Natural Gemstones I* ^H U.S

Total Page:16

File Type:pdf, Size:1020Kb

Natural Gemstones I* ^H U.S U.S. Department of the Interior U.S. Geological Survey Natural Gemstones i* ^H U.S. Department of the Interior U.S. Geological Survey Natural Gemstones Searching for gemstones in the United States is a popular recreational activity for collectors and hobbyists Cover: Quartz, Rhode Island. Inside covers: Amethyst crystals, Mexico. Natural gemstones The average grade of the richest diamond kimberlite pipes in Africa is about 1 part A natural gemstone is a mineral, stone, or diamond in 40 million parts "ore." organic matter that can be cut and polished Kimberlite, a plutonic igneous rock, as­ or otherwise treated for use as jewelry or cends from a depth of at least 100 kilome­ other ornament. A precious gemstone has ters (60 miles) to form a diatreme (narrow beauty, durability, and rarity, whereas a cone-shaped rock body or "pipe"). More­ semiprecious gemstone has only one or two over, because much diamond is not of gem of these qualities. A gem is a gemstone that quality, the average stone in an engagement has been cut and polished. ring is the product of the removal and pro­ cessing of 200 to 400 million times its Diamond, corundum (ruby and sapphire), volume of rock. beryl (emerald and aquamarine), topaz, and opal are generally classed as precious stones. All other gemstones are usually Gemstones occur in most major classed as semiprecious. geologic environments. A mineral is any naturally formed homoge­ Each environment tends to have a charac­ neous inorganic material. teristic suite of gem materials, but many kinds of gems occur in more than one envi­ A mineralogist is a person who studies the ronment. Most gemstones are found in formation, occurrence, properties, composi­ igneous rocks and alluvial gravels, but tion, and classification of minerals. sedimentary and metamorphic rocks may also contain gem materials. A gemologist is a person who has success­ fully completed recognized courses in Examples of geologic environments in gemology (the science and study of gem- which gemstones are found: stones) and has proven skills in identifying and evaluating gem materials. Pegmatite a coarse-grained intrusive igneous rock body, occurring as dikes (a A lapidary is a cutter, polisher, or engraver tabular-shaped body), lenses, or veins in the of precious stones. surrounding rock. Stream gravels (placers) deposits of Geologic environment heavier and more durable than average minerals that have been eroded out of the Gemstones are not plentiful. Gemstones do original rock. Often tourmaline, beryl, and not form "ore" deposits in the normal sense. many other gem-quality minerals have eroded out of the original rock in which Gems, when present at all, tend to be scat­ they formed and have moved and been tered sparsely throughout a large body of concentrated locally by water in streams. rock or to have crystallized as small aggre­ Sapphires in Judith Basin County, Mon­ gates or fill veins and small cavities. tana, were first found when the gravels were worked for gold from 1895 to 1930. Even stream gravel concentrations tend to be small a few stones in each of several Metamorphic rocks rocks that have been bedrock cracks, potholes, or gravel lenses altered by great heat, pressure, or both. in a stream bed. Garnet, for example, is commonly found as crystals in gneiss and mica schist. Quartz with phantoms, Brazil. Aquamarine, Brazil. Mineral gemstones Corundum (hardness: 9 Mohs) Aluminum oxide Hardness and specific gravity are two of the Specific gravity: 3.96-4.05 major characteristics of gemstones. Ruby: Intense red Hardness of a gemstone is its resistance to Sapphire: Blue scratching and may be described relative to a standard scale of 10 minerals known as Diamond (hardness: 10 Mohs) the Mohs scale. F. Mohs, an Austrian min­ Carbon eralogist, developed this scale in 1822. Specific gravity: 3.51 According to Mohs' scale, the hardness of Colorless to faint yellowish