SCOTT E. BARTON UNIMIN CORPORATION 500 WILSON PIKE CIRCLE, SUITE 127 BRENTWOOD, TENNESSEE USA EXECUTIVE SUMMARY

Size: px
Start display at page:

Download "SCOTT E. BARTON UNIMIN CORPORATION 500 WILSON PIKE CIRCLE, SUITE 127 BRENTWOOD, TENNESSEE USA EXECUTIVE SUMMARY"

Transcription

1 1 BENEFITS OF UTILIZING NEPHELINE SYENITE IN PORCELAIN TILE AND SANITARYWARE Proceedings of the 48 th Annual Meeting of the Brazilian Ceramic Society SCOTT E. BARTON UNIMIN CORPORATION 500 WILSON PIKE CIRCLE, SUITE 127 BRENTWOOD, TENNESSEE USA EXECUTIVE SUMMARY Nepheline syenite is a commercially prepared, rare feldspathoid-rich rock product that contributes both potassium and sodium oxides to the ceramic formulation. It has been used in both North America and Europe for the production of porcelain tile and sanitaryware for many years. It is the unique mineralogy and high levels of alkalis of nepheline syenite that justify its use in ceramics. These characteristics promote lower firing temperatures that can enhance productivity and lower production costs. Depending on location, the use of nepheline syenite can lower raw material cost by allowing more silica to be used in the formulation. Additionally, the process control found in most nepheline syenite operations offers a controlled level of Fe 2 O 3 that can help to improve fired color. The goal of this study is to illustrate the practical benefits of using nepheline syenite for the vitrification in a ceramic body formulation. Keywords: nepheline syenite, porcelain, tile, feldspar, sanitaryware INTRODUCTION As the porcelain tile and sanitaryware industries continue to globalize, manufacturers must continually improve the control and quality of their raw materials to effectively compete on the global scale. To do so, many manufacturers must look not only at domestic materials but also at external sources for these important requirements of quality and consistency. Nepheline syenite is one such product that is utilized on a global basis due to these requirements. Used both in ceramic bodies and glazes, nepheline syenite can both reduce vitrification temperature and allow for increased usage of more economic raw materials. More importantly, nepheline syenite can enhance productivity and quality in most ceramic applications. This paper will introduce nepheline syenite as a raw material and investigate its uses and benefits in porcelain tile formulation. Comments will also be made on its effect in other ceramic systems such as sanitaryware.

2 2 BACKGROUND ON NEPHELINE Anais do 48º SYENITE Congresso Brasileiro de Cerâmica Proceedings of the 48 th Annual Meeting of the Brazilian Ceramic Society GEOLOGY Nepheline syenite is an igneous rock, formed in a silica-deficient environment that is somewhat similar in appearance to granite. It is typically found as an irregularly shaped intrusion or in ring structures. The texture of the mineral is granitic and normally medium to coarse grained. Typically the most commercially viable deposits are found in intrusive structures with good liberation from contaminants such as biotite, hornblende and magnetite. Most noncommercial nepheline syenite deposits are gray or dark in color and have high iron levels that severely limit their potential in industrial applications. Those deposits associated with ring structures are especially difficult to beneficiate due to the extensive mixture of contaminant minerals. A few special ore reserves exist in Nephton and Blue Mountain, in Ontario, Canada, and on the island of Stjernøy in Norway where the ore is unusually light or near white in color. A third such deposit is located about 40 kilometers from Rio de Janeiro in the municipality of Duque de Caxias. Commercially, the Nephton/Blue Mountain deposit is an open pit operation owned and operated by Unimin Canada Ltd. The primary market for the Canadian material is the U.S. and Canada with ever increasing offshore usage due to industrial globalization. The Stjernøy deposit, owned and operated by North Cape Minerals AS, is both an underground and open-pit operation located on the island of Stjernøy in the Norwegian Arctic 1. Primary distribution for the Stjernøy materials is in Western Europe with the majority of product used in ceramic and glass applications. MINERALOGY Nepheline syenite is typically composed of three primary minerals: the albite form of feldspar, the microcline form of feldspar, and nepheline. The Norwegian and Brazilian deposits also contain what can be classified as perthitic feldspar, meaning a combination of sodium and potassium feldspar that began crystallization in solution but upon cooling became incompatible, forming sodium and potassium-rich lamellae. The percentages of each vary depending on the deposit location. The typical ceramic grade nepheline syenite will be composed of 20 to 30% nepheline. CHEMISTRY Nepheline syenite is anhydrous sodium potassium aluminosilicate. The typical chemical formulas for the components of nepheline syenite are: albite (Na 2 O Al 2 O 3 6SiO 2 ), microcline (K 2 O Al 2 O 3 6SiO 2 ), and nepheline (3Na 2 O 1K 2 O 4Al 2 O 3 8SiO 2 ). While pure nepheline has a theoretical chemistry of (Na 2 O Al 2 O 3 2SiO 2 ), it is normally found

