07853 "Vision is the best manifestation of Development of mission state- creative imagination and the prima- ments in the largest corporations Board of Directors ry motivation of human action. It's during the past 20 years has been President: the ability to see beyond our pre- at the core of the revolution in cor- Leo J. Schmied sent reality, to create, to invent porate culture, management style 1st Vice-President: what does not exist, to become and increased productivity as well Thom Underwood what we are not. It gives us capac- as efficiency. 2nd Vice-President: It is my belief that a well thought Joseph Du Mouchelle ity to live our imagination instead Secretary: of our memory. More than any out mission statement would be of Melinda H. Adducci other factor, vision affects the great benefit for AGA and have the Treasurer: choices we make and the way we following results: David L Harris spend our time." A mission statement will set the I would like to suggest the at the standard for short term planning Board of Governors AGA create a Mission Statement. and development and provide a Stanley P. Cohen No, not some pleasant, "feel good" consistent long range framework Therese S. Kienstra phrase to hang on the wall or put for all decisions made by the B. Young McQueen into a pamphlet. I mean a real executive board and the board of Anna M. Miller thoughtful approach to what we directors. This mission state- Larry Phillips want AGA to be, say 10 to 20 years ment also will guide and lift the Sharon Wakefield down the road. goals and objectives above and Just what is a good mission state- beyond any one administration for ment: Again, Dr. Stephen Covey... decades to me. (continued on page 8) AGA • CORNERSTONE • 2 SPRING 1 9 9 6 THE HEXAGONAL CRYSTAL SYSTEM By Joseph W. Tenhagen F.G.A., G.G., N.G.J.A. Most of you have had sufficient gemological training either from the GIA or GAGB to know that the hexagonal crystal system produces seven of the twelve principal birth stones. Whether there are six or seven crystal sys- tems is not the issue in this article; the intent is to broaden the readers depth of knowledge concerning the hexagonal crystal system. A. All crystals have a definite symmetry shown by the arrangement of their crystal faces which enables tielve,;//3 one to group them into different classes. The exter- nal crystal faces are the result of the three dimension- A/dtAtew al internal order of atoms in the crystal structure. The different types of symmetry elements in the Figure 4. hexagonal crystal system are: B. It is common to use a symmetry notation in any 1. Symmetry plane: A symmetry discussions relating to the crystal systems. In plane is an imaginary plane that Figure 1 . describing the symmetry of a crystal, it is convenient divides a crystal in half with each to use a shorthand notation for symmetry elements. half being a mirror image of the other. See Figure 1. A rotation axis is indicated by A n where n is 1-fold, 2-fold, 3-fold, or 6-fold. 2. Symmetry axis of rotation: A symme- try axis is an imagi- An axis of rotoinversion is indicated by CAR, nary line through a // where n is 1-fold, 2-fold, 3-fold, or 6-fold. crystal about which ; CD A plane of symmetry is indicated by P the crystal may be \\ A center of symmetry is indicated by C. rotated to repeat With this notation the symmetry of a crystal with itself in appearance a center of symmetry; one axis of 6-fold rotation one, two, three, or ------', symmetry; three axes of 2-fold rotation six times in a com- symmetry; and six planes of symmetry would be plete 360° rotation. 4, (;) written as: C, 1A6, 3A2, 6P. The symmetry rota- \ --- Lion axes in hexago- ‘, ,, Several of the more important gemstones crystallize lalnan nal crystals may be 3 in the hexagonal crystal system including seven of 1-fold (360°), 2-fold (180°), Fi 9 the birth stones.
Recommended publications
  • Mineral Processing

