General Information- Michigan's Gem Stones
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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. -
Compilation of Reported Sapphire Occurrences in Montana
Report of Investigation 23 Compilation of Reported Sapphire Occurrences in Montana Richard B. Berg 2015 Cover photo by Richard Berg. Sapphires (very pale green and colorless) concentrated by panning. The small red grains are garnets, commonly found with sapphires in western Montana, and the black sand is mainly magnetite. Compilation of Reported Sapphire Occurrences, RI 23 Compilation of Reported Sapphire Occurrences in Montana Richard B. Berg Montana Bureau of Mines and Geology MBMG Report of Investigation 23 2015 i Compilation of Reported Sapphire Occurrences, RI 23 TABLE OF CONTENTS Introduction ............................................................................................................................1 Descriptions of Occurrences ..................................................................................................7 Selected Bibliography of Articles on Montana Sapphires ................................................... 75 General Montana ............................................................................................................75 Yogo ................................................................................................................................ 75 Southwestern Montana Alluvial Deposits........................................................................ 76 Specifi cally Rock Creek sapphire district ........................................................................ 76 Specifi cally Dry Cottonwood Creek deposit and the Butte area .................................... -
Origin of Fibrosity and Banding in Agates from Flood Basalts: American Journal of Science, V
Agates: a literature review and Electron Backscatter Diffraction study of Lake Superior agates Timothy J. Beaster Senior Integrative Exercise March 9, 2005 Submitted in partial fulfillment of the requirements for a Bachelor of Arts degree from Carleton College, Northfield, Minnesota. 2 Table of Contents AGATES: A LITERATURE REVEW………………………………………...……..3 Introduction………………....………………………………………………….4 Structural and compositional description of agates………………..………..6 Some problems concerning agate genesis………………………..…………..11 Silica Sources…………………………………………..………………11 Method of Deposition………………………………………………….13 Temperature of Formation…………………………………………….16 Age of Agates…………………………………………………………..17 LAKE SUPERIOR AGATES: AN ELECTRON BACKSCATTER DIFFRACTION (EBSD) ANALYSIS …………………………………………………………………..19 Abstract………………………………………………………………………...19 Introduction……………………………………………………………………19 Geologic setting………………………………………………………………...20 Methods……………………………………………………...…………………20 Results………………………………………………………….………………22 Discussion………………………………………………………………………26 Conclusions………………………………………………….…………………26 Acknowledgments……………………………………………………..………………28 References………………………………………………………………..……………28 3 Agates: a literature review and Electron Backscatter Diffraction study of Lake Superior agates Timothy J. Beaster Carleton College Senior Integrative Exercise March 9, 2005 Advisor: Cam Davidson 4 AGATES: A LITERATURE REVEW Introduction Agates, valued as semiprecious gemstones for their colorful, intricate banding, (Fig.1) are microcrystalline quartz nodules found in veins and cavities -
The Lake Superior Agate
Minnesota Gem: The Lake Superior Agate Its wide distribution and iron-rich bands of color reflect the state gemstone's geologic history in Minnesota Scott F. Wolter N 1969 the dream of Mrs. Jean it was the best choice. The agate IDahlberg was realized: The Lake reflects many aspects of Minnesota. Superior agate was designated by the It was formed during violent, fiery lava Minnesota Legislature as the official eruptions that occurred in our state state gemstone. about a billion years ago. The stone's The late Mrs. Dahlberg, long-time predominant red color comes from rock hound and ardent fan of the agate, iron, the major industrial mineral in testified before the state legislative our state. Finally, the widely distrib- committee considering the bill. She uted agate reveals the impact of gla- knew how perfect the Lake Superior cial movement across Minnesota agate was for the state gemstone. 