Quartzite: Classically Beautiful Like Marble, but Strong and Unflappable Like Granite
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How to Identify Rocks and Minerals
How to Identify Rocks and Minerals fluorite calcite epidote quartz gypsum pyrite copper fluorite galena By Jan C. Rasmussen (Revised from a booklet by Susan Celestian) 2012 Donations for reproduction from: Freeport McMoRan Copper & Gold Foundation Friends of the Arizona Mining & Mineral Museum Wickenburg Gem & Mineral Society www.janrasmussen.com ii NUMERICAL LIST OF ROCKS & MINERALS IN KIT See final pages of book for color photographs of rocks and minerals. MINERALS: IGNEOUS ROCKS: 1 Talc 2 Gypsum 50 Apache Tear 3 Calcite 51 Basalt 4 Fluorite 52 Pumice 5 Apatite* 53 Perlite 6 Orthoclase (feldspar group) 54 Obsidian 7 Quartz 55 Tuff 8 Topaz* 56 Rhyolite 9 Corundum* 57 Granite 10 Diamond* 11 Chrysocolla (blue) 12 Azurite (dark blue) METAMORPHIC ROCKS: 13 Quartz, var. chalcedony 14 Chalcopyrite (brassy) 60 Quartzite* 15 Barite 61 Schist 16 Galena (metallic) 62 Marble 17 Hematite 63 Slate* 18 Garnet 64 Gneiss 19 Magnetite 65 Metaconglomerate* 20 Serpentine 66 Phyllite 21 Malachite (green) (20) (Serpentinite)* 22 Muscovite (mica group) 23 Bornite (peacock tarnish) 24 Halite (table salt) SEDIMENTARY ROCKS: 25 Cuprite 26 Limonite (Goethite) 70 Sandstone 27 Pyrite (brassy) 71 Limestone 28 Peridot 72 Travertine (onyx) 29 Gold* 73 Conglomerate 30 Copper (refined) 74 Breccia 31 Glauberite pseudomorph 75 Shale 32 Sulfur 76 Silicified Wood 33 Quartz, var. rose (Quartz, var. chert) 34 Quartz, var. amethyst 77 Coal 35 Hornblende* 78 Diatomite 36 Tourmaline* 37 Graphite* 38 Sphalerite* *= not generally in kits. Minerals numbered 39 Biotite* 8-10, 25, 29, 35-40 are listed for information 40 Dolomite* only. www.janrasmussen.com iii ALPHABETICAL LIST OF ROCKS & MINERALS IN KIT See final pages of book for color photographs of rocks and minerals. -
Crystalline Silica, Cristobalite (CAS No
Crystalline Silica, Quartz (CAS No. 14808-60-7) Crystalline Silica, Cristobalite (CAS No. 14464-46-1) Crystalline Silica, Tridymite (CAS No. 15468-32-3) Diatomaceous earth (CAS No. 61790-53-2) This dossier on crystalline silica, quartz, cristobalite and tridymite and diatomaceous earth presents the most critical studies pertinent to the risk assessment of these substances in their use in drilling muds and cement additives. This dossier does not represent an exhaustive or critical review of all available data. The majority of information presented in this dossier was obtained from the ECHA database that provides information on chemicals that have been registered under the EU REACH (ECHA). Where possible, study quality was evaluated using the Klimisch scoring system (Klimisch et al., 1997). For the purpose of this dossier, crystalline silica, quartz (CAS No. 14808-60-7) has been reviewed as representative of crystalline silica cristobalite and tridymite. Crystalline silica, quartz is also considered representative of diatomaceous earth, as they both consist mainly of silicon dioxide. Screening Assessment Conclusion – Crystalline silica, quartz, cristobalite and tridymite and diatomaceous earth are classified as tier 1 chemicals and require a hazard assessment only. 1 BACKGROUND Crystalline silica is a common mineral found in the earth's crust. Materials like sand, stone, concrete and mortar contain crystalline silica. It is also used to make products such as glass, pottery, ceramics, bricks and artificial stone. Silica, in the form of sand, is used as the main ingredient in sand casting for the manufacture of metallic components in engineering and other applications. The high melting point of silica enables it to be used in such applications. -
Bedrock Geology Glossary from the Roadside Geology of Minnesota, Richard W
