System/ Cleavage. Native Elements. Sulfides and Sulfosalts
|
|
- James Barnett
- 6 years ago
- Views:
Transcription
1 Element Formula System/ Cleavage Streak Miscellaneous Native Elements Copper Cu Isometric/ irregular masses Brownish High SG, metal sound Sulfur S Orthorhombic/ Rotten egg smell, bright Light yellow massive yellow color Graphite C Tabular Crystals/ Greasy look and feel, Gray 0001 metallic luster Sulfides and Sulfosalts Chalcocite Cu 2 S Massive Leaves black film on hands Bornite Cu 5 FeS 4 Massive/ rarely Tetragonal Brownish Gray Buish and purpleish. Greasy color Galena PbS Isometric 001 Gray High SG Sphalerite ZnS Isometric/ small Perfect cleavage and dodecahedrons Brown hardness, low SG Chalcopyrite CuFeS 2 Massive Greenish Gray Metallic luster Golden Pyrrhotite Fe 1x S Massive Magnetic Covellite CuS Basal 0001 Cinnabar HgS Massive/ rhombohedral Realgar AsS 001 good Dark Gray Scarlet Bright Orange Orpiment As 2 S Golden Stibnite Sb 2 S 3 Slender / Striations Pyrite FeS 2 Massive/ Choncoidal fracture Olivine Green Greenish Marcasite FeS 2 Radiating forms Gray Arsenopyrite FeAsS Granular/ Poor 101 Indigo blue color, iridescent, metallic luster Bright red color, high SG Mixture of colors Yellow, red, gray Golden color, excellent cleavage Similar to Galena but different cleavage and SG Gold color, harder than 6, duller than Chalcopyrite Spearhead appearance, pale yellow color and metallic Silver white color, high hardness, 5.56
2 Molybdenite MoS 2 Massive/ Perfect 0001 Enargite Cu 3 AsS 4 Perfect 110 Silver Gray Very soft 11.5, occurs with quartz Gray Iron Metallic luster, similar to pyrite Oxides and Hydroxides Spinel Group (AB 2 O 4 ) Magnetite Fe 3 O 4 Isometric/ massive Magnetic Chromite FeCr 2 O 4 Massive Iron black, no Dark Brown magnetism Very hard 8, Spinel MgAl 2 O 4 Isometric/ massive nonmagnetic, white streak Franklinite (Zn,Fe,Mn) (FeMn) 2 O 4 Massive/ granular Hematite Group (A 2 O 3 ) Red and Corundum Al 2 O 3 Hexagonal barrels Hematite Fe 2 O 3 Massive/ radiating structure Ilmenite FeTiO 3 Massive/ granular Rutile Group (AO 2 ) Rutile TiO 2 Tretragonal/ prismatic Pyrolusite MnO 2 Fibrous/ granular/ massive Cassiterite SnO 2 Massive/ fibrous Other Red Brown Brownish Red Pale Brown Iron Brown Cuprite Cu 2 O Isometric Brown Zincite ZnO Granular Red and Associated with Zincite, mixture of red and black and white Known for hardness 9, has Mica imbedded in it Red streak, earthy metallic luster Contains small flat silvery surfaces Located as dots in a predominatly white, Adamantine luster Soils fingers, very black streak High SG, adamantine luster, light streak Red color, high luster, associated with limonite Red color, associated with Franklinite
3 Hydroxides Brucite Mg(OH) 2 Massive Goethite FeO(OH) Orthorhombic/ 010 Bauxite A Mixture of 3 Minerals Yellow Brown Yellow Brown/ Orange Pearly white, harder than Talc but not elastic like Mica Radiating fibrous aggregation, bubbly Very light and porous, and a mixture of different colors Gibbsite Al(OH) 3 Boehmite AlO(OH) Diaspore HAlO 2 Halides Halite NaCl Isometric Tastes like salt Sylvite KCl Isometric Bitter taste Cubical forms due to Cryolite Na 3 AlF 6 parting Looks like watery snow Fluorite CaF 2 Isometric Perfect cleavage, fine colors Carbonates Distinctive Colors Rhodochrosite MnCO 3 rhombohedral Pink Red HCl, hardness 4, red Massive/ Not soluble in cold color Siderite FeCO 3 Rhombohedral Light Brown Well crystallized face, not soluble in HCl Malachite Cu 2 CO 3 (OH) 2 Radiating fibers/ stalactic masses Light Green HCl reaction, earthy, green, botryoidal forms Radiating spherical Azurite Cu 3 (CO 3 ) 2 (OH) 2 Dark Blue groups Hexagonal with rhombohedral cleavage Calcite CaCO 3 Rhombohedral Colorless HCl reactions, intense blue color Low SG, Hardness 2.5 3, HCl reaction Dolomite CaMg(CO 3 ) 2 Rhombohedral Clear Curved/ saddle shaped, powdered HCl reaction Magnesite MgCO 3 Granular masses Resembles chert but lower hardness, no HCl reaction