    Mineral Processing

    Mineral Processing Foundations of theory and practice of minerallurgy 1st English edition JAN DRZYMALA, C. Eng., Ph.D., D.Sc. Member of the Polish Mineral Processing Society Wroclaw University of Technology 2007 Translation: J. Drzymala, A. Swatek Reviewer: A. Luszczkiewicz Published as supplied by the author ©Copyright by Jan Drzymala, Wroclaw 2007 Computer typesetting: Danuta Szyszka Cover design: Danuta Szyszka Cover photo: Sebastian Bożek Oficyna Wydawnicza Politechniki Wrocławskiej Wybrzeze Wyspianskiego 27 50-370 Wroclaw Any part of this publication can be used in any form by any means provided that the usage is acknowledged by the citation: Drzymala, J., Mineral Processing, Foundations of theory and practice of minerallurgy, Oficyna Wydawnicza PWr., 2007, www.ig.pwr.wroc.pl/minproc ISBN 978-83-7493-362-9 Contents Introduction ....................................................................................................................9 Part I Introduction to mineral processing .....................................................................13 1. From the Big Bang to mineral processing................................................................14 1.1. The formation of matter ...................................................................................14 1.2. Elementary particles.........................................................................................16 1.3. Molecules .........................................................................................................18 1.4. Solids................................................................................................................19
  • Sugilite in Manganese Silicate Rocks from the Hoskins Mine and Woods Mine, New South Wales, Australia

    Sugilite in Manganese Silicate Rocks from the Hoskins Mine and Woods Mine, New South Wales, Australia

    Sugilite in manganese silicate rocks from the Hoskins mine and Woods mine, New South Wales, Australia Y. KAWACHI Geology Department, University of Otago, P.O.Box 56, Dunedin, New Zealand P. M. ASHLEY Department of Geology and Geophysics, University of New England, Armidale, NSW 2351, Australia D. VINCE 1A Ramsay Street, Essendon, Victoria 3040, Australia AND M. GOODWIN P.O.Bo• 314, Lightning Ridge, NSW 2834, Australia Abstract Sugilite relatively rich in manganese has been found at two new localities, the Hoskins and Woods mines in New South Wales, Australia. The occurrences are in manganese-rich silicate rocks of middle to upper greenschist facies (Hoskins mine) and hornblende hornfels facies (Woods mine). Coexisting minerals are members of the namansilite-aegirine and pectolite-serandite series, Mn-rich alkali amphiboles, alkali feldspar, braunite, rhodonite, tephroite, albite, microcline, norrishite, witherite, manganoan calcite, quartz, and several unidentified minerals. Woods mine sugilite is colour-zoned with pale mauve cores and colourless rims, whereas Hoskins mine sugilite is only weakly colour-zoned and pink to mauve. Within single samples, the chemical compositions of sugilite from both localities show wide ranges in A1 contents and less variable ranges of Fe and Mn, similar to trends in sugilite from other localities. The refractive indices and cell dimensions tend to show systematic increases progressing from Al-rich to Fe- Mn-rich. The formation of the sugilite is controlled by the high alkali (especially Li) and manganese contents of the country rock, reflected in the occurrences of coexisting high alkali- and manganese- bearing minerals, and by high fo2 conditions. KEYWORDS: sugilite, manganese silicate rocks, milarite group, New South Wales, Australia Introduction Na2K(Fe 3 +,Mn 3 +,Al)2Li3Sit2030.
  • Zincite (Zn, Mn2+)O

    Zincite (Zn, Mn2+)O

    Zincite (Zn, Mn2+)O c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Hexagonal. Point Group: 6mm. Crystals rare, typically pyramidal, hemimorphic, with large {0001}, to 2.5 cm, rarely curved; in broad cleavages, foliated, granular, compact, massive. Twinning: On {0001}, with composition plane {0001}. Physical Properties: Cleavage: {1010}, perfect; parting on {0001}, commonly distinct. Fracture: Conchoidal. Tenacity: Brittle. Hardness = 4 VHN = 205–221 (100 g load). D(meas.) = 5.66(2) D(calc.) = 5.6730 Rare pale yellow fluorescence under LW UV. Optical Properties: Translucent, transparent in thin fragments. Color: Yellow-orange to deep red, rarely yellow, green, colorless; deep red to yellow in transmitted light; light rose-brown in reflected light, with strong red to yellow internal reflections. Streak: Yellow-orange. Luster: Subadamantine to resinous. Optical Class: Uniaxial (+). ω = 2.013 = 2.029 R1–R2: (400) 13.0–13.6, (420) 12.8–13.2, (440) 12.6–12.8, (460) 12.3–12.6, (480) 12.1–12.4, (500) 12.0–12.2, (520) 11.8–12.1, (540) 11.8–12.0, (560) 11.7–11.9, (580) 11.6–11.8, (600) 11.4–11.7, (620) 11.3–11.6, (640) 11.2–11.5, (660) 11.1–11.4, (680) 11.0–11.2, (700) 11.0–11.2 Cell Data: Space Group: P 63mc (synthetic). a = 3.24992(5) c = 5.20658(8) Z = 2 X-ray Powder Pattern: Synthetic. 2.476 (100), 2.816 (71), 2.602 (56), 1.626 (40), 1.477 (35), 1.911 (29), 1.379 (28) Chemistry: (1) (2) SiO2 0.08 FeO 0.01 0.23 MnO 0.27 0.29 ZnO 99.63 98.88 Total 99.99 [99.40] (1) Sterling Hill, New Jersey, USA.
  • New Minerals Approved Bythe Ima Commission on New