Minnesota Bedrock Geology Glossary From the Roadside Geology of Minnesota, Richard W. Ojakangas Sedimentary Rock Types in Minnesota Rocks that formed from the consolidation of loose sediment Conglomerate: A coarse-grained sedimentary rock composed of pebbles, cobbles, or boul- ders set in a fine-grained matrix of silt and sand. Dolostone: A sedimentary rock composed of the mineral dolomite, a calcium magnesium car- bonate. Graywacke: A sedimentary rock made primarily of mud and sand, often deposited by turbidi- ty currents. Iron-formation: A thinly bedded sedimentary rock containing more than 15 percent iron. Limestone: A sedimentary rock composed of calcium carbonate. Mudstone: A sedimentary rock composed of mud. Sandstone: A sedimentary rock made primarily of sand. Shale: A deposit of clay, silt, or mud solidified into more or less a solid rock. Siltstone: A sedimentary rock made primarily of sand. Igneous and Volcanic Rock Types in Minnesota Rocks that solidified from cooling of molten magma Basalt: A black or dark grey volcanic rock that consists mainly of microscopic crystals of pla- gioclase feldspar, pyroxene, and perhaps olivine. Diorite: A plutonic igneous rock intermediate in composition between granite and gabbro. Gabbro: A dark igneous rock consisting mainly of plagioclase and pyroxene in crystals large enough to see with a simple magnifier. Gabbro has the same composition as basalt but contains much larger mineral grains because it cooled at depth over a longer period of time. Granite: An igneous rock composed mostly of orthoclase feldspar and quartz in grains large enough to see without using a magnifier. Most granites also contain mica and amphibole Rhyolite: A felsic (light-colored) volcanic rock, the extrusive equivalent of granite. -
Lithics, Landscape and People: Life Beyond the Monuments in Prehistoric Guernsey
UNIVERSITY OF SOUTHAMPTON FACULTY OF HUMANITIES Department of Archaeology Lithics, Landscape and People: Life Beyond the Monuments in Prehistoric Guernsey by Donovan William Hawley Thesis for the degree of Doctor of Philosophy April 2017 UNIVERSITY OF SOUTHAMPTON ABSTRACT FACULTY OF HUMANITIES Archaeology Thesis for the degree of Doctor of Philosophy Lithics, Landscape and People: Life Beyond the Monuments in Prehistoric Guernsey Donovan William Hawley Although prehistoric megalithic monuments dominate the landscape of Guernsey, these have yielded little information concerning the Mesolithic, Neolithic and Early Bronze Age communities who inhabited the island in a broader landscape and maritime context. For this thesis it was therefore considered timely to explore the alternative material culture resource of worked flint and stone archived in the Guernsey museum. Largely ignored in previous archaeological narratives on the island or considered as unreliable data, the argument made in this thesis is for lithics being an ideal resource that, when correctly interrogated, can inform us of past people’s actions in the landscape. In order to maximise the amount of obtainable data, the lithics were subjected to a wide ranging multi-method approach encompassing all stages of the châine opératoire from material acquisition to discard, along with a consideration of the landscape context from which the material was recovered. The methodology also incorporated the extensive corpus of lithic knowledge that has been built up on the adjacent French mainland, a resource largely passed over in previous Channel Island research. By employing this approach, previously unknown patterns of human occupation and activity on the island, and the extent and temporality of maritime connectivity between Guernsey and mainland areas has been revealed. -
Graveyard Geology
GRAVEYARD GEOLOGY A Guide to Rocks in Graveyards and Cemeteries Wendy Kirk Department of Earth Sciences, David Cook University College London & Aldersbrook Geological Society London Geodiversity Partnership Introduction Walk around graveyards and cemeteries (in this case, those of London and the southeast of England) and it becomes apparent that, prior to the latter part of the twentieth century, many memorials were made out of just a few different rock types. These were chosen for reasons of appearance, cost, workability and ease of transport to the cemetery, as well as for resistance to weathering and dependence on local regulations. In the last few decades, a range of different, interesting and beautiful stones have appeared, many brought in from abroad, enhancing the diversity of materials used. The intention of this guide