10,000 to 15,000 years ago. However, there were other logical The Lake Superior agate is inti- candidates. The brazen red Bing- mately related to two prominent geo- hamite and blazing yellow silkstone, logic features of Minnesota: the both iron-rich jaspers found in the majestic and rugged lava flows Cuyuna iron range area, were logical exposed along the shoreline of Lake selections. Thompsonite, the beau- Superior and the lake-freckled glacial tiful and popular zeolite mineral found debris that covers nearly all the state. only in Minnesota on an isolated More than a billion years ago, the stretch along Lake Superior, was North American continent began to another strong candidate. -
Evaluation of Brilliance, Fire, and Scintillation in Round Brilliant
Optical Engineering 46͑9͒, 093604 ͑September 2007͒ Evaluation of brilliance, fire, and scintillation in round brilliant gemstones Jose Sasian, FELLOW SPIE Abstract. We discuss several illumination effects in gemstones and University of Arizona present maps to evaluate them. The matrices and tilt views of these College of Optical Sciences maps permit one to find the stones that perform best in terms of illumi- 1630 East University Boulevard nation properties. By using the concepts of the main cutter’s line, and the Tucson, Arizona 85721 anti-cutter’s line, the problem of finding the best stones is reduced by E-mail: [email protected] one dimension in the cutter’s space. For the first time it is clearly shown why the Tolkowsky cut, and other cuts adjacent to it along the main cutter’s line, is one of the best round brilliant cuts. The maps we intro- Jason Quick duce are a valuable educational tool, provide a basis for gemstone grad- Jacob Sheffield ing, and are useful in the jewelry industry to assess gemstone American Gem Society Laboratories performance. © 2007 Society of Photo-Optical Instrumentation Engineers. 8917 West Sahara Avenue ͓DOI: 10.1117/1.2769018͔ Las Vegas, Nevada 89117 Subject terms: gemstone evaluation; gemstone grading; gemstone brilliance; gemstone fire; gemstone scintillation; gemstone cuts; round brilliant; gemstones; diamond cuts; diamonds. James Caudill American Gem Society Advanced Instruments Paper 060668R received Aug. 28, 2006; revised manuscript received Feb. 16, 8881 West Sahara Avenue 2007; accepted for publication Apr. 10, 2007; published online Oct. 1, 2007. Las Vegas, Nevada 89117 Peter Yantzer American Gem Society Laboratories 8917 West Sahara Avenue Las Vegas, Nevada 89117 1 Introduction are refracted out of the stone. -
Quartz: a Bull's Eye on Optical Activity
Quartz: a Bull’s Eye on Optical Activity Elise A. Skalwold The Mineralogical Society of America William A. Bassett Title: Quartz: a Bull’s Eye on Optical Activity Authors: Elise Ann Skalwold & William Akers Bassett Edition: First edition Publisher: Mineralogical Society of America, Chantilly, Virginia, USA Copyright: © 2015 by the authors, artists, and photographers. Reproduced with permission. All Rights Reserved. ISBN: 978-0-939950-00-3 Photographer & Designer: Elise A. Skalwold Front cover: Natural quartz crystal 60 x 65 x 40 mm; Hot Springs, Arkansas; ex. Dr. R.W.M. Woodside collection. Back cover: Lab-grown quartz cluster, 140 mm x 90 mm (hydrothermally grown by Mila and Vladimir A. Klipov, R&D XTALS, Inc.). Below: Natural quartz crystals and basal sections. On-going collaboration with Cornell’s Professor Emeritus William A. Bassett is truly priceless to me for this and other projects in the wings, as well as for those over the past eight years of work and research together. Bill shares my enthusi- asm for exploring the fascinating aspects of the classical science of mineralogy, and as my co-author he sets the highest bar for accuracy. All students should be so lucky to have such a mentor. Elise A. Skalwold, 2015 Ithaca, New York Mineralogical Society of America Quartz: a Bull’s Eye on Optical Activity Elise A. Skalwold [email protected] William A. Bassett [email protected] Both Authors: Department of Earth & Atmospheric Sciences Snee Hall, Cornell University Ithaca, NY 14853 All photographs: Elise A. Skalwold Figure 1. The “bull’s eye” uniaxial optic figure characteristic of quartz is indicative of its optical activity. -
Gemology with Kelly Sitek Ologies Podcast October 10, 2017