4 Smithsonite ZnCO 3 Granular High SG, stalactic habit, no HCl reaction Orthorhombic with no rhombohedral cleavage Cerussite PbCO 3 Fibrous crystal aggregates Light Brown Very high SG, no HCl reaction Aragonite CaCO 3 Columnar Orthorhombic/ Witherite BaCO 3 striations Fibrous with Strontianite SrCO 3 striations Sulfates Barite BaSO 4 Orthorhombic Celestite SrSO 4 Basal perfect, prismatic Anglesite PbSO 4 Orthorhombic Light Harder than Calcite, high SG, powdery appearance, HCl reaction High SG, HCl reaction High SG, powders easily, HCl reaction High SG, Brown stuff with pearly luster Light blue color, resembles Barite but low SG High SG, associated with Galena Anhydrite CaSO 4 Massive, orthorhombic Light Looks like Gypsum but harder, vitreous luster Gypsum CaSO 4. 2H2 0 Massive, monclinic Borates Kernite Na 2 B 4 O 7. 4H2 O Monoclinic Light Apatite Ca 5 (F,Cl,OH) (PO 4 ) 3 Hexagonal Light Monzanite (Ce,La,Y,Th)PO 4 Monoclinic Brown Amblygonite LiAlFPO 4 Massive, triclinic Wavellite Al 3 (PO 4 ) 2 (OH) 3. 5H2 O Radiating aggregates Very soft 2, can be scratched by a fingernail Turns chalky white, low SG Green, long prismatic Granular, occurs in sand, resinous luster Hard 6, might look like Feldspar Globular/ radiating forms
5 Tungstates Wolframite (Fe,Mn)WO 4 Monoclinic Brown Scheelite CaWO 4 Tetragonal Light Tektosilicates Quartz SiO 2 Conchoidal fracture Cristobalite SiO 2 Small octahedrons in lava Bladed/ tabular, high SG Very high SG, vitreous luster Hexagonal, hardness 7 Occurs with obsidian Opal SiO 2. nh2 O Amorphous Feldspars Milky appearance, flesh colored, play of colors Orthoclase/ Microcline KAlSi 3 O 8 Monoclinic, perfect 001 Looks like plagioclase but no striations Plagioclase Perfect 110 Albite NaAlSi 3 O 8 Anorthite CaAl 2 Si 2 O 8 to black Feldspathoids Leucite KAlSi 2 O 6 Phenocrysts/ isometric Striations, colors ranges from: Crystal forming, does not occur with quartz, is white to gray color Nepheline NaAlSiO 4 Hexagonal dots with Cancrinite, no striations Cancrinite Na 6 Ca(CO 3 ) (AlSiO 4 ) 6. 2H2 O Hexagonal Yellow, occurs with Nepheline Sodalite Na 8 (AlSiO 4 ) 6 Cl 2 Massive/ isometric Very blue color, little crystal faces, associated with Nepheline
6 Zeolites Analcime NaAlSi 2 O 6. H2 O Massive/ isometric Forms, but located in the matrix unlike Leucite Stilbite CaAl 2 SiO 18. 7H2 O Tabular / sheaflike aggregates Occurs in cavities Phyllosilicates Serpentine Group Massive/ fine Antigorite Mg 6 Si 4 O 10 (OH) 8 grained Hexagonal/ Chrysotile Mg 6 Si 4 O 10 (OH) 8 monoclinic Clay Mineral Group Greenish Kaolinite Al 4 Si 4 O 10 (OH) 8 Massive/ triclinic Montmorillonite Al 4 Si 8 O 20 (OH) 4. nh 2 O Massive Talc Mg 3 Si 4 O 10 (OH) 2 Massive/ triclinic Greasy luster Fibrous, silky luster Earthy luster, feels soapy, writes on cloth Earthy luster, expands with water Marks cloth, pearly, hardness 1 Pyrophyllite Al 2 Si 4 O 10 (OH) 2 Radiating aggregates Marks easily Muscovite Lepidolite Phlogopite KAl 2 (AlSi 3 O 10 ) (OH) 2 Mica Group Monoclinic Clear KLiAl(AlSi 3 O 10 ) (OH) 2 Massive/ monoclinic KMg 3 (AlSi 3 O 10 ) (OH) 2 Monoclinic Elastic sheets, clear Pastel colors, lilac, yellow and pink Elastic sheets, yellowish brown Biotite Vermiculite Chlorite Prehnite K(Mg,Fe) 3 (AlSi 3 O 10 )(OH) 2 Monoclinic Elastic sheets, black Mg 3 Si 4 O 10 (OH) 2. nh2 O Monoclinic Chlorite Group Mg 6 Si 8 O 20 (OH) 4 Mg 6 (OH) 12 Triclinic Ca 2 Al(AlSi 3 O 10 )(OH Crystalline ) 2 aggregates Elastic sheets, altered Biotite, expands upon heating, dark colors Greenblack colors, micaceous habit and cleavage Light Green Green color
7 Inosilicates Pyroxenes Diopside CaMgSi 2 O 6 Granular/ monoclinic Augite XYSi 2 O 6 Monoclinic Green Enstatite MgSiO 3 Massive Spodumene LiAlSi 2 O 6 Prismatic 8 sided, looks like olivine, white to green color, 2 directions cleavage 90 o cleavage unlike Hornblende, short Bronze like luster, dark green to dark brown Vitreous luster, vertical prismatic cleavage Pyroxenoids Wollastonite CaSiO 3 Massive/ fibrous Rhodenite MnSiO 3 Massive/ triclinic Pink Anthophyllite Tremolite Actinolite Amphiboles (Mg,Fe) 7 Si 8 O 22 (OH) 2 Fibrous Ca 2 Mg 5 Si 8 O 22 (OH) Prismatic / bladed Ca 2 (Mg,Fe) 5 Si 8 O 22 (O Columnar aggregates H) 2 Dark Light Green Hornblende XYSi 8 O 22 (OH) 2 Prismatic Greenish Neosilicates Granular/ conchoidal Olivine Series (Mg,Fe) 2 SiO 4 fracture Garnet Series A 3 B 2 (SiO 4 ) 3 MgFe MnCaAlSi 3 O 12 Dodecahedrons/ isometric Brownish Pearly, associated with Garnets, silky, elongated Pink color, high hardness 5.56, vitreous luster Like asbestos, clove brown color green purple, slender prisms Looks like Tremolite, dark green color Non90 o cleavage, silky appearance, looks like Augite Granular nature, green color Reddish/ brownish color, dodecahedron shape, hardness