tinge, also Talc is 1 Feldspar is 6 variable Gypsum is 2 Quartz is 7 Calcite is 3 Topaz is 8 Feldspar (hardness: 6-6.5 Mohs) Fluorite is 4 Sapphire is 9 Two distinctly different alkali alumino Apatite is 5 Diamond is 10 silicates: the Plagioclase and the Alkali Feldspar Series Specific gravity is the number of times Specific gravity: 2.55-2.76 heavier a gemstone of any volume is than an equal volume of water; in other words, it Plagioclase Series is the ratio of the density of the gemstone to Labradorite: Colorful, iridescent, also the density of water. transparent stones in yellow, orange, red, and green The 16 mineral gemstone groups listed Sunstone: Gold spangles from inclusions below are highly prized for their beauty, of hematite durability, and rarity: Peristerite: Blue white iridescence Beryl (hardness: 7.5-8 Mohs) Alkali Feldspar Group Beryllium aluminum silicate Orthoclase: Pale yellow, flesh red Specific gravity: 2.63-2.91 Amazonite: Yellow green to greenish blue Moonstone: Colorless; also white to Emerald: Intense green or bluish green yellowish, and reddish to bluish gray Aquamarine: Greenish blue or light blue Morganite: Pink, purple pink, or peach Garnet (hardness: 6.5-7.5 Mohs) Heliodore: Golden yellow to golden green A group of silicate minerals Red beryl: Raspberry red Specific gravity: 3.5-4.3 Goshenite: Colorless, greenish yellow, yellow green, brownish Almandine: Orangy red to purplish red Almandine-spessartine: Reddish orange Chrysoberyl (hardness: 8.5 Mohs) Andradite: Yellowish green to orangy Beryllium aluminum oxide yellow to black Specific gravity: 3.68-3.78 Demantoid: Green to yellow green andradite Chrysoberyl: transparent yellowish green to Topazolite: Yellow to orangy yellow greenish yellow and pale brown Grossular: Colorless; also orange, pink, Alexandrite: red in incandescent light and yellow, and brown green in daylight Tsavorite: Green to yellowish green Cat's eye: usually yellowish or greenish Hessonite: Yellow orange to red Pyrope: Colorless; also pink to red Chrome pyrope: Orange red Pyrope-Almadine: Reddish orange to red lazurite with variable amounts of pyrite purple (brassy flecks) and white calcite Pyrope-Spessartine: Greenish yellow to Specific gravity: 2.7-2.9 purple Malaia: Yellowish to reddish orange Deep blue, azure blue, greenish blue (bluish to brown color with flecks of white and gold) Color-change garnet. Blue green in day­ light to purple red in incandescent light Opal (hardness: 5.5-6.5 Mohs) Rhodolite: Purplish red to red purple Hydrated silica Spessartine: Yellowish orange Specific gravity: 1.98-2.25 Uvarovite: Emerald green White opal: Opaque, porcelain-like white Jade (hardness: 6 Mohs) material; colors resemble flashes or speckles Nephrite Black opal: Flashes and speckles appear Calcium magnesium silicate against black background Specific gravity: 2.9-3.1 Water opal: A transparent, colorless opal is the background for brilliant flashes of White, deep green, creamy brown color Fire opal: Reddish or orange opal Jadeite Sodium aluminum silicate Peridot [Olivine] (hardness: 7 Mohs) Specific gravity: 3.1-3.5 Magnesium iron silicate Specific gravity: 3.22-3.45 White, leafy and blue green, emerald green, lavender, dark blue green and greenish Olive to lime green black, deep emerald-green Quartz (hardness: 7 Mohs) Lapis lazuli (hardness: 5-5.5 Mohs) Silicon dioxide or silica A rock composed mainly of the mineral Specific gravity: 2.65 Coarsely crystalline varieties of silica Rock crystal: Colorless Amethyst: Purple Citrine: Yellow to amber Morion: Black Smoky quartz or cairngorm: smoky gray to brown Rose quartz: Translucent pink Green quartz or praziolite: Green Cryptocrystalline varieties of silica Chalcedony and Jasper (variable) Agate: Bull's eye agate, Iris or fire agate, Onyx, Sardonyx. Bloodstone or heliotrope. Cornelian. Chrysoprase. Moss agate. Plasma. Prase. Sard. Jasper. Spinel (hardness: 8 Mohs) Diamond Star of Sierra Leone. Magnesium aluminum oxide Specific gravity: 3.58-4.06 Candelabra: white