Gemology with Kelly Sitek Ologies Podcast October 10, 2017 Heeey, okay just a quick note up top, that this episode gets a little, like, woo-doo-to-doo, like a little mystical. We don’t not talk about the power of crystals in this. I wanted to know, as a gemologist, what this Ologist’s belief was in the mystical nature of rocks, if she believed in it. So, I hear her out, I also discuss the neuroscience of the placebo effect and how our thoughts can change our behaviors. It’s based in neuroscience. Try not to @ me about it ‘cause, like, I get it. Okay? Cool Episode 4 of Ologies, comin’ in hawt. First off, thanks to everyone who’s been listening and leaving reviews on iTunes, and rating, and subscribing. The more you do that, the higher this gets on the charts and the more people see it. And the more people share dumb science jokes, I guess, the better. I don't know. Also thank you to everyone who’s supporting on Patreon. I see you and I love you. And For everyone who had a hankering for merch and who’s been to OlogiesMerch.com. Cool shirt, or mug, or tote. Okay. Gems. This episode about gems is truly outrageous. Well, it’s pretty good. We don’t talk about crotches very much, but it's a pretty good episode. Let’s start with the etymology of gemology, it comes from ‘ology,’ the study of, and ‘gems,’ meaning gems. But ‘gems’ comes from an old dusty Latin word for.. -
Weight of Production of Emeralds, Rubies, Sapphires, and Tanzanite from 1995 Through 2005
Weight of Production of Emeralds, Rubies, Sapphires, and Tanzanite from 1995 Through 2005 By Thomas R. Yager, W. David Menzie, and Donald W. Olson Open-File Report 2008–1013 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior DIRK KEMPTHORNE, Secretary U.S. Geological Survey Mark D. Myers, Director U.S. Geological Survey, Reston, Virginia: 2008 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Suggested citation: Yager, T.R., Menzie, W.D., and Olson, D. W., 2008, Weight of production of emeralds, rubies, sapphires, and tanzanite from 1995 through 2005: U.S. Geological Survey Open-File Report 2008-1013, 9 p., available only online, http://pubs.usgs.gov/of/2008/1013. Any use of trade, product, or firm names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. ii Contents Introduction ...................................................................................................................................1 Emeralds.......................................................................................................................................2 -
Thunder Bay Agate Mine
Thunder Bay Agate Mine Last Spring I lead a group of undergraduate geology students around Lake Superior. One of the best stops we had was at the Thunder Bay Agate Mine. As it is right on the way to the better-known amethyst mines, I'd recommend all headed up that way stop for a visit. The mine is a dig-your-own fee area. It is located just a few miles north of Thunder Bay, just north-east of the Terry Fox Monument (another place that is worth a stop). A mile or so east of the monument on Hwy. 11-17, turn left on highway 527. There is an agate mine sign at the intersection, so it is hard to miss. The mine is about 1/2 mile up 527, on the left. That turn off is also well marked. There is a big parking area by their shop. You can walk or drive down a short distance down a well maintained dirt road to the mine from there. We were greeted and given a tour of the shop and the deposit. The students then got to go to work. The fee is $8 per pound, with the price pro-rated to reflect the poundage of agate rather than the surrounding matrix. There is a reduced rate for clubs. There was agate all over the place, and it could be collected without much in the way of tools. If you want to pound, well, there was opportunity for that too. The agate is a seam or vein agate, formed in brecciated iron carbonate of the Proterozoic Gunflint Formation. -
1 Optical Properties of Gem Substances
