29 Amethyst Absorption Spectrum – Amherst Stone Amethyst Absorption Spectrum; Absorption Spec- Amethyst Inclusions; ® Inclusion in Amethyst
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Download PDF About Minerals Sorted by Mineral Name
MINERALS SORTED BY NAME Here is an alphabetical list of minerals discussed on this site. More information on and photographs of these minerals in Kentucky is available in the book “Rocks and Minerals of Kentucky” (Anderson, 1994). APATITE Crystal system: hexagonal. Fracture: conchoidal. Color: red, brown, white. Hardness: 5.0. Luster: opaque or semitransparent. Specific gravity: 3.1. Apatite, also called cellophane, occurs in peridotites in eastern and western Kentucky. A microcrystalline variety of collophane found in northern Woodford County is dark reddish brown, porous, and occurs in phosphatic beds, lenses, and nodules in the Tanglewood Member of the Lexington Limestone. Some fossils in the Tanglewood Member are coated with phosphate. Beds are generally very thin, but occasionally several feet thick. The Woodford County phosphate beds were mined during the early 1900s near Wallace, Ky. BARITE Crystal system: orthorhombic. Cleavage: often in groups of platy or tabular crystals. Color: usually white, but may be light shades of blue, brown, yellow, or red. Hardness: 3.0 to 3.5. Streak: white. Luster: vitreous to pearly. Specific gravity: 4.5. Tenacity: brittle. Uses: in heavy muds in oil-well drilling, to increase brilliance in the glass-making industry, as filler for paper, cosmetics, textiles, linoleum, rubber goods, paints. Barite generally occurs in a white massive variety (often appearing earthy when weathered), although some clear to bluish, bladed barite crystals have been observed in several vein deposits in central Kentucky, and commonly occurs as a solid solution series with celestite where barium and strontium can substitute for each other. Various nodular zones have been observed in Silurian–Devonian rocks in east-central Kentucky. -
Tiger's Eye Is Not a Pseudomorph Glenn Morita in the Early 1800’S, Mineralogists Recognized That Tiger’S Eye Was a Fibrous Variey of Quartz
Minutes of the 05/20/03 Westside Board Meeting VP Stu Earnst opened the meeting at 7:31pm. Treasurer’s report read by Kathy Earnst. Minutes approved as published in the newsletter. Old business: Lease on Walker valley discussed. The expiration notice was sent but we are not sure who it went to. We do not see any obstacle to renewal as communication between the council and DNR are open and ongoing. Special thanks, to DNR representative, Laurie Bergvall and DNR staff for their time and effort in hearing our concerns and working towards mutually beneficial solutions on the Walker Valley issues. Sign production is on hold until the sign committee decides where and what the signs will say. We have decided that they will not be on the gate but separate from it. There will be a gate going up at Walker Valley but we will have access to that lock and it will probably be a combo type of thing that we can easily give to other rockhound clubs going there. Talked about the possibility of posing the combo on website but that will depend on the type of gate they put up and what ends up being possible with the mechanics of that gate. New business: Thank you from Bob Pattie and Ed Lehman to Bruce Himko and AAA Printing for donation of the paper. Thank you to Danny Vandenberg for providing sample Walker Valley Material to DNR to show the value of the material we are trying to preserve and enjoy. Bob Pattie is pursuing with the retrieval of our state seized funds through the unclaimed property process. -
Download the Scanned
THn ArrERrcAN M rlrERA LocIST JOURNAL OF THE MINERALOGICAL SOCIETY OF AMERICA Vol. 50 ]ANUARY-FEBRUARY. 