quartz, blue-capped red elbaite, and tan albite, California. Balas ruby: Red Indicolite: Dark blue Almandine spinel: Purple red Rubellite: Pink to red Rubicelle: Orange Siberite: Violet Sapphire spinel and ghanospinel: Blue Verdilite: Green Chlorspinel: Green Turquoise (hardness: 5-6 Mohs) Topaz (hardness: 8 Mohs) Hydrous copper aluminum phosphate Aluminum silicate fluoride hydroxide Specific gravity: 2.6-2.8 Specific gravity: 3.5-3.6 Sky blue; greenish blue Wine yellow, pale blue, green, violet, or red Zircon (hardness: 7.5 Mohs) Tourmaline (hardness: 7-7.5 Mohs) Zirconium silicate Complex aluminum borosilicate Specific gravity: 4.6-4.7 (Elbaite, Dravite, Uvite) Specific gravity: 3.03-3.25 Jargon: Variable Matura diamond: Colorless Achorite: Colorless Hyacinth: Yellow, orange, red, brown Brazilian emerald: Green Dravite: Brown The Hooker Emerald, Colombia. Birthstones Month Month of birth Gemstone Color of birth Gemstone Color January Garnet Dark red July Ruby (Corundum) Red February Amethyst (Quartz) Purple or Carnelian (Quartz) March Aquamarine (Beryl) Pale blue or Bloodstone August Peridot Pale green (Quartz) or Sardonyx Brown April Diamond or Colorless (Quartz) and white Rock Crystal September Sapphire Pale to dark (Quartz) (Corundum) blue May Emerald (Beryl) Bright green or Lapis Lazuli Deep blue or Chrysoprase Pale green October Opal or Tourmaline Variegated (Quartz) November Topaz or Citrine Yellow June Pearl or Moonstone Cream (Quartz) (Feldspar) December Turquoise Sky blue Organic gemstones This compact velvet-black coal takes a good polish and is often cut into beads, The four organic gemstone groups listed bracelets, and a wide range of decorative below are highly prized for their beauty and and useful objects. rarity. However, they are not as durable as gemstones from minerals: Pearl (hardness: 2.5-4.5 Mohs) Formed within a mollusk, such as an oyster, Amber (hardness: 2-2.5 Mohs) that deposits a substance called nacre A mixture of hydrocarbons around an irritant that entered the organism Specific gravity: 1.05-1.096 Specific gravity: 2.71 Hard fossil resin or sap of ancient pine Pearl-bearing mollusks are found in both trees.
Recommended publications
  • Structure and Physical Properties of Hydrogrossular Mineral Series
    STRUCTURE AND PHYSICAL PROPERTIES OF HYDROGROSSULAR MINERAL SERIES A THESIS IN PHYSICS Presented to the Faculty of the University of Missouri-Kansas City in Partial requirements for the degree MASTER OF SCIENCE By PUJA ADHIKARI M.Sc, Tribhuban University, Kathmandu, Nepal, 2010 Kansas City, Missouri 2015 ©2015 PUJA ADHIKARI ALL RIGHTS RESERVED Structure and physical properties of Hydrogrossular mineral series Puja Adhikari, Candidate for the Master of Science Degree University of Missouri-Kansas City, 2015 ABSTRACT The mineral hydrogrossular series (Ca3Al2(SiO4)3-x(OH) 4x; 0 ≤ x ≤ 3) are important water bearing minerals found in the upper and lower part of the Earth’s mantle. They are vital to the planet’s hydrosphere under different hydrothermal conditions. The composition and structure of this mineral series are important in geoscience and share many commonalities with cement and clay materials. Other than the end members of the series x = 0 (grossular) and x = 3 (katoite) which have a cubic garnet structure, the structure of the series is totally unknown. We used large-scale ab initio modeling to investigate the structures and properties for hydrogrossular series for x = 0, 0.5, 1, 1.5, 2, 2.5, 3. Results indicate that for x > 0 and x < 3, the structures are tetragonal. This shows that there is structural change related to the lowering of overall symmetry associated with the composition of SiO4 tetrahedra and AlO6 octahedra. Total Bond order also explains the reason behind the change in the compressibility of the series. The electronic structure, mechanical and optical properties of the hydrogrossular series are calculated and the results for grossular and katoite are in good agreement with the available experimental data.