8 Zircon ZrSiO 4 Crystals/ tetragonal Kyanite Al 2 SiO 5 Crystals/ triclinic Andalusite Al 2 SiO 5 Course square prisms Silliminite Al 2 SiO 5 Fibrous masses Topaz Al 2 SiO 4 (F,OH) 2 Vertical striated faces Staurolite Sphene CaTiO(SiO 4 ) Epidote Idocrase (Vesuvianite) Fe 2 Al 9 O 6 (SiO 4 ) 4 (O,OH) 2 Cruciform twins Ca 2 (Al,Fe)Al 2 O (SiO 4 )(Si 2 O 7 )OH Wedge shaped Sorosilicates Monoclinic CaMgAlSiO Tetragonal Cyclosilicates Shades of brown, translucent, adamantine luster, high SG Bladed, blue color Prisms, hardness 7.5, red colors Long needle like, pale colors High hardness 8, yellowish colors clear, high SG Brownish color, Brownish colors, occurs with a Quartzlike mineral Pistachio green, high hardness 67, basal cleavage Brown tetragonal, lower SG than Garnet Beryl Be 3 Al 2 Si 6 O 18 Vertically striated Light blue green color, greater hardness than Apatite 7.58 Cordierite (Mg,Fe) 2 Al 3 (AlSi 5 O 18 ) Orthorhombic Various shades of bluegray, resembles quartz Tourmaline NaFeMgLi Al(BO 3 )Si 6 O 18 (OH) Conchoidal fracture Spherical triangle cross section, black, striations
GEL Mineralogy - Optical Mineralogy
Disclaimer: These reviews are courtesy of the instructor. While care has been taken to include everything that might be tested, omissions or oversights may have occurred. The instructor shall NOT be liable
More informationLAB 1: MINERAL IDENTIFICATION INDEX
12.001 LAB 1: MINERAL IDENTIFICATION INDEX Minerals with a Metallic Luster Cleavage Streak Properties Comments and Uses Name and Harder than Glass Greenish Black Brass-yellow; H = 6.0 6.5; S.G. = 5.0;
More informationLAB 1: MINERAL IDENTIFICATION INDEX
Softer than Glass Hardness Similar to Glass Harder than Glass 12.001 LAB 1: MINERAL IDENTIFICATION INDEX Minerals with a Metallic Luster Cleavage Streak Properties Comments and Uses Name and Greenish Black
More informationIntroduction to Geology Spring 2008
MIT OpenCourseWare http://ocw.mit.edu 12.001 Introduction to Geology Spring 2008 For information about citing these materials or our Terms of Use, visit: http://ocw.mit.edu/terms. 12.001 LAB 1: MINERAL
More informationPROPERTIES OF MINERALS IN HAND-SAMPLE
EESC 2100: Mineralogy PROPERTIES OF MINERALS IN HAND-SAMPLE During the first two weeks of class, complete this lab assignment concurrently with Labs 1 and 2. Use the sample standards to become familiar
More informationPhysical Properties of Minerals
1 of 8 9/20/2002 9:30 AM Prof. Stephen A. Nelson Geology 211 Tulane University Mineralogy Physical Properties of Minerals This document last updated on 20-Sep-2002 Although we have discussed x-ray identification
More informationGEOLOGY 284: MINERALOGY
Dr. Helen Lang Dept. of Geology & Geography West Virginia University FALL 2015 GEOLOGY 284: MINERALOGY Mineral Properties in Hand Specimen Luster Metallic Sub-metallic Non-metallic Vitreous Adamantine
More informationUnit 2 6 th Grade PHYSICAL PROPERTIES OF MATTER
Unit 2 6 th Grade PHYSICAL PROPERTIES OF MATTER Elements can be classified as: Metals Good conductors of heat. Good conductors of electricity. Good reflectors of light when polished (shiny luster) Malleable
More informationCopy the ques,on below and write down an answer. Make a list of characteristics you can use to describe the minerals in these pictures.
Copy the ques,on below and write down an answer Make a list of characteristics you can use to describe the minerals in these pictures. Do Now Minerals and Rocks Defini,on of a Mineral A mineral is a naturally
More informationMinerals Basic Building Blocks Elements Compounds Definition of Minerals naturally occurring inorganic solid chemical formula regular structure
Minerals Rocks are made of minerals. Minerals are made of chemical compounds. Compounds are made of elements. Basic Building Blocks The smallest piece of a chemical compound that still has the properties
More informationGEOLOGY 284: MINERALOGY
Dr. Helen Lang Dept. of Geology & Geography West Virginia University FALL 2014 GEOLOGY 284: MINERALOGY Ore Deposits and Economic Minerals An ore is anything that can be mined from the Earth at a profit,
More informationMinerals to know. Mineral Families. Calcite Fluorite Galena Kaolinite Halite Copper Talc Graphite Bornite Pyrite. Quartz. Mica. Gypsum.
