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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. -
Geologic Storage Formation Classification: Understanding Its Importance and Impacts on CCS Opportunities in the United States
BEST PRACTICES for: Geologic Storage Formation Classification: Understanding Its Importance and Impacts on CCS Opportunities in the United States First Edition Disclaimer This report was prepared as an account of work sponsored by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor any of their employees, makes any warranty, express or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe privately owned rights. Reference therein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof. The views and opinions of authors expressed therein do not necessarily state or reflect those of the United States Government or any agency thereof. Cover Photos—Credits for images shown on the cover are noted with the corresponding figures within this document. Geologic Storage Formation Classification: Understanding Its Importance and Impacts on CCS Opportunities in the United States September 2010 National Energy Technology Laboratory www.netl.doe.gov DOE/NETL-2010/1420 Table of Contents Table of Contents 5 Table of Contents Executive Summary ____________________________________________________________________________ 10 1.0 Introduction and Background -
Mirabilite Na2so4 • 10H2O C 2001-2005 Mineral Data Publishing, Version 1
Mirabilite Na2SO4 • 10H2O c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Monoclinic. Point Group: 2/m. Crystals short to long prismatic, with complex form development, also crude, to 10 cm, in interlocking masses; crystalline, granular to compact massive, commonly as efflorescences. Twinning: Rare on {001} or {100}. Physical Properties: Cleavage: On {100}, perfect; on {010} and {001}, good to fair. Fracture: Conchoidal. Hardness = 1.5–2.5 D(meas.) = 1.464 D(calc.) = 1.467 Quickly dehydrates to th´enarditein dry air; very soluble in H2O, taste cool, then saline and bitter. Optical Properties: Transparent to opaque. Color: Colorless to white; colorless in transmitted light. Streak: White. Luster: Vitreous. Optical Class: Biaxial (–). Orientation: X = b; Z ∧ c =31◦. Dispersion: r< v,strong, crossed. α = 1.391–1.394 β = 1.394–1.396 γ = 1.396–1.398 2V(meas.) = 75◦560 Cell Data: Space Group: P 21/c (synthetic). a = 11.512(3) b = 10.370(3) c = 12.847(2) β = 107.789(10)◦ Z=4 X-ray Powder Pattern: Synthetic. (ICDD 11-647). 5.49 (100), 3.21 (75), 3.26 (60), 3.11 (60), 4.77 (45), 3.83 (40), 2.516 (35) Chemistry: (1) (2) SO3 25.16 24.85 Na2O 18.67 19.24 H2O 55.28 55.91 Total 99.11 100.00 • (1) Kirkby Thore, Westmoreland, England. (2) Na2SO4 10H2O. Occurrence: Typically in salt pans, playas, and saline lakes, where deposition may be seasonal, and bedded deposits formed therefrom; rarely in caves and lava tubes; in volcanic fumaroles; a product of hydrothermal sericitic alteration; a post-mining precipitate. -
Non-Clastic Sedimentary Rocks by Cindy Grigg
Non-Clastic Sedimentary Rocks By Cindy Grigg 1 Rocks can be put into three main groups. They are grouped by how the rocks formed. Sedimentary (sed-uh-MEN-tuh-ree) rocks are formed on or near Earth's surface. Sedimentary rocks are sorted into other groups. They can be sorted as clastic or non-clastic. This group tells something about the rocks' beginning and what they formed from. 2 Non-clastic rocks are created when water evaporates or from the remains of plants and animals. Limestone is a non-clastic sedimentary rock. Limestone is made of the mineral calcite. It often contains fossils. Limestone formed in the ocean from the shells and skeletons of dead sea creatures. Some of the fossils in limestone are too small to be seen without a microscope. Chalk is a type of limestone that is usually white. It consists almost entirely of the shells of tiny dead sea creatures. Limestone is a common building material. 