    [Show full text]
  • Heat Treating Corundum: the Bangkok Operation
    HEAT TREATING CORUNDUM: THE BANGKOK OPERATION By Jack S. D. Abraham Following LIP on Nassau's 1981 article on Banglzolz gem dealer buys a lo+-ct ruby for a six- the technical aspects of heat treating ruby A figure sum and heats it hoping to improve its color and sapphire, the author reports his and value. After one heating, the stone dulls and cannot personal observations of the actual heat be sold for half of its original price. But a few tries later treatment process in Bangkok. He the stone is so improved that a major European dealer discusses the potential effects that this buys it for almost five times the original amount- process can have on a stone-both positive and negative-and emphasizes lznowing that it has been heat treated. the importance of the natural make-up of Another Thai dealer pays a large sum for a 600-ct piece the stone itself to the success of heot of sapphire rough. He then cuts it into four sections and treatment. heats each. For the largest piece, which is over 100 ctl he receives 20% more than he paid for the entire original stone-again from a buyer who knows the stone is heated. A third dealer, however, heats a sapphire for which he has paid a six-figure sum but instead of enhancing the color, the treatment causes the stone to brealz into several pieces. It is now worth a fraction of its original price. Such incidents suggest that the heating of ruby and sapphire has become a fully acceptedl if very rislzyl fact of life in the Far East.
    [Show full text]
  • Rhodochrosite Gems Unstable Colouration of Padparadscha-Like
    Volume 36 / No. 4 / 2018 Effect of Blue Fluorescence on the Colour Appearance of Diamonds Rhodochrosite Gems The Hope Diamond Unstable Colouration of in London Padparadscha-like Sapphires Volume 36 / No. 4 / 2018 Cover photo: Rhodochrosite is prized as both mineral specimens and faceted stones, which are represented here by ‘The Snail’ (5.5 × 8.6 cm, COLUMNS from N’Chwaning, South Africa) and a 40.14 ct square-cut gemstone from the Sweet Home mine, Colorado, USA. For more on rhodochrosite, see What’s New 275 the article on pp. 332–345 of this issue. Specimens courtesy of Bill Larson J-Smart | SciAps Handheld (Pala International/The Collector, Fallbrook, California, USA); photo by LIBS Unit | SYNTHdetect XL | Ben DeCamp. Bursztynisko, The Amber Magazine | CIBJO 2018 Special Reports | De Beers Diamond ARTICLES Insight Report 2018 | Diamonds — Source to Use 2018 The Effect of Blue Fluorescence on the Colour 298 Proceedings | Gem Testing Appearance of Round-Brilliant-Cut Diamonds Laboratory (Jaipur, India) By Marleen Bouman, Ans Anthonis, John Chapman, Newsletter | IMA List of Gem Stefan Smans and Katrien De Corte Materials Updated | Journal of Jewellery Research | ‘The Curse Out of the Blue: The Hope Diamond in London 316 of the Hope Diamond’ Podcast | By Jack M. Ogden New Diamond Museum in Antwerp Rhodochrosite Gems: Properties and Provenance 332 278 By J. C. (Hanco) Zwaan, Regina Mertz-Kraus, Nathan D. Renfro, Shane F. McClure and Brendan M. Laurs Unstable Colouration of Padparadscha-like Sapphires 346 By Michael S. Krzemnicki, Alexander Klumb and Judith Braun 323 333 © DIVA, Antwerp Home of Diamonds Gem Notes 280 W.