is to help a non-specialist identify the main rock types, to recognize some of the varieties and to know where some of these might have come from. Graveyards are a wonderful resource for those with an interest in geology at any level, wildlife, plants, history or sculpture. We hope you gain as much pleasure as we have done. First things first A useful place to start is to be able to distinguish between igneous, sedimentary and metamorphic rocks. Igneous rocks form from melted rock called magma. If this erupts at the surface, it is called lava. It cools and crystallizes quickly, so the grains are too small to see even with a hand lens (magnifying glass). If the lava erupt explosively to form a spray, the cooled fragments are known as volcanic ash. -
Slabs | Tiles | Accessories Bring Your Vision to Life
SLABS | TILES | ACCESSORIES BRING YOUR VISION TO LIFE ¨STONES MARBLE ONYX LIMESTONE GRANITE TRAVERTINE QUARTZITE SEMI-PRECIOUS SPECIALTY STONE SLATE AGGLOMERATES MOSAICS MAGNUM OPUSTONE There is nothing quite like it. When you encounter the ideal stone, nothing else even comes close. More than just color, tone, texture and complexity, our stone must possess a certain character that elevates it and brings it to life. Richness, depth, a soul. We travel the globe to source the finest possible stones in a relentless pursuit of perfection. From quarry to quarry, we seek out and purchase the very best, the most distinctive, the only stones worthy of being Opustone. And we back it up with phenomenal industry-leading service, the kind of service you would only expect from a company that brings you the finest stones on earth. After all, we are not merely distributors of natural and manufactured stone. We assemble a distinctive, natural palette of materials for the design and creation of unique living spaces. Our stones were destined to be lived with. Nothing but Opustone will ever do. ¨GRANITE ¨MARBLE LEGENDARY AND TIMELESS. DESIGNED BY NATURE TO DEFINE THE SPACES WHERE HISTORY TAKES PLACE. ONYX¨ DEEP AND PONDEROUS. LOOK CLOSELY AND DISCOVER VAST WORLDS WITHIN. ¨LIMESTONE DEFINE YOUR SPACE WITH SUBTLE COLORS AND COMPLEX TEXTURES. BEAUTY ENDURES, SOLID AND ETERNAL, GRANITE¨ WAVES OF COLOR MELDING INTO ONE. COMPLEXITY IN ITS MOST SIMPLE FORM. ¨TRAVERTINE QUARTZITE¨ A DRAMATIC EXPERIENCE IN RICH TONES AND STRIKING DETAIL. ¨SEMI-PRECIOUS TRANSCENDING TIME WHERE. VISIONS BECOME REALITY. SPECIALTY STONE¨ ELEGANCE THAT GOES WELL BEYOND THE GOES WELL BEYOND ELEGANCE THAT OF THE ORDINARY. -
Building Stones of the National Mall
The Geological Society of America Field Guide 40 2015 Building stones of the National Mall Richard A. Livingston Materials Science and Engineering Department, University of Maryland, College Park, Maryland 20742, USA Carol A. Grissom Smithsonian Museum Conservation Institute, 4210 Silver Hill Road, Suitland, Maryland 20746, USA Emily M. Aloiz John Milner Associates Preservation, 3200 Lee Highway, Arlington, Virginia 22207, USA ABSTRACT This guide accompanies a walking tour of sites where masonry was employed on or near the National Mall in Washington, D.C. It begins with an overview of the geological setting of the city and development of the Mall. Each federal monument or building on the tour is briefly described, followed by information about its exterior stonework. The focus is on masonry buildings of the Smithsonian Institution, which date from 1847 with the inception of construction for the Smithsonian Castle and continue up to completion of the National Museum of the American Indian in 2004. The building stones on the tour are representative of the development of the Ameri can dimension stone industry with respect to geology, quarrying techniques, and style over more than two centuries. Details are provided for locally quarried stones used for the earliest buildings in the capital, including A quia Creek sandstone (U.S. Capitol and Patent Office Building), Seneca Red sandstone (Smithsonian Castle), Cockeysville Marble (Washington Monument), and Piedmont bedrock (lockkeeper's house). Fol lowing improvement in the transportation system, buildings and monuments were constructed with stones from other regions, including Shelburne Marble from Ver mont, Salem Limestone from Indiana, Holston Limestone from Tennessee, Kasota stone from Minnesota, and a variety of granites from several states. -