    New Minerals Approved Bythe Ima Commission on New

    NEW MINERALS APPROVED BY THE IMA COMMISSION ON NEW MINERALS AND MINERAL NAMES ALLABOGDANITE, (Fe,Ni)l Allabogdanite, a mineral dimorphous with barringerite, was discovered in the Onello iron meteorite (Ni-rich ataxite) found in 1997 in the alluvium of the Bol'shoy Dolguchan River, a tributary of the Onello River, Aldan River basin, South Yakutia (Republic of Sakha- Yakutia), Russia. The mineral occurs as light straw-yellow, with strong metallic luster, lamellar crystals up to 0.0 I x 0.1 x 0.4 rnrn, typically twinned, in plessite. Associated minerals are nickel phosphide, schreibersite, awaruite and graphite (Britvin e.a., 2002b). Name: in honour of Alia Nikolaevna BOG DAN OVA (1947-2004), Russian crys- tallographer, for her contribution to the study of new minerals; Geological Institute of Kola Science Center of Russian Academy of Sciences, Apatity. fMA No.: 2000-038. TS: PU 1/18632. ALLOCHALCOSELITE, Cu+Cu~+PbOZ(Se03)P5 Allochalcoselite was found in the fumarole products of the Second cinder cone, Northern Breakthrought of the Tolbachik Main Fracture Eruption (1975-1976), Tolbachik Volcano, Kamchatka, Russia. It occurs as transparent dark brown pris- matic crystals up to 0.1 mm long. Associated minerals are cotunnite, sofiite, ilin- skite, georgbokiite and burn site (Vergasova e.a., 2005). Name: for the chemical composition: presence of selenium and different oxidation states of copper, from the Greek aA.Ao~(different) and xaAxo~ (copper). fMA No.: 2004-025. TS: no reliable information. ALSAKHAROVITE-Zn, NaSrKZn(Ti,Nb)JSi401ZJz(0,OH)4·7HzO photo 1 Labuntsovite group Alsakharovite-Zn was discovered in the Pegmatite #45, Lepkhe-Nel'm MI.
  • Download the Scanned

    Download the Scanned

    American Mineralogist, Volume 70, pages 379-387, 1985 Ma_nganesehumites and leucophoenicitesfrom Franklin and Sterling- Hill' NewJersev: 'i"? andimplications ;ifi':il1,;;lfiil11"r's' Perr J. Dullx Department of Mineral Sciences Smithsonian lnstitution, Washington, D. C. 20560 Abstract The manganesehumites, (alleghanyite, manganhumite, and sonolite),together with some Mn-bearing samplesof the Mg-humites,and the related phasesleucophoenicite and jerry- gibbsite,from the orebodiesat Franklin and SterlingHill, New Jersey,are describedtogether with analytical data. Solid solution betweenhumite and manganhumiteis at least partially continuous. Expected Mn/Mg solid solutions between alleghanyiteand chondrodite, and betweensonolite and clinohumite, are discontinuous; they are interrupted by apparently orderedphases. In all cases,the possibleorderings involve Zn as well as Mn and Mg. There are no Mn end-membersof the manganesehumites at this locality. Manganeseis apparently restricted in leucophoenicite(5.42-6.63 Mn per 7 octahedral cations) and in jerrygibbsite (7.79-8.02Mn per 9 octahedralcations). Calcium is common to both leucophoeniciteand jerrygibbsite,but among the Mn-humites,only sonoliteaccepts appreciable Ca (0.65Ca per 9 octahedralcations). There is a "threshold" level ofzinc in all studiedsamples; this "threshold" levelis a constantfor leucophoenicite1-9.3 Znper 3 Si)and alleghanyite(-O.2Zn per 2 Si). No samplesof leucophoeniciteor jerrygibbsite were found to be Zn-ftee,suggesting either that Zn is required for their stability, or that these two phasesmight not be stable as end-members.Fluorine is present in all the Mn-humites and is proportional to the Mg- content,but is absentin leucophoeniciteand jerrygibbsite. Introduction humite speciesoccur there; the Mg-humites occur in the The magnesiumhumite species(norbergite, chondrodite, host Franklin Marble for the most part, and the Mn- humite, and clinohumite) have been well-studiedand re- humites in the orebodiesthemselves.
  • The Seven Crystal Systems