3 Coal is another non-clastic rock. It formed from the dead remains of plants. Millions of years ago, plants fell into swamps. They were covered with layers of sediment and did not rot. Over millions of years, as the remains were buried deeper under more and more layers of sediment, they were changed by pressure into coal. Coal is commonly used as fuel in power plants to make electricity. 4 Evaporite rocks formed when minerals such as gypsum and halite (rock salt) were left behind as water evaporated from oceans and lakes. Evaporite is common in desert areas, where evaporation is high, such as the Great Salt Lake in Utah. -
Salt Crystallization in Porous Construction Materials I Estimation of Crystallization Pressure
View metadata, citation and similar papers at core.ac.uk brought to you by CORE provided by EPrints Complutense Salt crystallization in porous construction materials I Estimation of crystallization pressure A. La Iglesiaa,*, V. Gonzalezb, V. L6pez-Acevedoc, C. Viedmac , Inslituto de Geologia Economica del CSIC, Facultad de Ciencias Ge% gicas, UCM, E·280411 Madrid. Spain b Deparlamento de Quimica, ETSI, Agronomos, UPM, E·28IJ40 Madrid, Spain , Deparlamenlo de Cristalografia y Mineralogia, Facultad de Ciencias Ge% gicas, UCM. E·28040 Madrid, Spain Abstract The crystallization process of soluble salts inside the natural and artificial porous materials partially immersed in different saline solutions has been studied, This procedure is used to simulate the conditions of exposure to salt weathering in which foundations and lower walls of building structures are within the zone of capillary rise of saline ground water. Crystallization pressures that can develop in the samples, which are a function of the pore size and salt-solution interfacial tension, have been calculated and are compared with experimental values of the materials tensile strength. since both these parameters allow the prediction of porous materials behaviour against salt weathering. Keywords: Salt weathering; Porous media; Salt crystallization; Crystallization pressure 1. Introduction The problem of crystallization pressure of salt was first studied by Correns [6J, who presented The crystallization process of soluble salts in a workable equation based on the Riecke principle porous materials can generate pressures inside the from which the pressure generated P versus salt pores sufficient to exceed the elastic limit of the supersaturation may be calculated: material, causing its breakage. -
Mineralogy of the Martian Surface
EA42CH14-Ehlmann ARI 30 April 2014 7:21 Mineralogy of the Martian Surface Bethany L. Ehlmann1,2 and Christopher S. Edwards1 1Division of Geological & Planetary Sciences, California Institute of Technology, Pasadena, California 91125; email: [email protected], [email protected] 2Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California 91109 Annu. Rev. Earth Planet. Sci. 2014. 42:291–315 Keywords First published online as a Review in Advance on Mars, composition, mineralogy, infrared spectroscopy, igneous processes, February 21, 2014 aqueous alteration The Annual Review of Earth and Planetary Sciences is online at earth.annualreviews.org Abstract This article’s doi: The past fifteen years of orbital infrared spectroscopy and in situ exploration 10.1146/annurev-earth-060313-055024 have led to a new understanding of the composition and history of Mars. Copyright c 2014 by Annual Reviews. Globally, Mars has a basaltic upper crust with regionally variable quanti- by California Institute of Technology on 06/09/14. For personal use only. All rights reserved ties of plagioclase, pyroxene, and