3 3 to have a 1:3 substitution of potassium into the matrix. Table 1 gives the calculated chemical composition of nepheline compared to that of microcline and albite, the two most common forms Proceedings of feldspar. of the 48 th (Note Annual Meeting that SiO of the 2 Brazilian contained Ceramic in Society albite, microcline, and nepheline is not free-silica, because the silicon and oxygen are combined with Al as well as Na/K.) It is the nepheline component of nepheline syenite that separates its performance from feldspathic minerals. This component boosts the concentration of alumina and alkali oxide levels higher than that found in typical feldspar sources. Table I. Calculated Chemistries of Nepheline Syenite Components Oxides Nepheline Albite Microcline (Na 3, K) AlSiO 4 NaAlSi 3 O 8 KAlSi 3 O 8 Alumina 34.9% 19.4% 18.3% Silica 41.1% 68.7% 64.8% Soda 15.9% 11.8% Potash 8.1% 16.9% Physical Properties Nepheline syenite is a moderately hard feldspathoid mineral assemblage that is deficient in silica. As an igneous rock, nepheline syenite was formed from molten magma material from deep within the earth s crust. Unlike the igneous rock granite, which contains crystalline silica (SiO 2 ), nepheline syenite was formed in nature only when the molten material was deficient in that chemical combination. This deficiency in silica means that the cooling molten material did not form crystals of quartz or other forms of crystalline silica, but instead only formed the components of nepheline syenite. The Mohs hardness of the rock is about 6. It possesses a fairly low index of refraction, in the range of 1.50 to Table II. Typical properties of nepheline Syenite Particle Shape angular to nodular Specific Gravity g/cc Mohs Hardness 6.0 Refractive Index Figure 1. SEM photomicrograph of nepheline syenite grains at 5,000x.

4 4 MATERIALS AND METHODS The first step of this Proceedings project was of the to 48 th select Annual Meeting the raw of the materials Brazilian Ceramic for comparison Society and prepare the formulations. The goal of the project was to illustrate the benefits of utilizing nepheline syenite in porcelain tile formulations. Three (3) nepheline syenite products were identified from the three (3) main sources: Canada, Norway, and Brazil. Two (2) feldspar products were identified from the Brazilian tile market: F1 and F2. All of the fluxes were obtained in granular form, approximately 30 / +200 mesh. Additional materials necessary for the testing were ball clay and ground silica. Respectively Unimin Premier BL AF and Unimin Cerasil 200 were utilized. These materials were obtained in 200-mesh form. Each of the fluxes were ground to 2% +/- 0.5% retained on 200 mesh in 5 liter capacity laboratory jar mills. After each material was milled, chemical and physical analyses were made for use in preparing the theoretical formulations. Those analyses can be found below in Table III. Table III. Results of chemical and physical analysis of fluxes after milling Norway Canada Brazil F1 F2 Residue (%) (+) 200 mesh 1.97% 2.26% 2.11% 1.63% 1.55% (+) 325 mesh 19.03% 18.96% 20.79% 17.58% 18.24% (-) 325 mesh 79.00% 78.78% 77.11% 80.79% 80.20% Total Grinding Time 390 min 420 min 286 min 260 min 290 min SSA PSA 20m (-100 mesh) 10m m m m m <0.1 < Chemistry (by XRF) SiO Al2O Fe2O TiO MgO CaO K2O Na2O Total Alkali LOI 0.95 <0.05 < <0.05 Using these analyses, formulations were prepared in two (2) phases. The 1 st Phase used a set formula based on 45% ball clay, 10% silica, and 45% flux. This formula was based on porcelain tile formulations actually used in the Brazilian ceramic industry. The 2 nd Phase controlled the theoretical chemistry of the formulation by varying the flux and

