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WORKS OF THE LATE S. L. PENFIELD PUBLISHED BY JOHN WILEY & SONS Noted on Determinative Mineralogy and Record of Mineral T ests· 8vo. Paper, 50 cents net. Tables of Minerals, Including the Uses of Minerals and Statistics of the Domestic Production. Second Edition, He Bet, 8vo, vi + 88 pages. Cloth, $1.00. REVISION. Manual of Determinative Mineralogy. With an introduction on Blowpipe Analysis, By George J. Brush, Director of the Sheffield Scientific School of Yale University. Revised and enlarged by Samuel jL Penfield. Sixteenth Edition. 8vo, x + 812 pages, including 375 figures and 57 tables for the determination of mineral species by means of simple chemical ex· periments in the wet and dry way and by their physical properties. Cloth. $4.00. IRIS - LILLIAD - Université Lille 1 TABLES OF MINERALS INCLUDING THE Uses of Minerals and Statistics of the Domestic Production BY SAMUEL LEWIS PENFIELD, M.A., LL.D. Late Professor o f Mineralogy in the Sheffield Scientific School o f Yale University, LSSS-1906 SECOND EDITION FIRST THOUSAND N E W Y O R K Jo h n w i l e y & s o n s Londbn: CHAPMAN & HALL, Limited 1907 IRIS - LILLIAD - Université Lille 1 Copyright, 1907 BY GRACE C. PENFIELD IRIS - LILLIAD - Université Lille 1 PREFACE TO FIRST EDITION. The minerals are arranged in the tables as follows: I. According to the six systems of crystallization and their prominent subdivisions, the minerals of each subdivision being arranged in accordance with the chemical classification as adopted b y D ana. II. According to the elements, emphasis being given to min­ erals which are important from an .economic standpoint. III. With reference to geological occurrence and association. Minerals are given three ranks in the tables, indicated by the type used in printing the names of the species, as follows:— (i) Minerals of the first rank are either very common, or espe­ cially important from a scientific or geological standpoint, and their names are printed in heavy type, capital letters. (2) Min­ erals which are of rather rare occurrence, including some very rare species provided they are especially important from an economic or scientific standpoint, are given a second rank, and their names are printed in heavy type, capital and small letters. (3) The names of rarer and less important species, constituting a third rank, are printed in small type. All of the important minerals (450 species) are included in the tables, and generally very rare species have been omitted, except where chemical com­ position or some pronounced features have given them special significance. The weighting of the minerals, or assignment to first, second or third rank, is an arbitrary matter, based upon the writer’s experience, but it is believed that students will appreciate this feature of the tables, enabling them almost at a glance to form some estimate of the relative importance of the several species. S. L. Penfield. M ineralogical L a b o r a t o r y o p t h e S h e f f i e l d S c i e n t i f i c S c h o o l o f Y a l e U n i v e r s i t y , 1903. PREFACE TO SECOND EDITION. T he “ Tables of Minerals” was written by Prof. Penfield in 1903 for use in connection with lectures on Descriptive Miner­ alogy in this School and has been used by successive classes since then. The present edition has been carefully revised, chiefly in the matter of bringing the statistics of mineral production down to date. Acknowledgment is gratefully made of the assist­ ance of Dr. George F. Kunz, who kindly furnished the figures for the values of the gem stones. Part III of the Tables has been rewritten and enlarged, with the purpose of making that section more useful to students who have only a slight knowledge of geology or petrology. W. E. Ford. M ineralogical L a b o r a t o r y o f t h e S h e f f i e l d S c i e n t i f i c S c h o o l o f Y a l e U n i v e r s i t y , J u n e 190 7. IRIS - LILLIAD - Université Lille 1 IRIS - LILLIAD - Université Lille 1 CONTENTS. P A R T I . A r r a n g e m e n t o p M i n e r a l s A c c o r d in g t o t h e Six S y s t e m s op C rystallization . PASS pag e Isometric System.................. 3 Monoclinic System.......................... 18 Tetragonal System........................... 1 Triclinic System.................................. 22 Hexagonal System............................ 9 Minerals which are Amorphous,'Mas­ Hexagonal-rhombohedral System.... io sive, or of Uncertain Crystallization 23 Orthorhombic System........................ J3 P A R T , I I . A r r a n g e m e n t o p t h e M i n e r a l s A c c o r d i n g t o t h e E l e m e n t s , w i t h U s e s a n d S t a t i s t i c s . Aluminium.................... T> · . t __ 28 « · .............. î8 Magnesium................... Zinc.,............ .......... Manganese................... Zirconium................ v IRIS - LILLIAD - Université Lille 1 vi CONTENTS. PART III. U s e f u A M i n e r a l s . PAGE page Abrasives.................................... Asbestos..................................... .. <8 O4 Cement....................................... 04 Clay.............................................. rn °5 Feldspar........................................ eo 66 Flint. ........................................... n 07 Fullers Earth............................. PART IV. L i s t s o f M i n e r a l s A c c o r d in g t o G e o l o g i c a l O c c u r r e n c e a n d A s s o c i a t i o n . Igneous Rocks........................... Accessory Minerals, Commonly Sedimentary Rocks.................... 75 Metamorphic Rocks................... Veins and Vein Minerals............... 76 Principal Rock-making Minerals. • 73 Minerals Resulting from Contact Metamorphism............................ 78 IRIS - LILLIAD - Université Lille 1 IRIS - LILLIAD - Université Lille 1 SYNOPSIS OF THE CHEMICAL CLASSIFICATION OF DANA. 1. Native Elements. 2. Sulphides, Selenides, Tellur ides, Arsenides, Antimonides. 3. Sulpharsenites, Sulphantimonites, Sulphobismuthites. 4. Chlorides, Bromides, Fluorides. 5. Oxides. 6. Carbonates. 7. Silicates, Titanates. 8. Niobates, Tantalates. 9. Phosphates, Arsenates, Vanadates. 10. Borates. 11. Uranates. 12. Sulphates, Chromates. 13. Tungstates, Molybdates. 2 IRIS - LILLIAD - Université Lille 1 TABLES OF MINERALS. PA R T I. ARRANGEMENT OF MINERALS ACCORDING TO TIJE SIX SYSTEMS OF CRYSTALLIZATION. N o te .— The chief object of tables of this kind is that they may serve as a guide and reference-list to accompany lectures on crystallography and descriptive mineralogy. In a measure, also, the tables may be made the basis of determinative mineralogy, for if it is discovered that a mineral crystallizes in a certain system, the list of minerals in that system may be studied and the name of the species found by. comparison either with labeled specimens or with descriptions as given in the texts referred to. ISOMETRIC SYSTEM; NORMAL GROUP. N o te .— The pyritohedral and tetrahedral groups are tabulated separately, while a few minerals belonging to the rarer plagihedral division are included in the normal group. Elements. \ T. B. * Sys. I. DIAMOND, C (perhaps tetrahedral), . 271, 3 2. GOLD, Au, always with some Ag, . • 275. ■ 14 3· S IL V E R , A g ............................................... 278, 19 4· C O P P E R , C u ................................................................ 278, 20 5- P la tin u m , P t ....................................................... 280, 25 6. Iron , F e w ith N i, b o th terrestrial and m eteoric, 281, 28 * The columns of numbers headed T. B. and Sys. refer respectively to the. pages pf D ana’s Text-Book of Mineralogy a n d System of Mineralogy o n which descriptions of the species m ay be found. 3 IRIS - LILLIAD - Université Lille 1 4 ISOMETRIC SYSTEM. Sulphides, Selenides, Tellurides. T. B. Sys. I. GALENA, Pb S, often carrying Ag, 287, 48 2. A lta ite , P b T e , .................................................................. 288, 51 3· Argentite, A g 2 S ............................................................... 288, 46 4- H essite, A g 2 T e ..................................................................... 289, 47 5· Petzite, (Ag, Au)2 Te ......................................................... 289, 48 6. Berzelianite, Cu2 S e , ........................................................ 289, 52 7· Crookesite, (Cu, Tl, Ag)2 Se............................................ 289, 54 8. Pentlandite, (Ni, F e )S ...................................................... 293. 65 9· BORNITE, Cu5 Fe S4................................................ 297, 77 10. Linnaeite, Co3 S4=CoS . Co2 S3..................................... 297, 78 / II. Argyrodite, Ag8 Ge S6= 4 A g 2 S . Ge S2, . 3i 6> i 5° 12. Canfieldite, Agg Sn S6=4 Ag 2 S . Sn S2, . 316. — Chlorides, Bromides, Fluorides. I. HALITE, Na Cl........................................ ......... 318, 154 2. SYLVITE, K Cl (plagihedral)......................................... 318, 156 3· Cerargyrite, A g C l , ......................................................... 319. 158 4· Embolite, Ag (Cl, Br)........................................................ 3i 9> *59 5· N an tokite, Cu C l , ......................................................... 3i 7> 154 6. Percylite (Boldite), Pb Cu Cl2 [0 H]2, 322, 172 7· FLUORITE, Ga F2.............................................................. 320, i6 r 8. Ralstonite (Na2, Mg) F2 . 3 A 1 (F, 0 H)3 . 2H20, . 323. i8 r Oxides. I. Arsenolite, As2 0 3, . 33° , ! 98 2. Senarmontite, S b 2 0 3, ............................................... 33° . I 98 3· CUPRITE, Cu2 0 (p lagih ed ral)..................................... 331, 206 4· Periclase, Mg 0 , ......................................................... 331 > 207 5· Manganosite, Mn 0 , . ................................................ 332, 207 Spinel Group. R"R 2'"O i or R "0 . R 2"'0 Z.