olivine associated with distinctive terrains. Enrichments in olivine (>20%) are found around the largest basins and Annu. Rev. Earth Planet. Sci. 2014.42:291-315. Downloaded from www.annualreviews.org within late Noachian–early Hesperian lavas. Alkali volcanics are also locally present, pointing to regional differences in igneous processes. Many ma- terials from ancient Mars bear the mineralogic fingerprints of interaction with water. Clay minerals, found in exposures of Noachian crust across the globe, preserve widespread evidence for early weathering, hydrothermal, and diagenetic aqueous environments. Noachian and Hesperian sediments include paleolake deposits with clays, carbonates, sulfates, and chlorides that are more localized in extent. -
S40645-019-0306-X.Pdf
Isaji et al. Progress in Earth and Planetary Science (2019) 6:60 Progress in Earth and https://doi.org/10.1186/s40645-019-0306-x Planetary Science RESEARCH ARTICLE Open Access Biomarker records and mineral compositions of the Messinian halite and K–Mg salts from Sicily Yuta Isaji1* , Toshihiro Yoshimura1, Junichiro Kuroda2, Yusuke Tamenori3, Francisco J. Jiménez-Espejo1,4, Stefano Lugli5, Vinicio Manzi6, Marco Roveri6, Hodaka Kawahata2 and Naohiko Ohkouchi1 Abstract The evaporites of the Realmonte salt mine (Sicily, Italy) are important archives recording the most extreme conditions of the Messinian Salinity Crisis (MSC). However, geochemical approach on these evaporitic sequences is scarce and little is known on the response of the biological community to drastically elevating salinity. In the present work, we investigated the depositional environments and the biological community of the shale–anhydrite–halite triplets and the K–Mg salt layer deposited during the peak of the MSC. Both hopanes and steranes are detected in the shale–anhydrite–halite triplets, suggesting the presence of eukaryotes and bacteria throughout their deposition. The K–Mg salt layer is composed of primary halites, diagenetic leonite, and primary and/or secondary kainite, which are interpreted to have precipitated from density-stratified water column with the halite-precipitating brine at the surface and the brine- precipitating K–Mg salts at the bottom. The presence of hopanes and a trace amount of steranes implicates that eukaryotes and bacteria were able to survive in the surface halite-precipitating brine even during the most extreme condition of the MSC. Keywords: Messinian Salinity Crisis, Evaporites, Kainite, μ-XRF, Biomarker Introduction hypersaline condition between 5.60 and 5.55 Ma (Manzi The Messinian Salinity Crisis (MSC) is one of the most et al. -
1469 Vol 43#5 Art 03.Indd
1469 The Canadian Mineralogist Vol. 43, pp. 1469-1487 (2005) BORATE MINERALS OF THE PENOBSQUIS AND MILLSTREAM DEPOSITS, SOUTHERN NEW BRUNSWICK, CANADA JOEL D. GRICE§, ROBERT A. GAULT AND JERRY VAN VELTHUIZEN† Research Division, Canadian Museum of Nature, P.O. Box 3443, Station D, Ottawa, Ontario K1P 6P4, Canada ABSTRACT The borate minerals found in two potash deposits, at Penobsquis and Millstream, Kings County, New Brunswick, are described in detail. These deposits are located in the Moncton Subbasin, which forms the eastern portion of the extensive Maritimes Basin. These marine evaporites consist of an early carbonate unit, followed by a sulfate, and fi nally, a salt unit. The borate assemblages occur in specifi c beds of halite and sylvite that were the last units to form in the evaporite sequence. Species identifi ed from drill-core sections include: boracite, brianroulstonite, chambersite, colemanite, congolite, danburite, hilgardite, howlite, hydroboracite, kurgantaite, penobsquisite, pringleite, ruitenbergite, strontioginorite, szaibélyite, trembathite, veatchite, volkovskite and walkerite. In