Revisions to the Nonmetallic Mineral Processing Plants (Subpart OOO) NSPS
Economic and Small Business Analysis – Revisions to the Nonmetallic Mineral Processing Plants (Subpart OOO) NSPS EPA-452/R-09-003 April 2009 Economic and Small Business Analysis – Revisions to the Nonmetallic Mineral Processing Plants (Subpart OOO) NSPS By: U.S. Environmental Protection Agency Office of Air Quality Planning and Standards Research Triangle Park, North Carolina U.S. Environmental Protection Agency Office of Air Quality Planning and Standards Health and Environmental Impacts Division Air Benefits and Costs Group Research Triangle Park, NC 2 SECTION 1 INTRODUCTION To meet the requirements of section 111(b)(1)(B) of the CAA, the Environmental Protection Agency (EPA) is currently conducting the second review of the new source performance standards (NSPS) for non-metallic mineral processing plants (NMPP). The NMPP NSPS was promulgated on August 1, 1985 (40 CFR Part 60 subpart OOO, 50 FR 31328) and subsequently reviewed in 1997. Subpart OOO requires new, modified, or reconstructed affected facilities at NMPP to achieve emission levels that reflect the best demonstrated system of continuous emission reduction, considering cost, non-air quality health, environmental, and energy impacts. These emission levels, referred to as “best demonstrated technology (BDT),” are specified in subpart OOO. The purpose of this report is to provide economic and small business impact analyses for the requirements of this NSPS. We include revenue and other economic data for affected industries and businesses in the industry profile for this NSPS, and that profile is included in this report. The analysis will focus on estimating such impacts by providing annualized cost as a percent of sales or revenues for firms in industries likely to be affected by this NSPS. -
Dimension Stone Feasibility Study
DIMENSION STONE FEASIBILITY STUDY: DEVELOPMENT POTENTIAL IN MICHIGAN'S UPPER PENINSULA H. James Bourque and Associates 402 Ashmun Street, P.O. Box 292 Sault Ste. Marie, MI 49783 (906) 635-9191 July 1, 1999 Page 2 Table of Contents Acknowledgements ................................................................................................... 4 Project Background.................................................................................................... 5 In Recent Years . ...................................................................................................... 5 Study Methods............................................................................................................ 7 Geology of the Upper Peninsula................................................................................. 7 Dimension Stone Production ...................................................................................... 8 1997 Dimension Stone Production By Types: ...........................................................9 Dimension Stone Pricing ...........................................................................................11 Sandstone ..............................................................................................................12 Granite...................................................................................................................12 Limestone ..............................................................................................................12 Stone Sites Investigated -
BUIL])ING STON.E O·F WASHINGTON