Optical Properties of Gem Substances Educational objective: This exercise, unit 7 in the above syllabus, will introduce students to skills and equipment that will continue to be used throughout the following modules. You should attempt to master these skills and the use of the equipment. The student should become familiar with the equipment, its application to solving gem problems, its proper use, and the precautions necessary to ensure both the safety of the student and the equipment. This lab may take up to two full meetings. Depending on equipment availability and time one or two setups for each experiment may be present. For each lab experiment, the student group will consist of 2 students. Groups are requested to make a 5 to 10 minute presentation using the digital Elmo overhead projector or a series of digital images (as in previous labs). There are some guiding questions for each exercise, but your overall grade is based on your presentation and discussion ensuing from it, plus observations of your behavior and preparedness in the lab. Images for your presentation are available in a “lab library” of images that you can pick and choose from as you see fit. The order in which the experiments will be presented does not have to correspond with the order they are presented here. 1. Refraction and the critical angle. Objectives. To observe the change in light’s path as it moves from one substance to another, record the angle of incidence and refraction, see total internal reflection, attempt to measure the critical angle, and learn about refractive index. -
Spring 2002 Gems & Gemology
Spring 2002 VOLUME 38, NO. 1 EDITORIAL 1 Richard T. Liddicoat: Celebrating 50 Years of Leadership William E. Boyajian FEATURE ARTICLES 2 The Ultimate Gemologist: A Tribute to Richard T. Liddicoat Dona M. Dirlam, James E. Shigley, and Stuart D. Overlin A look at the extraordinary career of Richard Liddicoat. 14 Portable Instruments and Tips on Practical Gemology in the Field Edward W. Boehm An essential guide to the use of portable instruments when purchasing gems. 28 Liddicoatite Tourmaline from Anjanabonoina, Madagascar Dona M. Dirlam, Brendan M. Laurs, Federico Pezzotta, and William B. (Skip) Simmons pg. 3 Explores the world’s primary source of this remarkable calcium-rich lithium tourmaline, named in honor of Richard T. Liddicoat. 54 Star of the South: A Historic 128 ct Diamond Christopher P. Smith and George Bosshart A history and characterization of this famous diamond. NOTES AND NEW TECHNIQUES 66 Identification of Yellow Cultured Pearls from the Black-Lipped Oyster Pinctada Margaritifera Shane Elen How absorption features can establish the origin of these cultured pearls. pg. 22 73 Serendibite from Sri Lanka Karl Schmetzer, George Bosshart, Heinz-Jürgen Bernhardt, Edward J. Gübelin, and Christopher P. Smith A characterization of this rare gem material from Sri Lanka. REGULAR FEATURES 80 Gem Trade Lab Notes • Color grade vs. value for fancy-color diamonds • Diamond with eclogitic inclusions • Diamond with a large void • Genthelvite: A second occurrence • Jadeite carving: Assembled, dyed, and impregnated • Coated natural pearls • -
Pamphlet 4: Collecting Minerals in Michigan
Pamphlet 4 Make a point of visiting and using the museums listed on page 7. The finest specimens find their way eventually COLLECTING MINERALS IN MICHIGAN into these institutions. Likely you will be able to obtain information on nearby societies, and perhaps purchase by R. W. Kelley and H. J. Hardenburg, Geologists some literature or other material. Lansing, MI If the bug bites you, you will also probably want to subscribe to a periodical. Some of the more popular ones April, 1962 are shown on page 7. CLASSWORK Eventually you may wish to take courses of instruction in the lapidary arts, mineralogy, or geology. Inquiries relating to the various possibilities should be directed to colleges, local schools, museums, and clubs. Some dealers, too, provide class sessions. Before investing in expensive equipment, beginners would do well to get From Pebble to Pendant some actual practice at available training facilities. You'll be the wiser for this experience when it comes to selecting things needed for your chosen activities. INTRODUCTION Many people are just beginning to discover how VARIETY OF INTERESTS interesting stones can be. The last few years have seen a tremendous growth in the number, hobbyists and Some hobbyists become known as collectors because otherwise, who are now collecting rocks and minerals, their interest lies mostly in the acquisition of specimens. often converting their finds into attractive display pieces Their reward is to behold the enchanting colors and forms and jewelry. Much can be said in favor of these of nature's minerals. Collectors, however, often become fascinating pursuits but we won’t discuss that here.