1965 Nos. 1 and 2 STUDIES OF THE TORBERNITE MINERALS (III): ROLE OF THE INTERLAYER OXONIUM, POTASSIUM, AND AMMONIUM IONS, AND WATER MOLECULES1 Mercorlt Ross Ar.rnH. T. EvaNs, Jn., LI. S. GeologicalSuraey, Wash,i,ngton,D. C. Alstnact Structural and chemical evidence is given to show that solid-solution series probably exist in the torbernite mineral group between the foliowing pairs of end members: K(UOzAsOa)'3I{:O (abernathyite) and H3O(UOrAsOD.3HzO (troegerite),K(UOrPO' '3HzO (meta-ankoleite) and HaO(UOzPO4).3HrO, NH+(UOzAsOd.3HzO and lroegerite, and NHr(UOzPOt '3HrO (uramphite) and H:O(UO:PO ) '3HrO. These seriesare erpressed by the formula A,_u(ttro)u(uorxo4).3H,o r,vhereA:K+ or NHa+, and X:As or P. Other possiblesolid-solution seriesare also given. The structures of K(UOzAsOa).3HzO (abernathyite), NHr(UOzAsOr)'3HzO, K(HrO)(UO:AsOa)z'6HrO, and Cu(UOrPOr)r'SHzO (meta-torbernite) are related to other torbernite minerals and possible structural similarities are suggested. The role of the interlayer cations and water moleculesin the torbernite minerals is related to other mineral groups including the zeolites, the feldspars and micas, the clay minerals, the jarosites and alunites, and the clathrate compounds. It is predicted that the distribution of the cations H3O+, K+, and NHr+ over the ll'ater molecules sites observed in the abernathyite-like compounds may be a common feature of the interlayer structure of the hydrous layer sili- cates and of the intercage structure of the zeolites and clathrate compounds The specia- nature of the oxonium ion in hvdrous structures is discussed. -
The Hydrous Component in Andradite Garnet
American Mineralogist, Volume 83, pages 835±840, 1998 The hydrous component in andradite garnet GEORG AMTHAUER* AND GEORGE R. ROSSMAN² Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California 91125, U.S.A. ABSTRACT Twenty-two andradite samples from a variety of geological environments and two syn- thetic hydroandradite samples were studied by Fourier transform IR spectroscopy. Their 2 spectra show that H enters andradite in the form of OH . Amounts up to 6 wt% H2O occur in these samples; those from low-temperature formations contain the most OH2. Some 42 ↔ 42 features in the absorption spectra indicate the hydrogarnet substitution (SiO4) (O4H4) whereas others indicate additional types of OH2 incorporation. The complexity of the spectra due to multi-site distribution of OH2 increases with increasing complexity of the garnet composition. 42 ↔ 42 INTRODUCTION tution (O4H4) (SiO4) . This observation has been Systematic studies have shown that hydroxide is a con®rmed by XRD of a hydrous andradite with a Si de- common minor component of grossular and pyrope-al- ®ciency of about 50%, and a high OH content (Arm- mandine-spessartite garnets (Aines and Rossman 1985; bruster 1995). The structure of this particular sample with Rossman and Aines 1991). Comparable surveys of an- space group Ia3d is composed of disordered microdo- dradite garnet have not been previously presented. Sev- mains containing (SiO4) and (O4H4) tetrahedral units. eral reports indicate that appreciable amounts of OH2 can The aim of the present investigation was to perform a be incorporated in both natural and synthetic andradite- Fourier transform infrared (FTIR) study on different sam- rich garnet (Flint et al. -
Geology and Selected Minerals of the Diamond Hill Quartz Mine Antreville, South Carolina by Mike Streeter, GMS Member Copyright March 2004
Tips and Trips Page 11 The Georgia Mineral Society May 2004 Geology and Selected Minerals of the Diamond Hill Quartz Mine Antreville, South Carolina by Mike Streeter, GMS Member Copyright March 2004 Chrissy and I have spent a great deal of time at the Diamond Diamond Hill is nothing short of remarkable when you consider Hill Quartz Mine near Antreville, South Carolina over the past that the actual collecting areas occupy a total of less than 3 several months. Chester Karwoski, who purchased the acres and that each variety requires its own unique set of property in 2003, brought in some heavy earth-moving conditions to form. The three most sought after varieties of equipment last fall and has opened up some new collecting quartz at the mine are skeletal, smoky and amethyst. opportunities. On our most recent trip to the mine on February 28, 2004, members of the Rome Georgia Gem and Mineral Skeletal quartz (also known Society and the Southern Appalachian Mineral Society joined as elestial quartz) exhibits a us. Since it is no secret that that I am a geologist by trade, I layered or ribbed pattern. am often asked geological and mineralogical questions about Its appearance gave rise to collecting locales. While digging at Diamond Hill, I was asked the term "skeletal" as the to explain how the rocks and crystals formed. Now there's a crystals resemble what $64,000 question for you! I answered the question as best I someone with a good could at the time. Since then, I have researched the literature imagination would expect to obtain a more detailed explanation that I would like to share the skeleton of a quartz with you. -