    [Show full text]
  • Download Course Outline for This Program
    Program Outline 434- Jewellery and Metalwork NUNAVUT INUIT LANGUAGES AND CULTURES Jewelry and Metalwork (and all fine arts) PROGRAM REPORT 434 Jewellery and Metalwork Start Term: No Specified End Date End Term: No Specified End Date Program Status: Approved Action Type: N/A Change Type: N/A Discontinued: No Latest Version: Yes Printed: 03/30/2015 1 Program Outline 434- Jewellery and Metalwork Program Details 434 - Jewellery and Metalwork Start Term: No Specified End Date End Term: No Specified End Date Program Details Code 434 Title Jewellery and Metalwork Start Term No Specified End Date End Term No Specified End Date Total Credits Institution Nunavut Faculty Inuit Languages and Cultures Department Jewelry and Metalwork (and all fine arts) General Information Eligible for RPL No Description The Program in Jewellery and Metalwork will enable students to develop their knowledge and skills of jewellery and metalwork production in a professional studio atmosphere. To this end the program stresses high standards of craftship and creativity, all the time encouraging and exposing students to a wide range of materials, techniques and concepts. This program is designed to allow the individual student to specialize in an area of study of particular interest. There is an emphasis on creative thinking and problem-solving throughout the program.The first year of the program provides an environment for the students to acquire the necessary skills that will enable them to translate their ideas into two and three dimensional jewellery and metalwork. This first year includes courses in: Drawing and Design, Inuit Art and Jewellery History, Lapidary and also Business and Communications.
    [Show full text]
  • The Red Emerald
    The Red Emerald Black Album Words by Seth William Rozendaal Photos by David Rozendaal This work is for the enjoyment of gemstone aficionados around the world and throughout time, and dedicated to the divine muse who inspires everything. This book celebrates the Red Emerald’s public debut at the 2017 Tucson Gem and Mineral Show. Graphics taken from the Mineralogical Record Volume 47 Number 1: Colombian Emeralds where noted. The two photos of the Heart matrix specimen on the top of the page in Section VI were taken by Wayne Schrimp. Seth Rozendaal is responsible for the landscape photo in Section II, the beveled heart in Section VI and Office Suite Graphics. The Suite Treasure necklace photo in Section XIII was taken at the Brent Isenberger Studio. Cover and all other interior photos in this album were taken by David Rozendaal. Without his tireless dedication, this publication would not have been possible. For additional information, please contact: Seth William Rozendaal (515) 868-7207 [email protected] Index I - Red Beryl IS Red Emerald II - Formation III - Matrix Specimens IV - Wafers V - Prisms VI - Twins VII - Clusters VIII - Bixbyite Combinations IX - Topaz Combinations X - Hourglass Patterning XI - The Scarlet Spectrum XII - Facet-Grade Red Emerald XIII - The Red Emerald Suite Treasure I ~ Red Beryl IS Red Emerald The human infatuation with Emeralds runs so deep, and our desire for them traces so far back… It's one of the only gemstones found in rank-signifying Neolithic headdresses. Yeah, you heard me: Caveman Crowns. Aja Raden - Author, Historian and Scientist Diamonds may be forever, but only Emeralds are eternal; our appreciation of Emeralds stretches from the beginning of human civilization to the very end.