BUIL])ING STON.E o·f WASHINGTON By WAYNE S. MOEN Washington Department of Conservation Division of Mines and Geology Bulletin No. 55 1967 State of Washington DANIEL J. EV ANS, Governor Department of Conservation H. MAURICE AHLQUIST, Director DIVISION OF MINES AND GEOLOGY MARSHALL T. HUNTTING, Supervisor Bulletin No. 55 BUILDING STONE OF WASHINGTON By WAYNE S. MOEN STATE PRINTING PLANT. OLYMPI A , WASHINGTON 1967 For sale by Department Pof? ceConsl]SliARYervation, Olympia, Washington. PACIFIC NORTHWEST FOREST AND RANGE EXPERIMENT STATION etnDTLAND. OR£00N CONTENTS Poge Introduction 7 General history .. ...... ...........................•............ 8 Production and vo lue . 10 Forms of building stone . 12 Field stone . 12 Rough building stone . 13 Rubble . • . 14 Flogging (flagstone) . 14 Ashlar . .. ......... ........ , ................. , . , . 15 Crushed stone . 16 Terrozzo . 17 Roofing granules.............. .... ..... ......... 18 Exposed aggregate . 18 Reconstituted stone . • . 19 Landscape rock . 20 Area coverage of bui Iding stone . 21 Acquisition of bui )ding stone . 22 Examination of stone deposits . 23 General quarrying methods . 24 Physical properties of building stone . 26 Strength . 26 Hardness and workabi Iity . • . 27 Color . 28 Alteration ....•...................... , ........... , . 29 Porosity and absorption ...........•. : . 31 Testing of building stone... .. .................... ................ 33 Common building stones of Washington . 34 Granite . 35 Geology and distribution . 35 Physical properties . 38 Varieties -
List of Stones
LIST OF STONES cognac colour diamond DN prehnite PR diamond D pyrite PY, MA heat enhanced black diamond DB quartzite QW amazonite AZ treated quartz RA amber AMB, R rhodolite RHL, RHG, RHP amethyst AM, AMP rock crystal RC, BK aquamarine AQ rose quartz RQ black onyx ON, O ruby RU black spinel SPB, ME sapphire SA black/white agate cameo CAM smoky quartz SQ blue topaz BTP, TPA smoky quartz/mother of pearl doublet P carnelian CAR, K tanzanite TZ chalcedony CA tourmalinated quartz BRU chrysoprase CH treated quartz RA citrine CI, CIG, CIC, CIY treated topaz, paraiba blue TPP cognac quartz CQ treated topaz, pink TPK garnet GR, GA treated pink sapphire PSA green quartz GQ, GAM turquoise TQ grey moonstone MSG whisky quartz WQ, BQ hematite HEM white agate AGW iolite IO, IOB white opal WOP labradorite LBG black crystal NCK lapis lazuli LP, L black cubic zirconia CZK lemon quartz LQ blue cubic zirconia CZB light colour amethyst PAM brown cubic zirconia BCZ moonstone MS champagne coloured cubic zirconia CCZ nephrite-jade NJA cubic zirconia CZ orange moonstone MSO dark blue synthetic spinel SSB peridot PE, PEA dark green cubic zirconia CZN pink opal POP green cubic zirconia GCZ pink rock PRO, RNI grey crystal NGY pink sapphire PSA honey cubic zirconia CZM pink tourmaline TU lavender cubic zirconia LCZ light blue cubic zirconia CZA copper coloured cultured pearl PRC, RRC light blue synthetic spinel SSL golden mabe cultured pearl PGO light rose cubic zirconia TCZ green cultured pearl PG lime cubic zirkonia CZL grey faceted cultured pearl PSG orange cubic -
Geological Field Trip 1 from Opals and Ancient Mountaintops to Ice Age Lakes Guide Written by Dr
1 Geological Field Trip 1 From Opals and Ancient Mountaintops to Ice Age Lakes Guide written by Dr. E.K. Peters WSU Geology Department OVERVIEW: The first portion of the trip is in central Pullman and may be most easily accomplished on foot. It consists of five stops, "A" through "E," and can be done in an hour or two. The rest of the trip requires a vehicle and will take the remainder of a long day. SKETCH MAP OF THE TRIP Start: Kate Webster Physical Science Building, WSU-Pullman Campus, College Avenue Proceed west on the service portion of College Avenue, under the skywalk of Owen Science Library and then onto the regular section of College Avenue. Continue west, going downhill. The steepest portion of College Avenue takes you 2 past engineering buildings on your right and then by WSU's power plant at the bottom of the hill. Stop A: Depending on the season, you may see large piles of bituminous coal at the power plant. Coal is the compressed and compacted remains of ancient plants. You can think of it as fossil plant matter, made mostly of carbon. There are three common grades of coal used in the world: 1. Brown coal or lignite: this is low grade coal. It has abundant nitrogen and sulfur impurities. It therefore does not burn cleanly. The nitrogen and sulfur compounds go up in the smoke and then combine with water droplets in the air to make "acid rain" (small amounts of nitric and sulfuric acids). Lignite (brown coal) is used in China today, but not in the U.S.