    The Seven Crystal Systems

    Learning Series: Basic Rockhound Knowledge The Seven Crystal Systems The seven crystal systems are a method of classifying crystals according to their atomic lattice or structure. The atomic lattice is a three dimensional network of atoms that are arranged in a symmetrical pattern. The shape of the lattice determines not only which crystal system the stone belongs to, but all of its physical properties and appearance. In some crystal healing practices the axial symmetry of a crystal is believed to directly influence its metaphysical properties. For example crystals in the Cubic System are believed to be grounding, because the cube is a symbol of the element Earth. There are seven crystal systems or groups, each of which has a distinct atomic lattice. Here we have outlined the basic atomic structure of the seven systems, along with some common examples of each system. Cubic System Also known as the isometric system. All three axes are of equal length and intersect at right angles. Based on a square inner structure. Crystal shapes include: Cube (diamond, fluorite, pyrite) Octahedron (diamond, fluorite, magnetite) Rhombic dodecahedron (garnet, lapis lazuli rarely crystallises) Icosi-tetrahedron (pyrite, sphalerite) Hexacisochedron (pyrite) Common Cubic Crystals: Diamond Fluorite Garnet Spinel Gold Pyrite Silver Tetragonal System Two axes are of equal length and are in the same plane, the main axis is either longer or shorter, and all three intersect at right angles. Based on a rectangular inner structure. Crystal shapes include: Four-sided prisms and pyramids Trapezohedrons Eight-sided and double pyramids Icosi-tetrahedron (pyrite, sphalerite) Hexacisochedron (pyrite) Common Tetragonal Crystals: Anatase Apophyllite Chalcopyrite Rutile Scapolite Scheelite Wulfenite Zircon Hexagonal System Three out of the four axes are in one plane, of the same length, and intersect each other at angles of 60 degrees.
  • Leucophoenicite Mn (Sio4)3(OH)2