Minerals Minerals to know Calcite Fluorite Galena Kaolinite Halite Copper Talc Graphite Bornite Pyrite Mineral Families Mica Biotite Muscovite Lepidolite Gypsum Satin Spar Selenite Feldspar Pink Others
More informationGeology Physical Geology. Box of Minerals
Geology 1403- Physical Geology Box of Minerals Minerals 1-Talc Talc O Luster: pearly/silky O Hardness: 1 O Streak: white/gray O Fracture O Color: sea green, white, gray O Uses: Talcum power, paint, ceramics,
More informationWhy Study Minerals? blocks of Earth materials. to understanding rock formation
Minerals I Elements of the Earth s crust Properties of minerals Crystal form; Cleavage/Fracture; Color, streak, luster; Hardness, tenacity; Specific gravity; Acid test, magnetism, etc. Why Study Minerals?
More informationES 104: # 6 PHYSICAL PROPERTIES OF MINERALS AND MINERAL IDENTIFICATION
ES 104: Laboratory # 6 PHYSICAL PROPERTIES OF MINERALS AND MINERAL IDENTIFICATION Introduction Minerals are naturally occurring, usually inorganic, solids that possess a definite chemical composition and
More informationEXAM RETURN EXAM RETURN EXAM RETURN. Why study minerals and rocks?
Exam return 15 minutes before break. RESULTS: A: B: C: D: F: % of class got As and Bs CONGRATS! % got a D or lower If your grade is what you want, keep up the good work! If not, see me for advice. EXAM
More informationCOPY. Topic 6 MINERALS. Mr. Rocco
COPY Topic 6 MINERALS Mr. Rocco Mineral? COPY Naturally occurring in the earth Solid Definite chemical composition Atoms arranged in a specific pattern Inorganic not from once living organisms (See ESRT
More informationWELCOME TO THE GLENDALE COMMUNITY COLLEGE MINERAL IDENTIFICATION PROGRAM
presented by: WELCOME TO THE GLENDALE COMMUNITY COLLEGE MINERAL IDENTIFICATION PROGRAM Susan Celestian - Curator of the Arizona Mining and Mineral Museum Stan Celestian - Photographer copyright 2002 Where
More informationThe Study of Minerals (Chapter 1) - Introduction to Mineral Physical Properties and Mineral Identification
GEOLOGY 306 Laboratory NAME: Instructor: TERRY J. BOROUGHS Lab Section: The Study of Minerals (Chapter 1) - Introduction to Mineral Physical Properties and Mineral Identification For this assignment you
More informationA few silicate minerals
A few silicate minerals Stony materials and conservation of the built heritage Natural Stone _Mineralogy_ BR /18 Nesosilicates / Garnets (X 3 2+ Y 2 3+ [SiO 4 ] 3 ) Use: gemstone, abrasive Stony materials
More informationpage - Labs 09 & 10 - Mineral Identification
Labs 09 & 10 - Mineral Identification page - All rocks are composed of one or more minerals. In order to be able to identify rocks you have to know how to recognize those key minerals that make of the
More informationpage - 1 Lab 9 - Mineral Identification
Lab 9 - Mineral Identification page - 1 All rocks are composed of one or more minerals. In order to be able to identify rocks you have to know how to recognize those key minerals that make of the bulk
More informationA mineral is a naturally occurring, inorganic solid that has a crystal structure and a definite chemical composition.
Minerals Objectives List the 5 traits of minerals Identify minerals Describe characteristics of minerals Know how minerals form Describe ways that we use minerals A mineral is a naturally occurring, inorganic
More information2 Identifying Minerals
CHAPTER 1 2 Identifying Minerals SECTION Minerals of the Earth s Crust BEFORE YOU READ After you read this section, you should be able to answer these questions: What seven properties can be used to identify
More information9/13/2009. Minerals Chapter 5 (pg. 120) Democritus BCE. electron shells Shells have 2, 8, or 18 electrons. The periodic table
Minerals Chapter 5 (pg. 120) Atoms: smallest indivisible particles of matter Democritus 460-370 BCE Atomic Number Protons (+) Neutrons (0) Electrons (-) electron shells Shells have 2, 8, or 18 electrons
More informationA mineral is a naturally occurring, inorganic solid that has a crystal structure and a definite chemical composition.
A mineral is a naturally occurring, inorganic solid that has a crystal structure and a definite chemical composition. Naturally Occurring Formed by processes that occur in the natural world Inorganic Not
More informationOverview of minerals 2.2 PHYSICAL PROPERTIES
Chapter 2: Minerals Adapted by Lyndsay R. Hauber, Michael B. Cuggy, & Joyce M. McBeth (2018) University of Saskatchewan from Deline B, Harris R & Tefend K. (2015) "Laboratory Manual for Introductory Geology".