The A-Z List of Bridal Accessories to Guide Your Own Wedding Shopping Spree 10/3/2019 the A-Z List of Bridal Accessories to Guide Your Own Wedding Shopping Spree
10/3/2019 The A-Z List of Bridal Accessories To Guide Your Own Wedding Shopping Spree 10/3/2019 The A-Z List of Bridal Accessories To Guide Your Own Wedding Shopping Spree The A-Z List of Bridal Accessories To Guide Your Own Wedding Shopping Spree | Wedding Tips ARE YOU A VENDOR? Budget PLANNING TOOLS WEDDING VENUES WEDDING VENDORS BRIDES GROOMS WEDDING IDEAS Wedding Website LOG IN SIGN UP FOR FREE Plan on the go with the WeddingWire app Wedding / Wedding Ideas / Wedding fashion / The Bride SEARCH iPhone Android THE BRIDE MOST POPULAR ON WEDDINGWIRE The A-Z List of Bridal Accessories To Guide Your Own Wedding Shopping Spree 15 Latest Daily Wear Gold 1 Mangalsutra Designs For By Vidhi Maingi Gaur Today's Brides 25 of February of 2019 HAKIM CREATION PHOTOGRAPHY 10 Anita Dongre Bridal 2 Lehengas We Saw on Real Brides From plain jane anklets to heavy, Ghungroo-laden jewellery, the anklet is essential Wonder what all should you don for your very special day? We've gone across for nearly all Indian brides. It's soft tinkles announce her entry into a new home the length and breadth of India to come up with an all-inclusive list of bridal 155 Mehndi Designs and heath, while their look adds volumes to her individual bridal look. From the accessories for the dainty Indian bride. Here's everything that common or 3 Every Bride Needs to See thread-like anklet to heavy temple jewellery, from heavy Jhanjhar and Pajeb to the completely unique. Right Now Jhallar and Payal - you will be oored by the number of options available. -
The New IMA List of Gem Materials – a Work in Progress – Updated: July 2018
The New IMA List of Gem Materials – A Work in Progress – Updated: July 2018 In the following pages of this document a comprehensive list of gem materials is presented. The list is distributed (for terms and conditions see below) via the web site of the Commission on Gem Materials of the International Mineralogical Association. The list will be updated on a regular basis. Mineral names and formulae are from the IMA List of Minerals: http://nrmima.nrm.se//IMA_Master_List_%282016-07%29.pdf. Where there is a discrepancy the IMA List of Minerals will take precedence. Explanation of column headings: IMA status: A = approved (it applies to minerals approved after the establishment of the IMA in 1958); G = grandfathered (it applies to minerals discovered before the birth of IMA, and generally considered as valid species); Rd = redefined (it applies to existing minerals which were redefined during the IMA era); Rn = renamed (it applies to existing minerals which were renamed during the IMA era); Q = questionable (it applies to poorly characterized minerals, whose validity could be doubtful). Gem material name: minerals are normal text; non-minerals are bold; rocks are all caps; organics and glasses are italicized. Caveat (IMPORTANT): inevitably there will be mistakes in a list of this type. We will be grateful to all those who will point out errors of any kind, including typos. Please email your corrections to [email protected]. Acknowledgments: The following persons, listed in alphabetic order, gave their contribution to the building and the update of the IMA List of Minerals: Vladimir Bermanec, Emmanuel Fritsch, Lee A. -
List of New Mineral Names: with an Index of Authors