    Leucophoenicite Mn (Sio4)3(OH)2

    2+ Leucophoenicite Mn7 (SiO4)3(OH)2 c 2001 Mineral Data Publishing, version 1.2 ° Crystal Data: Monoclinic. Point Group: 2=m: Crystals rare, typically slender, prismatic, elongated and striated [010], to 8 mm; in isolated grains or granular massive. Twinning: On k 001 , common, contact or interpenetrant twins, lamellar. f g Physical Properties: Cleavage: 001 , imperfect. Tenacity: Brittle. Hardness = 5.5{6 f g D(meas.) = 3.848 D(calc.) = [4.01] Optical Properties: Transparent to translucent. Color: Brown to light purple-red, raspberry-red, deep pink to light pink; rose-red to colorless in thin section. Luster: Vitreous. Optical Class: Biaxial ({). Pleochroism: Faint; rose-red 001 ; colorless 001 . Orientation: k f g ? f g X 001 cleavage. Dispersion: r > v; slight. ® = 1.751(3) ¯ = 1.771(3) ° = 1.782(3) ? f g 2V(meas.) = 74(5)± Cell Data: Space Group: P 21=a: a = 10.842(19) b = 4.826(6) c = 11.324(9) ¯ = 103:93(9)± Z = [2] X-ray Powder Pattern: Franklin, New Jersey, USA. 1.8063 (10), 2.877 (9), 2.684 (8), 4.36 (5), 3.612 (5), 2.365 (5), 2.620 (4) Chemistry: (1) (2) (3) (1) (2) (3) SiO2 26.36 26.7 26.7 CaO 5.67 2.4 2.8 FeO trace 0.3 0.3 Na2O 0.39 MnO 60.63 62.8 64.7 K2O 0.24 ZnO 3.87 0.0 0.0 H2O 2.64 [2.3] [2.8] MgO 0.21 5.5 2.7 Total 100.01 [100.0] [100.0] (1) Franklin, New Jersey, USA; composite of two analyses, corresponding to (Mn5:89Ca0:70Zn0:32 Na0:04Mg0:03K0:01)§=6:99(Si1:01O4)3(OH)2: (2) Kombat mine, Namibia; by electron microprobe, H2O by di®erence; corresponding to (Mn5:98Mg0:92Ca0:29Fe0:02)§=7:21(SiO4)3(OH)1:72: (3) Valsesia-Valtournanche area, Italy; by electron microprobe, H2O by di®erence; corresponding to (Mn6:16Mg0:45Ca0:34Fe0:03)§=6:98(SiO4)3(OH)2:10: Mineral Group: Leucophoenicite group.
  • TEPHROITE from FRANKLIN, NEW JERSEY* Connbrrus S. Hunrsur

    TEPHROITE from FRANKLIN, NEW JERSEY* Connbrrus S. Hunrsur

    THE AMERICAN MINERALOGIST, VOL 46, MAY_JUNE, 1961 TEPHROITE FROM FRANKLIN, NEW JERSEY* ConNBrrus S. Hunrsur, Jn., Departmentof Mineralogy, Harvard, Uniaersity. Assrnlcr A study of tephroite specimens from Franklin and Sterling Hill, New Jersey showed in all of them the presence of thin sheets of willemite believed to be a product of exsolution. .fhese sheets are oriented parallel to the {100} and [010] planes of tephroite with the o and r axes of tephroite and willemite parallel. It is believed that Iittle zinc remains in the tephroite structure and that much of it reported in chemical analyses has been con- tributed by intergrown u'illemite. This conclusion is supported by experiments syn- thesizing tephroite. The indices of refraction and d spacing of {130} vary as would be expected with changes in amounts of MgO, FeO and CaO. INrnooucrroN 'fephroite, Mn2SiO4,a member of the olivine group, was describedas a new mineral from SterlingHill by Breithaupt in 1823.A chemicalanal- ysis of the original material was published by Brush (1864) together with severaladditional chemical analysesof tephroite made by others. These analysesreport ZnO in varying amounts which Brush attributed to invariably associatedzincite. Palache (1937) did not agree with Brush and stated " . that the molecularratios in someanalyses more nearly satisfy the orthosilicateformula when zinc is regardedas essen- tially a part of the mineral rather than as a constituent of mechanical inclusions." The present study was undertaken for the purpose of in- vestigatingthe variations in the propertiesof tephroite with changesin chemical composition, particularly the effect of zinc. Relationships were not expectedto be simplefor analysesshow, in addition to ZnO, variable amounts of MgO, FeO, and CaO.
  • POUDRETTEITE, Knarb3si12o3e, a NEW MEMBER of the OSUMILITE GROUP from MONT SAINT-HILAIRE, OUEBEC, and ITS CRVSTAL STRUCTURE Assr

    POUDRETTEITE, Knarb3si12o3e, a NEW MEMBER of the OSUMILITE GROUP from MONT SAINT-HILAIRE, OUEBEC, and ITS CRVSTAL STRUCTURE Assr