More informationThe Study of Minerals (Chapter 1)
GEOLOGY 306 Laboratory Instructor: TERRY J. BOROUGHS NAME: The Study of Minerals (Chapter 1) For this assignment you will require: a streak plate, glass plate, magnet, dilute hydrochloric (HCl) acid, microscope,
More informationThe Study of Minerals (Chapter 1)
GEOLOGY 306 Laboratory Instructor: TERRY J. BOROUGHS NAME: The Study of Minerals (Chapter 1) For this assignment you will require: a streak plate, glass plate, magnet, dilute hydrochloric (HCl) acid, microscope,
More informationIdentifying Minerals
Identifying Minerals Beryl, feldspar, quartz Rock-forming Minerals Rock-forming minerals Common minerals that make up most of the rocks of Earth s crust Only a few dozen members Composed mainly of the
More informationClassifying Minerals. Name: Date: Class: #: Materials: Magnifying lens (2) Copper Penny (2) Glass Plate Mohs Scale Set of minerals Mineral
Name: Date: Class: #: Classifying Minerals Materials: Magnifying lens (2) Copper Penny (2) Glass Plate Mohs Scale Set of minerals Mineral Magnet Iron Nail Streak Plates (1 white & 1 black) Identification
More informationPhysical Properties of Minerals Part II
GEOLOGY 333 LAB 2 PHYSICAL PROPERTIES OF MINERALS PART II Physical Properties of Minerals covered last week: 1. Hardness 2. Cleavage 3. Crystal Shape 4. Specific Gravity Physical Properties of Minerals
More informationMinerals page 1. Minerals
Minerals page 1 Minerals Introduction Most people are familiar with the commonly applied classification of all physical entities into the three categories of animal, vegetable and mineral. We now know
More informationPage - 1 Lab 1 - Physical Properties and the Identification of Nonsilicate Minerals
Page - 1 Lab 1 - Physical Properties and the Identification of Nonsilicate Minerals All rocks are composed of one or more minerals. In order to be able to identify rocks you have to be able to recognize
More informationPhysical Properties of Minerals
Physical Properties of Minerals Hardness This is an indirect measure of the bond strength in the mineral. It is exhibited in the form of resistance to abrasion on a relatively smooth, fresh surface. Friedrich
More informationElements and Compounds
Chemistry Name: Partners: Date: Elements and Compounds Introduction Most of the materials you have used so far in this course were mixtures. If you could take them apart physically, you would find that
More informationOxides and Hydroxides
Descriptive Mineralogy Oxides and Hydroxides Classification of the Minerals Non-Silicates Native Elements Halides Sulfides Oxides Hydroxides Carbonates Sulfates Phosphates Silicates Orthosilicates Sorosilicates
More information3.3 Minerals. Describe the characteristics that define minerals.
3.3 Minerals Describe the characteristics that define minerals. Are you a mineral? There used to be a TV commercial that said "you are what you eat." If that s true - and to some extent it is - then you
More informationGLY 4200C LAB 1. 1 Talc 6 Orthoclase 2 Gypsum 7 Quartz 3 Calcite 8 Topaz 4 Fluorite 9 Corundum 5 Apatite 10 Diamond
GLY 4200C LAB 1 PHYSICAL AND CHEMICAL PROPERTIES OF MINERALS IN HAND SPECIMEN There are a number of physical properties which are suitable for field use on hand specimens. One chemical test also falls
More informationModule 5: Minerals Topic 3 Content: Identification of a Mineral Presentation Notes. Identification of Minerals
Identification of Minerals 1 Minerals occur in different colors, sizes, and shapes. Minerals also differ in the way that they reflect light and in the way that they break. Some minerals are softer than
More informationOverview of geochemistry, acid generation, and metal solubility
Overview of geochemistry, acid generation, and metal solubility Spring Creek, 1974, ph =2.75 Acid/base Acid (mine/rock) drainage (ph < 1 to 6) One of largest water quality problems at hardrock mine sites
More informationStudent Exploration: Mineral Identification
Name: Date: Student Exploration: Identification Vocabulary: crystal, density, hardness, homogeneous, luster, mass, mineral, streak, volume Prior Knowledge Questions (Do these BEFORE using the Gizmo.) 1.
More informationMinerals. Mohs Scale of Hardness
Part I: Testing Mineral Properties You will perform the following tests on each mystery mineral as directed by your teacher. Be sure to record your observations in the appropriate row of the data table.
More informationThe Study of Minerals (Chapter 1) Introduction to Mineral Identification: THE NON - SILICATE MINERALS
GEOLOGY 306 Laboratory NAME: Instructor: TERRY J. BOROUGHS The Study of Minerals (Chapter 1) Introduction to Mineral Identification: THE NON - SILICATE MINERALS For this assignment you will require: a
More informationClassification and Nomenclature of Minerals. Unit 3
Classification and Nomenclature of Minerals Unit 3 Introduction to Berzelian Classification The Berzelian mineral classification system was named in honor of the Swedish chemist and mineralogist Jons Jakob
More informationEARTH SCIENCE 11 CHAPTER 4 NOTES HOW TO KNOW THE MINERALS. Introduction. Background
EARTH SCIENCE 11 CHAPTER 4 NOTES HOW TO KNOW THE MINERALS KEY Introduction Much of the Earth is covered with loose rock, soil, or sand. Beneath this loose material there is always unbroken solid rock which
More informationEARTH SCIENCE 11 CHAPTER 4 NOTES HOW TO KNOW THE MINERALS. Introduction. Background
EARTH SCIENCE 11 CHAPTER 4 NOTES HOW TO KNOW THE MINERALS KEY Introduction Much of the Earth is covered with loose rock, soil, or sand. Beneath this loose material there is always unbroken solid rock which
More information5. MINERALS LAST NAME (ALL IN CAPS): FIRST NAME:
LAST NAME (ALL IN CAPS): FIRST NAME: 5. MINERALS Instructions: When you test a mineral for effervescence and you apply HCl, you must first ask permission from your instructor (remember HCl is an acid and
More informationWhat is a Mineral? A Mineral is: Pure Naturally occurring Crystalline Solid
Mineral Properties What is a Mineral? A Mineral is: Pure Naturally occurring Crystalline Solid Mineral Properties Color Streak Luster Hardness Density Crystal Shape Cleavage Fracture Fluorescence Reaction
More informationBORATES. 59. Ulexite - NaCaB 5 O 6 (OH) 6 5H 2 O. Color - Crystal Habit - Crystal System - Cleavage - Hardness - Luster/Streak / Use (if any) - Other
BORATES Borate minerals are minerals that contain a borate anion group. Simple borate anion is BO 3 and has a -3 charge. This means each borate anion requires a +3 cation to generate a non-charged stable
More informationThere are about 3,000 known minerals, only about 30 are common. The most common are quartz,feldspar,mica, and calcite.