    [Show full text]
  • SGG Corundum Treatment.Pptx
    The beauty of colour © Swiss Gemmological Institute SSEF SGG Zentralkurs, Thun, 15. April 2013 Treatment of corundum characteristics, detection and declaration Michael S. Krzemnicki Swiss Gemmological Institute SSEF Switzerland Photos and figures © H.A. Hänni & M.S. Krzemnicki 1! Consumer+expectation+ Quality& Every&gemstone&deposit&produces&stones&of&high&and&low&quality.& Usually&the&quality&distribution&has&the&shape&of&a&pyramid.&& Top&stones&are&rare,&stones&of&lower&quality&are&very&abundant.& The&exploitation&of&gems&is&expensive,&regardless&of&their&quality.& It&is&economically&and&important&to&be&able&to&enhance&stones&of&& the&lower&part&of&the&quality&pyramid&(also&for&the&miners!)& Once&a&treatment&is&developed&and&successfull,&it&often&is&also&applied&& on&stones&of&better&quality&to&make&them&even&better&looking.& Gem$deposit+production+ Quantity& © SSEF Swiss Gemmological Institute Treatment options for corundum... To&modify&transparency:&& &F&Gilling&of&Gissures&with&colourless&substance&&(oil,&artiGicial&resin,&glass)& &F&heating&to&dissolve&inclusions& & To&modify&colour& &F&Gilling&of&Gissures&with&coloured&substance&(oil,&artiGicial&resin,&glass)& &F&heating&in&oxidising&or&reducing&conditions&(±&with&additives)& &F&diffusion&of&„colouring“&elements&into&the&corundum&lattice& &F&irradiation& & To&enhance&stability& &F&Gilling&of&Gissures/cavities&with&solidifyig&substances&& & To&create&optical&effects&& &F&heating&with&additives& & © SSEF Swiss Gemmological Institute! 2! Treatment options for corundum... Fissure&Gilling&and&dyeing& & Foiling,&Painting& Heating&with&blowFpipe& ©&F.&Notari& Heating&with&electrical&furnace& ©&H.A.&Hänni& Irradiation& Heating&combined&with&surface&diffusion& Heating&with&borax&to&induce&Gissure&„healing“& Beryllium&diffusion& LeadFglass&Gissure&Gilling& & CobaltFglass&Gissure&Gilling& & next&treatment&??& & future& 0& 1000& 1900& 2000& Time+scale+ & © SSEF Swiss Gemmological Institute! Treatment options for corundum..
    [Show full text]
  • The Wittelsbach-Graff and Hope Diamonds: Not Cut from the Same Rough
    THE WITTELSBACH-GRAFF AND HOPE DIAMONDS: NOT CUT FROM THE SAME ROUGH Eloïse Gaillou, Wuyi Wang, Jeffrey E. Post, John M. King, James E. Butler, Alan T. Collins, and Thomas M. Moses Two historic blue diamonds, the Hope and the Wittelsbach-Graff, appeared together for the first time at the Smithsonian Institution in 2010. Both diamonds were apparently purchased in India in the 17th century and later belonged to European royalty. In addition to the parallels in their histo- ries, their comparable color and bright, long-lasting orange-red phosphorescence have led to speculation that these two diamonds might have come from the same piece of rough. Although the diamonds are similar spectroscopically, their dislocation patterns observed with the DiamondView differ in scale and texture, and they do not show the same internal strain features. The results indicate that the two diamonds did not originate from the same crystal, though they likely experienced similar geologic histories. he earliest records of the famous Hope and Adornment (Toison d’Or de la Parure de Couleur) in Wittelsbach-Graff diamonds (figure 1) show 1749, but was stolen in 1792 during the French T them in the possession of prominent Revolution. Twenty years later, a 45.52 ct blue dia- European royal families in the mid-17th century. mond appeared for sale in London and eventually They were undoubtedly mined in India, the world’s became part of the collection of Henry Philip Hope. only commercial source of diamonds at that time. Recent computer modeling studies have established The original ancestor of the Hope diamond was that the Hope diamond was cut from the French an approximately 115 ct stone (the Tavernier Blue) Blue, presumably to disguise its identity after the that Jean-Baptiste Tavernier sold to Louis XIV of theft (Attaway, 2005; Farges et al., 2009; Sucher et France in 1668.