    Canadian Mineralogist Vol. 25, pp.763-166(1987) POUDRETTEITE,KNarB3Si12O3e, A NEW MEMBEROF THE OSUMILITEGROUP FROM MONT SAINT-HILAIRE,OUEBEC, AND ITS CRVSTALSTRUCTURE JOEL D. GRICE, T. SCOTT ERCIT AND JERRY VAN VELTHUIZEN Mineral SciencesDivision, National Museumof Natural Sciences,Ottawa, Ontario KIA 0M8 PETE J. DUNN Departmentof Mineral Sciences,Smithsonian Institution, Washington,D.C, 20560,U,S.A. Assrnact positionC d coordinanceXII, le sodium,la position,4d unecoordinance VI, le bore,la position72 ir coordinance Poudretteiteis a newmineral species from the Poudrette IV, le silicium,la position71 i coordinanceIV, etla posi- quarry, Mont Saint-Hilaire,Quebec. It occursin a marble tion B estvacante. xenolith includedin nephelinesyenite, associated with pec- tolite, apophyllite, quartz and minor aegirine.It forms clear, Mots-clds: poudrettdite, nouvelle espbce min6rale, groupe colorlessto very pale pink, equidimensional,subhedral del'osumilite, mont Saint-Hilaire, borosilicate, affi ne. prismsup to 5 mm. It is brittle, H about 5, with a splin- mentde Ia structure. tery fracture;Dmetr. 2.51(l) g/cml, D"6".2.53 g/cm3. Uniaxialpositive, co 1.516(l), e 1.532(l).It is-hexagonal, spacegroup P6/ mcc, a I 0.239(l), c 13.485(3)A and,Z : 2. INTRoDUcTIoN The strongestten X-ray-diffractionlines in the powderpat- tern [d in A(r\(hkDl are: 6.74(30)(002),5.13 (100)(110), The optical and physical propertiesof members 4.07(30)(r 12), 3.70(30)(202), 3.3 6e(30)(004), 3.253 ( I 00) of the osumilite group are similar to those of com- (2r r), 2.9s6(40)(3 00), 2.8 I 5(60)(I I 4), 2.686(50)(213,204) mon mineralssuch as quartz and cordierite;for this and 2.013(30)(321).An analysisby electron microprobe reason, they are probably generally overlooked.
  • Useful Primitive Radio Detector Minerals H.P

    Useful Primitive Radio Detector Minerals H.P

    Sheet1 Useful Primitive Radio Detector Minerals H.P. Friedichs, AC7ZL Chemical Chemical Crystal PW Eccles Toricata Morgan Mineral Composition Formula Category Suitable Contacts (1925) (1928) (1910) (1913) Allemontite Arsenic antimonide AsSb Antimonide x Anatase Titanium dioxide TiO2 Oxide Metals and Zincite x x Antimony Element Sb Element Zincite, silicon, etc. x Argentite (silver glance) Silver sulfide Ag2S Sulfide Metals, graphite, tellurium x Arkansite See Anatase x Arsenic Element As Element Metals and Zincite x x x Arsenic pyrites See Mispickel x Bornite (peacock Sulfide of copper and ore) iron Cu5FeS4 Sulfide Zincite, silicon, etc. x x x x Boron Element B Element Zincite, tellurium x x Sulfide of antimony Boulangerite and lead Pb5Sb4S11 Sulfosalt x Sulfide of copper, Zincite, tellurium, Bourmonite antimony and lead PbCuSbS3 Sulfosalt antimony, bismuth x Brookite See Anatase x x Carborundum Silicon Carbide SiC Steel, zincite x Zincite (this combination is Sulfide of iron and the famous Perikon Chalcopyrite copper CuFeS2 Sulfide detector) x x x Cobaltite Cobalt arsenic sulfide CoAsS Zincite x x Cassiterite Tin Oxide SnO2 Oxide Metals x x Cerussite Lead Carbonate PbCo3 Carbonate ?x Chalcocite (copper glance) Copper sulfide Cu2S Sulfide Zincite, tellurium x x x Zincite (this combination is Sulfide of iron and the famous Perikon Copper pyrites copper CuFeS2 Sulfide detector) x x Corundum Aluminum oxidde Al2O3 Oxide Zincite, bornite x Page 1 Sheet1 Covellite Copper sulfide CuS Sulfide Zincite, etc x x Cuprite (Cuprous oxide) Copper oxide
  • Guide to Healing Uses of Crystals & Minerals