There are about 3,000 known minerals, only about 30 are common. The most common are quartz,feldspar,mica, and calcite. These minerals make up most of the rocks found in the Earth s crust. Most of the Earth
More informationName Class Date. Does it have a crystalline structure? Minerals are crystals. Each mineral has a certain crystal structure that is always the same.
CHAPTER 1 1 What Is a Mineral? SECTION Minerals of the Earth s Crust BEFORE YOU READ After you read this section, you should be able to answer these questions: What are minerals? What determines the shape
More informationB.Using the information from ESRT p. 16- how many minerals could this be?
NAME PARTNER(s) DATE PERIOD OBJECTIVE: (1) Identify minerals using physical characteristics (2) Make observations, (3) Become skilled at using mineral identification tools. MATERIALS NEEDED: mineral samples,
More informationMake Five. A game about the chemical formulas of some common minerals
Make Five A game about the chemical formulas of some common minerals By defi nition, a mineral has a defi nite chemical composition. It s sort of like a recipe. This game is for students who want to (or
More informationVOCABULARY: mineral, luster, streak, hardness, cleavage, fracture, organic, inorganic, composition
Name Science: TITLE: Mineral Identification Lab OBJECTIVE: Of some 3,000 known minerals, only about a dozen called common rockforming minerals make-up Earth s crust. They are identified in the field by
More informationMineral Notes. The crust is made of mixtures of naturally occurring compounds and elements called minerals.
Mineral Notes Mineral Notes Earth s crust is the solid outermost layer of Earth. It is thicker under the continents and thinner under the oceans. The crust is made of mixtures of naturally occurring compounds
More information2Matter and Minerals
2Matter and Minerals Adapted by Lyndsay R. Hauber, Michael B. Cuggy, & Joyce M. McBeth (2018) University of Saskatchewan from Deline B, Harris R & Tefend K. (2015) "Laboratory Manual for Introductory Geology".
More informationExternal Symmetry of Crystals, 32 Crystal Classes
Prof. Stephen A. Nelson Geology 211 Tulane University Mineralogy External Symmetry of Crystals, 32 Crystal Classes This page last updated on 03-Sep-2002 As stated in the last lecture, there are 32 possible
More informationNATURE Sunday Academy What Parts of Computers are Mined
2013-14 NATURE Sunday Academy What Parts of Computers are Mined Activity B: Ore Body Mystery In this activity students will explore the processes of core drilling and geological testing. Students will
More informationA SAMPLER OF SELECTED 2017 BMC AUCTION SPECIMENS (2017 Auction Date is Saturday, 21 January) Volume 2
A SAMPLER OF SELECTED 2017 BMC AUCTION SPECIMENS (2017 Auction Date is Saturday, 21 January) Volume 2 Apophyllite [KCa 4 (Si 4 O 10 ) 2 F 8(H 2 O)], Stilbite [NaCa 4 Al 8 Si 28 O 72 30(H 2 O)] & Scolecite
More informationENGINEERING GEOLOGY PROF. DEBASIS ROY DEPARTMENT OF CIVIL ENGINEERING. INDIAN INSTITUTE OF TECHNOLOGY, Kharagpur LECTURE - 5
ENGINEERING GEOLOGY PROF. DEBASIS ROY DEPARTMENT OF CIVIL ENGINEERING INDIAN INSTITUTE OF TECHNOLOGY, Kharagpur LECTURE - 5 Physical Properties of Minerals Hello everyone and welcome back to the class
More informationShape - from breaking
Shape descriptions Different ways to describe the appearance of a crystal or aggregation of crystals not necessarily related to symmetry (though some are a result of that). Table 3.2 in the text will see
More informationMinerals Reading with Questions (Pg. 3-7) Properties of Common Minerals Reading (Pg. 8-9 ) Crossword Puzzle (Pg. 17) Flashcard Matching
NAME: Kick Off Activity Classification of Minerals (Pg. 2) MUST DO ALL The Foundation Minerals Reading with Questions (Pg. 3-7) Properties of Common Minerals Reading (Pg. 8-9 ) OR Prop. of Common Minerals
More informationThe Chemical Composition of. Minerals. Article and photography by Ashley Atwater
The Chemical Composition of Minerals Article and photography by Ashley Atwater Introduction Minerals are often referred to as the building blocks of rocks. In order to be deemed a mineral, the subject
More informationMinerals. Natural Solid Inorganic Definite chemical composition Crystal structure due to internal arrangement of atoms
Minerals Natural Solid Inorganic Definite chemical composition Crystal structure due to internal arrangement of atoms http://www.minerals.net/gemstone/index.htm http://www.mii.org/www.mii.org General Facts
More information5. MINERAL PROPERTIES, IDENTIFICATION, & USES
LAST NAME (ALL IN CAPS): FIRST NAME: 5. MINERAL PROPERTIES, IDENTIFICATION, & USES Instructions: Refer to Laboratory 3 in your Lab Manual on pages 73-110 to answer the questions in this work sheet. Your
More information3 The Formation, Mining, and Use of Minerals
CHAPTER 1 3 The Formation, Mining, and Use of Minerals SECTION Minerals of the Earth s Crust BEFORE YOU READ After you read this section, you should be able to answer these questions: How do minerals form?