    [Show full text]
  • The Anjahamiary Pegmatite, Fort Dauphin Area, Madagascar
    The Anjahamiary pegmatite, Fort Dauphin area, Madagascar Federico Pezzotta* & Marc Jobin** * Museo Civico di Storia Naturale, Corso Venezia 55, I-20121 Milano, Italy. ** SOMEMA, BP 6018, Antananarivo 101, Madagascar. E-mail:<[email protected]> 21 February, 2003 INTRODUCTION Madagascar is among the most important areas in the world for the production, mainly in the past, of tourmaline (elbaite and liddicoatite) gemstones and mineral specimens. A large literature database documents the presence of a number of pegmatites rich in elbaite and liddicoatite. The pegmatites are mainly concentrated in central Madagascar, in a region including, from north to south, the areas of Tsiroanomandidy, Itasy, Antsirabe-Betafo, Ambositra, Ambatofinandrahana, Mandosonoro, Ikalamavony, Fenoarivo and Fianarantsoa (e.g. Pezzotta, 2001). In general, outside this large area, elbaite-liddicoatite-bearing pegmatites are rare and only minor discoveries have been made in the past. Nevertheless, some recent work made by the Malagasy company SOMEMEA, discovered a great potential for elbaite-liddicoatite gemstones and mineral specimens in a large, unusual pegmatite (the Anjahamiary pegmatite), hosted in high- metamorphic terrains. The Anjahamiary pegmatite lies in the Fort Dauphin (Tôlanaro) area, close to the southern coast of Madagascar. This paper reports a general description of this locality, and some preliminary results of the analytical studies of the accessory minerals collected at the mine. Among the most important analytical results is the presence of gemmy blue liddicoatite crystals with a very high Ca content, indicating the presence in this tourmaline crystal of composition near the liddicoatite end-member. LOCATION AND ACCESS The Anjahamiary pegmatite is located about 70 km NW of the town of Fort Dauphin (Tôlanaro) (Fig.
    [Show full text]
  • Geology Club Mineral: Collecting Trip
    Geology Club: Mineral Collecting Trip (10 October 2009) Trip Notes by Charles Merguerian STOP 1 – Grossular Garnet Locality, West Redding, Connecticut. [UTM Coordinates: 630.71E / 4575.38N, Bethel quadrangle]. Covering roughly 60 acres of land, this enigmatic massive fine-grained grossularite garnet + diopside rock in West Redding has made many mineral collectors and geologists take notice. Walk up the steep slope east of Simpaug Turnpike to see highly fractured, massive cinnamon-colored grossular garnet rock, part of a 0.6-km wide heart-shaped mass found at the faulted contact between the Stockbridge Marble (OCs) and injected muscovitic schist of the Rowe Schist member (OCr) of the Hartland Formation (Figure 1). According to Rodgers et al. (1985), we are very near Cameron’s Line (red and black line in Figure 1). Figure 1 – Geologic map of the area surrounding Stop 1 showing the Proterozoic gneissic rocks (Yg) and Cambrian Dalton Schist (Cd) to the west, the Stockbridge Marble (OCs), Cameron’s Line (CL in red), the injected schistose rocks of the Rowe Formation (OCr), and an Ordovician granitoid (Og) that may be responsible for this unusual Ca++-enriched skarn deposit. Note the NW-trending high-angle brittle faults that cut the region. (Adapted from Rodgers et al. 1985.) Two knolls at this locality are almost entirely composed of grossularite garnet (var. essonite) and lesser clinopyroxene. Mostly the garnet occurs alone with minor quartz and localized quartz veining has been observed. Chemical analysis of the garnet (SiO2 = 39.10%, CaO = 34.85%, Al2O3 = 19.61%, and total FeO+Fe2O3 = 5.44%), are quite similar to published analyses of grossular garnet, including the phenomenal grossular garnet crystals from Morelos, Mexico.