    Guide to Healing Uses of Crystals & Minerals

    Guide to Healing Uses of Crystals & Minerals Addiction- Iolite, amethyst, hematite, blue chalcedony, staurolite. Attraction – Lodestone, cinnabar, tangerine quartz, jasper, glass opal, silver topaz. Connection with Animals – Leopard skin Jasper, Dalmatian jasper, silver topaz, green tourmaline, stilbite, rainforest jasper. Calming – Aqua aura quartz, rose quartz, amazonite, blue lace agate, smokey quartz, snowflake obsidian, aqua blue obsidian, blue quartz, blizzard stone, blood stone, agate, amethyst, malachite, pink tourmaline, selenite, mangano calcite, aquamarine, blue kyanite, white howlite, magnesite, tiger eye, turquonite, tangerine quartz, jasper, bismuth, glass opal, blue onyx, larimar, charoite, leopard skin jasper, pink opal, lithium quartz, rutilated quartz, tiger iron. Career Success – Aqua aura quartz, ametrine, bloodstone, carnelian, chrysoprase, cinnabar, citrine, green aventurine, fuchsite, green tourmaline, glass opal, silver topaz, tiger iron. Communication – Apatite, aqua aura quartz, blizzard stone, blue calcite, blue kyanite, blue quartz, green quartz, larimar, moss agate, opalite, pink tourmaline, smokey quartz, silver topaz, septarian, rainforest jasper. www.celestialearthminerals.com Creativity – Ametrine, azurite, agatized coral, chiastolite, chrysocolla, black amethyst, carnelian, fluorite, green aventurine, fire agate, moonstone, celestite, black obsidian, sodalite, cat’s eye, larimar, rhodochrosite, magnesite, orange calcite, ruby, pink opal, blue chalcedony, abalone shell, silver topaz, green tourmaline,
  • Mineral Index

    Mineral Index

    Mineral Index Abhurite T.73, T.355 Anandite-Zlvl, T.116, T.455 Actinolite T.115, T.475 Anandite-20r T.116, T.45S Adamite T.73,T.405, T.60S Ancylite-(Ce) T.74,T.35S Adelite T.115, T.40S Andalusite (VoU, T.52,T.22S), T.27S, T.60S Aegirine T.73, T.30S Andesine (VoU, T.58, T.22S), T.41S Aenigmatite T.115, T.46S Andorite T.74, T.31S Aerugite (VoU, T.64, T.22S), T.34S Andradite T.74, T.36S Agrellite T.115, T.47S Andremeyerite T.116, T.41S Aikinite T.73,T.27S, T.60S Andrewsite T.116, T.465 Akatoreite T.73, T.54S, T.615 Angelellite T.74,T.59S Akermanite T.73, T.33S Ankerite T.74,T.305 Aktashite T.73, T.36S Annite T.146, T.44S Albite T.73,T.30S, T.60S Anorthite T.74,T.415 Aleksite T.73, T.35S Anorthoclase T.74,T.30S, T.60S Alforsite T.73, T.325 Anthoinite T.74, T.31S Allactite T.73, T.38S Anthophyllite T.74, T.47S, T.61S Allanite-(Ce) T.146, T.51S Antigorite T.74,T.375, 60S Allanite-(La) T.115, T.44S Antlerite T.74, T.32S, T.60S Allanite-(Y) T.146, T.51S Apatite T.75, T.32S, T.60S Alleghanyite T.73, T.36S Aphthitalite T.75,T.42S, T.60 Allophane T.115, T.59S Apuanite T.75,T.34S Alluaudite T.115, T.45S Archerite T.75,T.31S Almandine T.73, T.36S Arctite T.146, T.53S Alstonite T.73,T.315 Arcubisite T.75, T.31S Althausite T.73,T.40S Ardaite T.75,T.39S Alumino-barroisite T.166, T.57S Ardennite T.166, T.55S Alumino-ferra-hornblende T.166, T.57S Arfvedsonite T.146, T.55S, T.61S Alumino-katophorite T.166, T.57S Argentojarosite T.116, T.45S Alumino-magnesio-hornblende T.159,T.555 Argentotennantite T.75,T.47S Alumino-taramite T.166, T.57S Argyrodite (VoU,