More informationCh. 2. Categories. Hand Sample ID. Crystal Shape. Crystal Habit. Interactions with light. Geo 271, Spring Elizabeth Goeke 1
Categories Hand Sample ID Spring 2011 Klein & Dutrow appearance xtal form habit interaction with light diaphaneity luster color streak luminescence mechanical properties hardness tenacity cleavage fracture
More informationGY 302: Crystallography & Mineralogy
UNIVERSITY OF SOUTH ALABAMA GY 302: Crystallography & Mineralogy Lecture 6: Polymorphism and Crystal Habit Instructor: Dr. Douglas Haywick Online Lecture Review 1. Polymorphs and Polymorphism 2. Pseudomorphs
More information3 The Formation, Mining, and Use of Minerals
CHAPTER 3 3 The Formation, Mining, and Use of Minerals SECTION Minerals of the Earth s Crust BEFORE YOU READ After you read this section, you should be able to answer these questions: How do minerals form?
More informationMINERAL IDENTIFICATION
Testing the Streak of a Mineral The streak of a mineral is its colour when it is crushed into a fine powder. It is usually observed with the aid of a streak plate, which is a piece of hard white unglazed
More informationENGINEERING GEOLOGY PROF: DEBASIS ROY DEPARTMENT OF CIVIL ENGINEERING. INDIAN INSTITUTE OF TECHNOLOGY, Kharagpur LECTURE - 6
ENGINEERING GEOLOGY PROF: DEBASIS ROY DEPARTMENT OF CIVIL ENGINEERING INDIAN INSTITUTE OF TECHNOLOGY, Kharagpur LECTURE - 6 Crystallography and Optical Properties of Minerals Hello every one and welcome
More informationSteven Dutch, Natural and Applied Sciences, University of Wisconsin - Green Bay
The CIPW Norm Steven Dutch, Natural and Applied Sciences, University of Wisconsin - Green Bay Simplified by JFM (feb. 06), by removing most of the accessory minerals, and the steps needed only in rare
More informationMagnet Filter model CS Electromagnetic Separator model CG
Magnet Filter model CS Electromagnetic Separator model CG Electromagnetism Material Nippon Magnetics, Inc. Electromagnetic Separator Model: CG Fine iron powder from raw material! Usage Model CG is designed
More informationLecture 5. Exchange Reactions. Cation exchange Salt/Sodium Affected Soils Acid Soils
Lecture 5 Exchange Reactions Cation exchange Salt/Sodium Affected Soils Acid Soils General Classes (layer build-up) of Phyllosilicate Minerals: Layer Type Charge Trioctahedral Dioctahedral 1 octahedra
More informationGEOL.3070 EARTH MATERIALS I FORENSIC APPLICATIONS OF X-RAY DIFFRACTION
GEOL.3070 EARTH MATERIALS I FORENSIC APPLICATIONS OF X-RAY DIFFRACTION NAME I. Introduction Our knowledge of the crystalline state is gained by studies utilizing x-rays (the field of x- ray crystallography).
More informationAl-Omam International School
Al-Omam International School Science Work sheet Grade-5 Unit-9 Lesson (1) Multiple Choice Identify the choice that best completes the statement or answers the question. 1. Study the table of mineral properties.
More informationCHAPTER 2: ATOMIC ARRANGEMENTS AND MINERALOGICAL STRUCTURES. Sarah Lambart
CHAPTER 2: ATOMIC ARRANGEMENTS AND MINERALOGICAL STRUCTURES Sarah Lambart RECAP CHAP. 1 Mineral: naturally occurring (always) a structure and a composition that give it defined macroscopic properties (always)
More informationMini Miners Monthly. Mineral Bingo. A fun & exciting way to learn about minerals, their properties and uses.
Mini Miners Monthly A fun & exciting way to learn about minerals, their properties and uses. Vol. 7 No. 9 September 2013 Mineral bingo Everybody loves BINGO! It s easy. It s fun. And it s a great way to
More informationMIST-2016 INTERNATIONAL SEMINAR ON START UP AND STAND UP INDIA FROM MINES TO STEEL. MECON, RANCHI 29 th,30 th & 31 st January,2016
MIST-2016 INTERNATIONAL SEMINAR ON START UP AND STAND UP INDIA FROM MINES TO STEEL MECON, RANCHI 29 th,30 th & 31 st January,2016 Technical Session-1 Managing Indian Iron Ore Fines - Beneficiating for
More informationMagnetic Susceptibility Index for the Primary Gemstones
Magnetic Susceptibility Index for the Primary Gemstones 2010 Kirk Feral Magnetic measurements are standardized to N-52 magnets. Colorless and extremely pale stones of any species tend to be Inert (Inert
More informationMINERAL PHASES IN VARIOUS FUEL ASHES USING DIFFERENT ASHING METHODS AND RELATED TEMPERATURES
Institute of Energy Process Engineering and Chemical Engineering Chair EVT MINERAL PHASES IN VARIOUS FUEL ASHES USING DIFFERENT ASHING METHODS AND RELATED TEMPERATURES M. Reinmöller, M. Schreiner, S. Guhl,
More informationChapter 20 CHEMISTRY. Metallurgy and the Chemistry of Metals. Dr. Ibrahim Suleiman
CHEMISTRY Chapter 20 Metallurgy and the Chemistry of Metals Dr. Ibrahim Suleiman GENERAL PROPERTIES AND STRUCTURE OF METALS opaque good conductors of heat and electricity high malleability and ductility
More informationFull file at
Chapter 2 Test Bank Completion 1. A/an is a naturally occurring inorganic solid with a characteristic chemical composition and a crystalline structure. 2. A positively charged ion is a. 3. A/an is a planar
More informationName October 3, K FIRST HOUR EXAM
1 Name October 3, 1994 347K FIRST HOUR EXAM Answer the following questions as directed. For multiple choice questions choose the single best answer. Multiple choice are worth 3 pts, T/F are worth 1 pt.