415 A (fifth) list of new mineral names: with an index of authors. 1 By L. J. S~v.scs~, M.A., F.G.S. Assistant in the ~Iineral Department of the,Brltish Museum. [Communicated June 7, 1910.] Aglaurito. R. Handmann, 1907. Zeita. Min. Geol. Stuttgart, col. i, p. 78. Orthoc]ase-felspar with a fine blue reflection forming a constituent of quartz-porphyry (Aglauritporphyr) from Teplitz, Bohemia. Named from ~,Xavpo~ ---- ~Xa&, bright. Alaito. K. A. ~Yenadkevi~, 1909. BuU. Acad. Sci. Saint-P6tersbourg, ser. 6, col. iii, p. 185 (A~am~s). Hydrate~l vanadic oxide, V205. H~O, forming blood=red, mossy growths with silky lustre. Founi] with turanite (q. v.) in thct neighbourhood of the Alai Mountains, Russian Central Asia. Alamosite. C. Palaehe and H. E. Merwin, 1909. Amer. Journ. Sci., ser. 4, col. xxvii, p. 899; Zeits. Kryst. Min., col. xlvi, p. 518. Lead recta-silicate, PbSiOs, occurring as snow-white, radially fibrous masses. Crystals are monoclinic, though apparently not isom0rphous with wol]astonite. From Alamos, Sonora, Mexico. Prepared artificially by S. Hilpert and P. Weiller, Ber. Deutsch. Chem. Ges., 1909, col. xlii, p. 2969. Aloisiite. L. Colomba, 1908. Rend. B. Accad. Lincei, Roma, set. 5, col. xvii, sere. 2, p. 233. A hydrated sub-silicate of calcium, ferrous iron, magnesium, sodium, and hydrogen, (R pp, R',), SiO,, occurring in an amorphous condition, intimately mixed with oalcinm carbonate, in a palagonite-tuff at Fort Portal, Uganda. Named in honour of H.R.H. Prince Luigi Amedeo of Savoy, Duke of Abruzzi. Aloisius or Aloysius is a Latin form of Luigi or I~ewis. -
Symposium on Agate and Cryptocrystalline Quartz
Symposium on Agate and Cryptocrystalline Quartz September 10 – 13, 2005 Golden, Colorado Sponsored by Friends of Mineralogy, Colorado Chapter; Colorado School of Mines Geology Museum; and U.S. Geological Survey 2 Cover Photos {top left} Fortification agate, Hinsdale County, Colorado, collection of the Geology Museum, Colorado School of Mines. Coloration of alternating concentric bands is due to infiltration of Fe with groundwater into the porous chalcedony layers, leaving the impermeable chalcedony bands uncolored (white): ground water was introduced via the symmetric fractures, evidenced by darker brown hues along the orthogonal lines. Specimen about 4 inches across; photo Dan Kile. {lower left} Photomicrograph showing, in crossed-polarized light, a rhyolite thunder egg shell (lower left) a fibrous phase of silica, opal-CTLS (appearing as a layer of tan fibers bordering the rhyolite cavity wall), and spherulitic and radiating fibrous forms of chalcedony. Field of view approximately 4.8 mm high; photo Dan Kile. {center right} Photomicrograph of the same field of view, but with a 1 λ (first-order red) waveplate inserted to illustrate the length-fast nature of the chalcedony (yellow-orange) and the length-slow character of the opal CTLS (blue). Field of view about 4.8 mm high; photo Dan Kile. Copyright of articles and photographs is retained by authors and Friends of Mineralogy, Colorado Chapter; reproduction by electronic or other means without permission is prohibited 3 Symposium on Agate and Cryptocrystalline Quartz Program and Abstracts September 10 – 13, 2005 Editors Daniel Kile Thomas Michalski Peter Modreski Held at Green Center, Colorado School of Mines Golden, Colorado Sponsored by Friends of Mineralogy, Colorado Chapter Colorado School of Mines Geology Museum U.S. -
Exceptional Works of Art 2017 PUSHKIN ANTIQUES – MAYFAIR –
Exceptional works of art 2017 PUSHKIN ANTIQUES – MAYFAIR – At Pushkin Antiques we specialise in unique statement Each item is professionally selected and inspected pieces of antique silver as well as branded luxury items, to ensure we can give our customers a guarantee of stylish interior articles and objects d’art. authenticity and the required peace of mind when buying from us. Since the inception of our company, we’ve been at the forefront of online sales for high end, quality antiques. Our retail gallery is located on the lower floor of the world Our presence on most major platforms has allowed us famous Grays Antiques Centre in the heart of Mayfair. to consistently connect exquisite pieces with the most discerning collectors and interior decorators from all over the world with particular focus on the demands of the markets from the Far East, the Americas, Europe & Russia. www.pushkinantiques.com [email protected] We aim to provide the highest quality in every department: rare hand crafted articles, accurate item descriptions (+44) 02085 544 300 to include the history and provenance of each item, an (+44) 07595 595 079 extensive photography report, as well as a smooth buying process thus facilitating an efficient and pleasant online Shop 111, Lower Ground Floor, Grays Antiques Market. experience. 58 Davies St, London. W1K 5AB, UK. ALEX PUSHKIN OLGA PUSHKINA DUMITRU TIRA Founder & Director Managing Director Photographer Contents 6 ENGLISH SILVER 42 CHINESE SILVER 56 JAPANESE SILVER 66 INDIAN SILVER 78 BURMESE SILVER 86 CONTINENTAL SILVER 100 FRENCH SILVER 108 GERMAN SILVER 118 RUSSIAN SILVER 132 OBJECTS OF VERTU English Silver The style and technique in manufacturing silver during Hester Bateman (1708-1794) was one of the greatest this era (over 100 years) changed radically, reflecting silversmiths operating in this style, she is the most the variations in taste, society, costumes, economic and renowned and appreciated female silversmith of all time. -