    [Show full text]
  • March 2019 Agate Explorer.Pub
    Cuyuna Rock, Gem and Mineral Society The Agate Explorer March 2019 Summer Field Trip Plans are being made for a long weekend trip to Thunder Bay to collect amethyst. The tentative dates are Friday -Sunday, July 5 -7. A sign -up sheet will be available at upcoming meeting in order to plan this trip. It is necessary to have a passport to travel to Canada. You may also check to see if an enhanced driver’s license is acceptable. March meeting Open Shop from 9 a.m. —noon Franklin Art Center Club member, Ray Strassberg, will be available for members to learn how Club Information to cut rocks using the 10” or 16” inch saws. Website -www.cuyunarockclub.org - Email [email protected] Bring rocks of your own or purchase something in the Rock Room. Meeting Place Lower level Franklin Arts Center Kids’ Program 1001 Kingwood St, Brainerd, MN 56401 Did you know that there are many Directions .4 mile east of Business Hwy. 371 different kinds of Lake Superior & Hwy. 210 intersection. agates? Lisa will tell you all about it (Castle turret water tower.) at the March meeting! Date/Time the 2nd Saturday of each month Rock Wrappers at 2 p.m. unless otherwise noted. Meets starting at 10 a.m. on meeting Saturdays. Club Dues $20/ family ,An open gathering for wire wrappers. Hang out with other wrappers, Free /unaccompanied juniors and work on your projects. (Bring all supplies needed.) Membership runs Learn tricks to make wrapping easier, a new design, from Jan. 1-Dec. 31st. or perhaps a new place to find supplies.
    [Show full text]
  • Preliminary Investigation of Purple Garnet from a New Deposit in Mozambique
    GIT GEMSTONE UPDATE Preliminary Investigation of Purple Garnet from a New Deposit in Mozambique By GIT-Gem testing laboratory 11 May 2016 Introduction In March 2016, a group of Thai gem dealer led by Mr. Pichit Nilprapaporn paid a visit to the GIT and informed us about a new garnet deposit in Mozambique, that was discovered near the western border with Zimbabwe. They also displayed a large parcel of rough and a few cut stones claimed to be the material found in this new deposit (Figure 1). According to the stone’s owner, these garnet specimens were unearthed from an unconsolidated sediment layer, just a few meters below ground surface. This brief report is our preliminary investigation on the interesting vivid purple garnet from the new deposit in Mozambique. Figure 1: Mr. Pichit Nilprapaporn (center), the stone’s owner, showing a large parcel of purple gar- net roughs claimed to be from a new deposit in Mozambique to the GIT director (left). The Gem and Jewelry Institute of Thailand (Public Organization) 140, 140/1-3, 140/5 ITF-Tower Building. 1st - 4th and 6th Floor,Silom Road, Suriyawong, Bangrak, Bangkok 10500 Thailand Tel: +66 2634 4999 Fax: +66 2634 4970; Web: http://www.git.or.th; E-mail: [email protected] 11 May, 2016 Preliminary Investigation of Purple Garnet from a New Deposit in Mozambique 2 Samples and Testing Procedure The stone’s owners donated some specimens (one 6.10 ct oval-facetted stone and 13 rough samples weighing from 3.83 to 9.43 cts) to the GIT Gem Testing Laboratory for studying.
    [Show full text]
  • Renowned for His Iconic Designs and Breathtaking Gem Collections, Harry Winston Was a Man Who Knew the True Value of a Diamond
    A BRILLIANT LEGACY Renowned for his iconic designs and breathtaking gem collections, Harry Winston was a man who knew the true value of a diamond. BY ALLISON HATA 54 A diamond is anything but just another stone. Highly coveted, precious and exceedingly rare, diamonds can take on different meanings: a symbol of status, a statement of love or a sign of purity. “Diamonds are a physical connection to [the earth] other than our feet on the ground,” says Russell Shor, a senior industry analyst for the Gemologist Institute of America. “When the earth was young and there was volcanic mass seething inside—this is how diamonds were formed. Diamonds connect us to that.” One man understood this intrinsic connection and dedicated his life to bringing the world closer to the precious gem through his jewelry designs and generous gifts to national institu- tions. Known as the “king of dia- monds,” the late Harry Winston was the first American jeweler to own and cut some of the most iconic stones in history, in addi- tion to setting a new standard for jewelry that showcases a gem’s natural beauty. Born more than a century ago, the young Winston—the son of a small jewelry shop owner—demonstrated a natural instinct for examining diamonds and precious gems. In subsequent years, he cultivated this talent to become one of the most prominent diamond merchants and designers of his time. His legacy lives on through the house of Harry Winston, which pairs his classic vision with a contemporary sensi- bility to create modern pieces that still grace the red carpet today.
    [Show full text]