More informationOxidation and Reduction: Chemical Weathering and Smelting
Dissolution Chemical Weathering Oxidation and Reduction: Chemical Weathering and Smelting H 2 CO 3 + CaCO 3 Ca 2+ (aq) + 2HCO 3 - (aq) Dissolution of calcite in carbonic acid All rainwater is a weak carbonic
More informationEarth s Crust. Atoms build Molecules build Minerals build. Rocks build. Lecture 3 - Mineralogy.
Lecture 3 - Mineralogy http://www.soest.hawaii.edu/coasts/gg101/index.html Atoms build Molecules build Minerals build Rocks build Earth s Crust Common minerals that we mine and use. Mineral Name What It
More informationNOTES Minerals.notebook. May 03, ,000. Inorganic. Solid. chemical 3,000. Oxygen. Naturally. elements. Earth's. Crystalline. crust.
Minerals Mineral Characteristics 1. occurring 2. 3. 4. structure 5. Definite composition Naturally Mineral Characteristics 1. occurring Inorganic 2. Solid 3. Crystalline 4. structure chemical 5. Definite
More informationMineral of the Month Club
Mineral of the Month Club September 2016 Offering Sheet Our four special offers for September are from Nepal, Mexico, Madagascar, and the United States (Colorado). Their colors range from white and green
More informationMurder on the Beach: A Crime Scene Investigation
Murder on the Beach: A Crime Scene Investigation Just the Facts A victim of foul play (as determined by the coroner) was found on Prospector s Cove, a beach known for its distinctive sand. Someone stabbed
More informationMinerals of Earth s Crust
Chapter5 Chapter Outline Minerals of Earth s Crust 1 What Is a Mineral? Characteristics of Minerals Kinds of Minerals Crystalline Structure Crystalline Structure of Silicate Minerals Crystalline Structure
More informationPhysical Characteristics of Minerals
Physical Characteristics of Minerals 1. Introduction 2. Color Idiochromatism and the Chromophores Allochromatism 3. Streak 4. Luster 5. Density 6. Hardness The Mohs Scale The Diamond Indentation Method
More informationMagnificent Minerals By Satchel Harris
Magnificent Minerals By Satchel Harris Table of Contents What Is a Mineral?... 1 Cool ol Crystals... 3 Glorious Gemstones.. 7 Mischievous Myths about Minerals... 9 Minerals are Resources... 11 Glossary..
More information16 1 Minerals and Mineral Resources
Mining and Mineral Resources CHAPTER 16 1 Minerals and Mineral Resources 2 Mineral Exploration and Mining 3 Mining Regulations and Mine Reclamation READING WARM-UP Before you read this chapter, take a
More informationMineral Identification
Geosc 00 Spring 006 Lab Mineral Identification Your Geosc 00 instructors, Eliza and Dave, along with your Geosc 00 TAs, Emily and Brett, were invited to President Spanier s house to watch the Orange Bowl.
More informationAtoms to Minerals. Introduction to Geology Lecture. Tonight s Lecture. GLG 101 Jeff Simpson. brought to you by...
Introduction to Geology Lecture GLG 101 Jeff Simpson Atoms to Minerals Tonight s Lecture brought to you by... Na 2 B 4 O 7 10H 2 O Sodium Tetraborate Keep the study sheet handy while listening to this
More informationMINERALS MR. WHITE ADVANCED CONTENT EARTH SCIENCE
MINERALS MR. WHITE ADVANCED CONTENT EARTH SCIENCE WHO STUDIES THE EARTH S SURFACE & ITS CHANGING SHAPE? Geologists! GEOLOGISTS STUDY minerals rocks earthquakes volcanoes plate tectonics WHAT IS A MINERAL?
More informationTHE LINE FROM THE LODE
Volume 10, Issue 1 March 2009 Inside This issue Article: Mineral Identification Sorting Silicates Puzzle Page - Where Are We and Quick Quiz A Bit Of History Rock - On 2009 Info Field Trip Calendar T h
More informationMineral Identification
Name: Geosc 001 Spring 2008 Lab 3 Mineral Identification The basic goal of this lab is to introduce you to some basic ideas and strategies for identifying minerals, which are the building blocks of rocks
More informationMini Miners Monthly A Monthly Publication for Young Mineral Collectors. July 2015 Vol. 9 No. 7
Mini Miners Monthly A Monthly Publication for Young Mineral Collectors. July 2015 Vol. 9 No. 7 Many Mini Miners are out in the field digging for minerals and crystals at this time of year. We have a tradition
More information