5 5 silica levels, while holding the ball clay concentration constant. The formulations can be seen in Table IV. Proceedings of the 48 th Annual Meeting of the Brazilian Ceramic Society Table IV. Phase 1 and 2 Formulations Formulations Phase 1 Phase 2 Canada Norway Brazil F1 F2 Canada Norway Brazil F1/F2 Premiere BL AF Cerasil Canada Norway Brazil F F Total SiO Al 2 O Fe 2 O TiO MgO CaO K 2 O Na 2 O Total Alkali LOI Total A 57 mm circular steel die was used to prepare each disk. 40 grams of dry powder formulation was pressed to 20 metric tons of pressure. The moisture level was controlled to approximately 6% for each disk. In Phase 1, nine (9) disks of each formulation were prepared for 3 firing temperatures. In Phase 2, ten (10) disks of each formulation were prepared for 5 firing temperatures. The number was limited to allow for sufficient room in the kiln for firing all disks together. After drying at C, each disk was weighed and each diameter was measured for calculating loss on ignition (LOI) and fired shrinkage. The disks were then fired at the appropriate temperatures. Phase 1 temperatures consisted of C, C, and C. Phase 2 temperatures consisted of an initial firing of C, C, and C, followed by additional firings at C and C. All firings utilized a similar firing curve with a heating rate of 15 0 C per minute, maintaining maximum temperature for 30 minutes. Following firing, each disk was again weighed and diameter measured for completing the loss on ignition and fired shrinkage calculations. The disks were then analyzed for fired color and water absorption.

6 6 RESULTS AND DISCUSSION Both the Blue Mountain, Proceedings Canada of the and 48 th Annual Stjernøy, Meeting of Norway the Brazilian deposits Ceramic Society are currently producing ceramic grade nepheline syenite under the trade names Spectrum and Altaflux, respectively. The nepheline syenite sample from Brazil was obtained from the Duque de Caxias deposit near Rio de Janeiro. The Brazilian feldspar samples were obtained from a Brazilian porcelain tile producer. Due to potential differences in firing due to particle size, great care was taken in the preparation of the nepheline syenite and feldspar powders. By controlling the ground residue, each powder was produced to be as similar as possible. The Phase 1 formulations compare the relative performance of the different alkali sources in a standard formula. This illustrates the comparative firing performance of the nepheline syenite and feldspar samples at various temperatures. The results of Phase 1 can be found in Table V. From these results, it was determined that the level of alkali needed to be normalized in the formulations to better compare the fired properties. It was obvious that the initial firing of C resulted in over-firing of the nepheline syenite formulations. Additional firings were necessary to determine the firing range of the feldspar formulations, which was found to be between C and C. Table V. Averaged results from Phase C Shrinkage LOI Water Absorption GEB L a b Canada 8.56% 4.44% 0.04% Norway 8.84% 4.67% 0.07% Brazil 8.13% 4.62% 0.10% F1 6.88% 4.51% 2.76% F2 6.36% 4.76% 4.77% C Shrinkage LOI Water Absorption GEB L a b F1 7.79% 4.54% 0.43% F2 8.02% 4.79% 1.34% C Shrinkage LOI Water Absorption GEB L a b F1 6.91% 4.52% 0.19% F2 7.97% 4.78% 0.32% The Phase 2 formulations were calculated using theoretical chemical analyses. Modifying the silica and flux levels, the nepheline formulations were normalized to a target total alkali level (5.0%). That target alkali level was calculated from blending F1 and F2 at a ratio of 1:1 for use as 45% of the formulation, which was indicated to be the ratio currently used in the industry. The modified formulas were fired from C to C. The results are found below in Table VI. The results from Phase 2 (Table VI) illustrated good comparisons of fired quality between the different formulations. Maximum vitrification was achieved at approximately C. After that temperature, the shrinkages decrease and water absorption properties notably increase, indicating that there was bloating (expansion) in