addition, 41 non-borate species have been identifi ed, including magnesite, monohydrocalcite, sellaite, kieserite and fl uorite. The borate assemblages in the two deposits differ, and in each deposit, they vary stratigraphically. At Millstream, boracite is the most common borate in the sylvite + carnallite beds, with hilgardite in the lower halite strata. At Penobsquis, there is an upper unit of hilgardite + volkovskite + trembathite in halite and a lower unit of hydroboracite + volkov- skite + trembathite–congolite in halite–sylvite. At both deposits, values of the ratio of B isotopes [␦11B] range from 21.5 to 37.8‰ [21 analyses] and are consistent with a seawater source, without any need for a more exotic interpretation. -
Nabokoite Cu7(Te4+O4)
4+ Nabokoite Cu7(Te O4)(SO4)5 • KCl c 2001-2005 Mineral Data Publishing, version 1 Crystal Data: Tetragonal. Point Group: 4/m 2/m 2/m. Crystals are thin tabular on {001}, to 1 mm, showing {001}, {110}, {102}, {014}, in banded intergrowth with atlasovite. Physical Properties: Cleavage: Perfect on {001}. Hardness = 2–2.5 D(meas.) = 4.18(5) D(calc.) = 3.974 Optical Properties: Transparent. Color: Pale yellow-brown, yellow-brown. Streak: Yellow- brown. Luster: Vitreous. Optical Class: Uniaxial (–). ω = 1.778(3) = 1.773(3) Cell Data: Space Group: P 4/ncc. a = 9.833(1) c = 20.591(2) Z = 4 X-ray Powder Pattern: Tolbachik volcano, Russia. 10.35 (10), 2.439 (7), 3.421 (6), 2.881 (5), 4.57 (4), 3.56 (4), 1.972 (4) Chemistry: (1) (2) SO3 33.66 33.60 TeO2 13.78 13.40 V2O3 0.07 Bi2O3 0.49 Fe2O3 0.09 CuO 45.25 46.74 ZnO 1.26 PbO 0.28 K2O 3.94 3.95 Cs2O 0.11 Cl 2.92 2.98 −O=Cl2 0.66 0.67 Total 101.19 100.00 (1) Tolbachik volcano, Russia; by electron microprobe, corresponds to (Cu6.74Zn0.18)Σ=6.92 (Te1.02Bi0.02Pb0.01Fe0.01V0.01)Σ=1.07O4.10(SO4)4.98Cl0.98. (2) KCu7(TeO4)(SO4)5Cl. Polymorphism & Series: Forms a series with atlasovite. Occurrence: A rare sublimate formed in a volcanic fumarole. Association: Atlasovite, chalcocyanite, dolerophanite, chloroxiphite, euchlorine, piypite, atacamite, alarsite, fedotovite, lammerite, klyuchevskite, anglesite, langbeinite, hematite, tenorite. Distribution: From the Tolbachik fissure volcano, Kamchatka Peninsula, Russia. -
Evolution of the Astonishing Naica Giant Crystals in Chihuahua, Mexico
minerals Review Evolution of the Astonishing Naica Giant Crystals in Chihuahua, Mexico Iván Jalil Antón Carreño-Márquez 1 , Isaí Castillo-Sandoval 2, Bernardo Enrique Pérez-Cázares 3, Luis Edmundo Fuentes-Cobas 2 , Hilda Esperanza Esparza-Ponce 2 , Esperanza Menéndez-Méndez 4, María Elena Fuentes-Montero 3 and María Elena Montero-Cabrera 2,* 1 Department of Engineering, Universidad La Salle Chihuahua, Chihuahua 31625, Mexico; [email protected] 2 Department of Environment and Energy, Centro de Investigación en Materiales Avanzados, Chihuahua 31136, Mexico; [email protected] (I.C.-S.); [email protected] (L.E.F.-C.); [email protected] (H.E.E.-P.) 3 Department of Computational Chemistry, Universidad Autónoma de Chihuahua, Chihuahua 31125, Mexico; [email protected] (B.E.P.-C.); [email protected] (M.E.F.-M.) 4 Department Physicochemical Assays, Instituto Eduardo Torroja de Ciencias de la Construcción, 28033 Madrid, Spain; [email protected] * Correspondence: [email protected] Abstract: Calcium sulfate (CaSO4) is one of the most common evaporites found in the earth’s crust. It can be found as four main variations: gypsum (CaSO4·2H2O), bassanite (CaSO4·0.5H2O), soluble Citation: Carreño-Márquez, I.J.A.; anhydrite, and insoluble anhydrite (CaSO4), being the key difference the hydration state of the Castillo-Sandoval, I.; Pérez-Cázares, sulfate mineral. Naica giant crystals’ growth starts from a supersaturated solution in a delicate B.E.; Fuentes-Cobas, L.E.; Esparza- thermodynamic balance close to equilibrium, where gypsum can form nanocrystals able to grow Ponce, H.E.; Menéndez-Méndez, E.; up to 11–12 m long. -