A Midsummer Night's Bollywood Dream by © 2009
A MIDSUMMER NIGHT’S BOLLYWOOD DREAM BY © 2009 Madison Elizabeth Spencer Submitted to the graduate degree program in Design and the Graduate Faculty of the University of Kansas in partial fulfillment of the requirements of the degree of Master of Fine Arts ________________________ Chairperson ________________________ ________________________ ________________________ Date defended: ________04/06/2009______ The Thesis Committee for Madison Elizabeth Spencer certifies that this is the approved Version of the following thesis: A MIDSUMMER NIGHT’S BOLLYWOOD DREAM Committee: ________________________ Chairperson ________________________ ________________________ ________________________ Date approved: _________04/24/2009_____ ii TABLE OF CONTENTS INTRODUCTION 1 HINDU DEITIES AND THE CASTE SYSTEM 4 DESIGN CONCEPT 8 COSTUME DESIGN 11 MAKE-UP 17 SET DESIGN 19 LIGHTING DESIGN 22 CONCLUSION 23 CLOTHING GLOSSARY 25 BIBLIOGRAPHY 27 NOTES 29 IMAGE INDEX 30 DOCUMENT INDEX 34 iii INTRODUCTION “Bollywood” is the colloquial term used to describe the Hindi film industry in India. It describes that part of the film industry with colorful, exaggerated, overly dramatic, music-and-dance-filled characteristics rather than this nation’s entire film making. In contrast to Hollywood, from which it takes its tongue-in-cheek name, Bollywood is no actual place; rather, it is the term that best describes a style of film making. Bollywood style in its broadest meaning is the mass media vehicle for entertainment that feeds some of the amusement needs of a population with a variety of languages and ethnic/caste backgrounds. Themes are simple and predictable for the most part, with a great degree of flexibility in the telling of even the most well known story in order to make a relevant point on a particular issue or current event. -
47. Chert and Porcellanite from Deep Sea Drilling Project Site 436, Northwest Pacific
47. CHERT AND PORCELLANITE FROM DEEP SEA DRILLING PROJECT SITE 436, NORTHWEST PACIFIC K. A. Pisciotto,1 Earth Science Board, University of California, Santa Cruz, California ABSTRACT Cretaceous chert and porcellanite recovered at Site 436, east of northern Honshu, Japan, are texturally and mineralogically similar to siliceous rocks of comparable age at Sites 303, 304, and 307 in the northwest Pacific. These rocks probably were formed by impregna- tion of the associated pelagic clay with locally derived silica from biogenic and perhaps some volcanic debris. Fine horizontal lamina- tions are the only primary sedimentary structures, suggesting mini- mal reworking and transport. Collapse breccias and incipient chert nodules are diagenetic features related to silicification and compac- tion of the original sediment. Disordered opal-CT (^[101] = 4.09 Å) and microgranular quartz (crystallinity index < 1.0) are the two common silica minerals pres- ent. Some samples show quartz replacing this poorly ordered opal- CT, supporting the notion that opal-CT does not become completely ordered (i.e., d[101] = 4.04 Å) in some cases before being converted to quartz. The present temperature calculated for the depth of the shallowest chert and porcellanite at this site is 30 °C; this may repre- sent the temperature of conversion of opal-CT to quartz. High reflection coefficients (0.29-0.65) calculated for the boundary be- tween chert-porcellanite and clay-claystone support the common observation that chert is a strong seismic reflector in deep-sea sedimentary sections. INTRODUCTION This paper discusses the petrology and origin of cherts and porcellanites at Site 436. In addition, the Keene's (1975, 1976) comprehensive work on cherts temperature of formation and acoustic impedances of and porcellanites from the North Pacific clearly demon- these siliceous rocks are calculated.