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  • Nickeline Nias C 2001-2005 Mineral Data Publishing, Version 1

    Nickeline Nias C 2001-2005 Mineral Data Publishing, Version 1

    Nickeline NiAs c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Hexagonal. Point Group: 6/m 2/m 2/m. Commonly in granular aggregates, reniform masses with radial structure, and reticulated and arborescent growths. Rarely as distorted, horizontally striated, {1011} terminated crystals, to 1.5 cm. Twinning: On {1011} producing fourlings; possibly on {3141}. Physical Properties: Fracture: Conchoidal. Tenacity: Brittle. Hardness = 5–5.5 VHN = n.d. D(meas.) = 7.784 D(calc.) = 7.834 Optical Properties: Opaque. Color: Pale copper-red, tarnishes gray to blackish; white with strong yellowish pink hue in reflected light. Streak: Pale brownish black. Luster: Metallic. Pleochroism: Strong; whitish, yellow-pink to pale brownish pink. Anisotropism: Very strong, pale greenish yellow to slate-gray in air. R1–R2: (400) 39.2–45.4, (420) 38.0–44.2, (440) 36.8–43.5, (460) 36.2–43.2, (480) 37.2–44.3, (500) 39.6–46.4, (520) 42.3–48.6, (540) 45.3–50.7, (560) 48.2–52.8, (580) 51.0–54.8, (600) 53.7–56.7, (620) 55.9–58.4, (640) 57.8–59.9, (660) 59.4–61.3, (680) 61.0–62.5, (700) 62.2–63.6 Cell Data: Space Group: P 63/mmc. a = 3.621(1) c = 5.042(1) Z = 2 X-ray Powder Pattern: Unknown locality. 2.66 (100), 1.961 (90), 1.811 (80), 1.071 (40), 1.328 (30), 1.033 (30), 0.821 (30) Chemistry: (1) (2) Ni 43.2 43.93 Co 0.4 Fe 0.2 As 55.9 56.07 Sb 0.1 S 0.1 Total 99.9 100.00 (1) J´achymov, Czech Republic; by electron microprobe, corresponds to (Ni0.98Co0.01 Fe0.01)Σ=1.00As1.00.
  • Mineralogical Chemistry

    Mineralogical Chemistry

    View Article Online / Journal Homepage / Table of Contents for this issue 282 ABSTRACTS OF CHEMICAL PAPERS. Downloaded on 22 February 2013 Published on 01 January 1900 http://pubs.rsc.org | doi:10.1039/CA9007805282 Mineralogical Chemistry. Roumanian Petroleuws. By A LFONS 0. SALIGNY(Chem. Centy., 1900, 60 ; from Bul. Bozcmccnie, 8, 351 --365).-In the original paper, the physical and chemical properties of 12 kinds of Roumanian MINERALOGICAL CHEMISTRY View Article Online283 petroleum are described and tabulated. The flash points of the various fractions are given, and their suitability for use as burning oils is also discussed. These petroleums contain very variable amounts of volatile oils, and ethylisobutane and isopropane were found in the fractions boiling below 70”. E. w. w. Melonite from South Australia. By ALFREDJ. HIGGIN(Trans. Roy. Xoc. South Austdia, 1899, 23, 21 1-212).-This mineral, pre- viously only known from California, has now been found with quartz and calcite at Worturpa, South Australia. The thin lamells have a brilliant metallic lustre; the cleavage planes are silver-white to reddish- brown. H- 1.5 ; sp. gr., 7.6. Analyses I and IT: agree with the formula Ni,Te, (compare this vol., ii, 22). Te. Xi. Au. Insol. Total. I. 74.49 22.99 0.329 2.091 99.90 11. 71.500 21.274 0.018 7*319 100.11 Traces of bismuth and lead are present. On dissolving the mineral in nitric acid, the gold is left as bright spangles. L. J. S. Titaniferous Magnetites. By JAMESF. KENP(School of Mines Quart., 1899, 20, 323-356 ; 21, 56-65).-Titaniferous magnetites, with the exception of the occnrrences in sands, are almost invariably found associated with rocks of the gabbro type, and have originated by a process of segregation from the magma, The mineral, as a rule, contains vanadium, cbromium, nickel and cobalt, which together may amount to several per cent.