Cement Render and Mortar and Their Damages Due to Salt Crystallization in the Holy Trinity Church, Dominicans Monastery in Cracow, Poland
minerals Article Cement Render and Mortar and Their Damages Due to Salt Crystallization in the Holy Trinity Church, Dominicans Monastery in Cracow, Poland Mariola Marszałek * , Krzysztof Dudek and Adam Gaweł Department of Mineralogy, Petrography and Geochemistry, AGH University of Science and Technology, al. Mickiewicza 30, 30-059 Kraków, Poland; [email protected] (K.D.); [email protected] (A.G.) * Correspondence: [email protected] Received: 22 June 2020; Accepted: 17 July 2020; Published: 20 July 2020 Abstract: The investigations focused on the façade of the 17th-century Myszkowskis chapel at the 13th-century Church of the Holy Trinity in Cracow, Poland. Most of the chapel’s façade is made of rusticated limestone blocks, but its lower part is covered with cement render, and the basement consists of irregular pieces of limestone and sandstone, bound and partly replaced with cement mortar. The façade exhibited clearly visible damages: gray soiling of the surface, cracks, scaling, and efflorescence. The study presents characteristics of the cement render and mortar used for stone repair and/or substitution, as well as efflorescence from the lower part of the Myszkowskis chapel façade. The materials were analyzed with optical microscopy, scanning electron microscopy (SEM-EDS), Raman microspectroscopy, X-ray diffractometry (XRPD), and mercury intrusion porosimetry. The analyses demonstrated that the render covering some of the decayed limestone blocks was prepared using Portland cement (residual clinker grains represent alite and belite) as a binding agent, mixed with crushed stone as an aggregate. The cement mortar consisted of rounded quartz grains, rock fragments, and feldspars in very fine-grained masses of calcite and gypsum, also containing relics of cement clinker (alite, belite, ferrite, and aluminate). -
Crystal Structure and Magnetic Properties of the New Zn1. 5Co1
Crystal Structure and Magnetic Properties of the New Zn1.5Co1.5B7O13Br Boracite Roberto Escudero∗ and Francisco Morales Instituto de Investigaciones en Materiales, Universidad Nacional Aut´onoma de M´exico. A. Postal 70-360. M´exico, D.F., 04510 MEXICO.´ Marco A Leyva Ramirez Departamento de Qu´ımica, Centro de Investigaci´on y Estudios Avanzados del IPN. 07360, M´exico, D. F. Jorge Campa-Molina and S. Ulloa-Godinez C. Universitario de Ciencias Exactas e Ingenieras, Universidad de Guadalajara, Laboratorio de Materiales Avanzados Departamento de Electronica. 044840, Guadalajara, Jalisco. MEXICO.´ (Dated: August 29, 2021) arXiv:1106.5446v1 [cond-mat.mtrl-sci] 27 Jun 2011 1 Abstract New Zn1.5Co1.5B7O13Br boracite crystals were grown by chemical transport reactions in quartz ampoules, at a temperature of 1173 K. The crystal structure was characterized by X-ray diffraction. The crystals present an orthorhombic structure with space group Pca21, (No. 29). The determined cell parameters were: a = 8.5705(3)A,˚ b = 8.5629(3) A,˚ and c = 12.1198(4)A,˚ and cell volume, V = 889.45(5) A˚3 with Z = 4. Magnetic properties in single crystals of the new boracite, were determined. The Susceptibility-Temperature (χ−T ) behavior at different magnetic intensities was studied. The inverse of the magnetic susceptibility χ−1(T ) shows a Curie-Weiss characteristic with spin s = 3/2 and a small orbital contribution, l. At low temperatures, below 10 K, χ(T ) shows irreversibility that is strongly dependent on the applied magnetic field. This boracite is ferrimag- netic up to a maximum temperature of about 16 K, as shows the coercive field.