7 7 the disk. The fired shrinkage and loss on ignition (LOI) were similar, with the F1/F2 blend having slightly lower shrinkage and slightly higher LOI. Proceedings of the 48 th Annual Meeting of the Brazilian Ceramic Society Table VI. Averaged fired results from Phase C Shrinkage LOI Water Absorption GEB L a b Canada 7.17% 4.54% 0.85% Norway 7.22% 4.60% 1.86% Brazil 6.98% 4.63% 1.16% F1/F2 7.21% 4.72% 1.85% C Shrinkage LOI Water Absorption GEB L a b Canada 8.24% 4.62% 0.33% Norway 7.93% 4.70% 0.37% Brazil 7.91% 4.70% 0.27% F1/F2 7.71% 4.82% 0.31% C Shrinkage LOI Water Absorption GEB L a b Canada 7.97% 4.66% 0.23% Norway 7.73% 4.74% 0.27% Brazil 7.83% 4.77% 0.24% F1/F2 7.53% 4.86% 0.23% C Shrinkage LOI Water Absorption GEB L a b Canada 7.20% 4.53% 0.30% Norway 7.02% 4.57% 0.52% Brazil 6.52% 4.58% 0.36% F1/F2 6.02% 4.66% 0.40% C Shrinkage LOI Water Absorption GEB L a b Canada 5.45% 4.53% 0.29% Norway 6.17% 4.61% 0.43% Brazil 5.58% 4.65% 0.47% F1/F2 4.72% 4.68% 0.76% The fired brightness of the nepheline syenite formulations was higher than the feldspar blend at virtually all temperatures. This improved fired brightness can mainly be attributed to the chemistry of the product. In commercial nepheline syenite deposits, iron-bearing contaminants such as biotite mica can normally be removed using separation techniques resulting in a product with a controlled iron (Fe 2 O 3 ) level. Since nepheline syenite contributes a greater concentration of alkali oxides to the batch, greater amounts of silica will be required. This increase in silica utilization will put a greater emphasis on obtaining a silica source low in coloring contaminants, such as iron (Fe 2 O 3 ). The fired brightness results can be found in Figure 2. Table VII. Calculated Coefficients of Thermal Expansion Coefficient of Thermal Expansion (x 10-6 ) C C Canada Norway Brazil Feldspar

8 8 Due to the major difference in the silica level of the nepheline syenite and feldspar formulations, thermal expansion was measured for the disks fired at C. This was the first temperature Proceedings that the of the fired 48 th Annual absorption Meeting of was the Brazilian lower Ceramic than Society 1.0%. The calculated thermal expansion coefficients are in Table VII above, and the graph is in Figure 3 below. The increased level of quartz in the formulation did increase the coefficient of thermal expansion for the nepheline syenite formulations. Some minor modifications to glaze formula may be required to prevent excessive compression in the body-to-glaze fit. Figure 2. Fired Brightness (GEB) Figure 3. Fired thermal expansion of Phase 2 fired disks

9 9 COMMENTS ON THE USE OF NEPHELINE SYENITE IN SANITARYWARE Anais do 48º Congresso In 2001, authors G. Klein and B. Ersen 2 Brasileiro de Cerâmica Proceedings of the 48 th Annual wrote Meeting of the Brazilian benefits Ceramic of Society using nepheline syenite versus feldspar in sanitaryware formulations. The authors conducted a very complete analysis of using three (3) formulations: feldspar only, feldspar/nepheline syenite, and nepheline syenite only. The levels of kaolinite, quartz, and alkali were controlled in the study. This resulted in the need to use additional quartz, as less nepheline syenite was necessary to achieve vitrification. Three (3) distinct advantages were observed using 100% nepheline syenite as the fluxing agent. 1. Relative amount of flux was reduced by 50%, substituted using quartz. 2. Higher mechanical strength after sintering. 3. Lower deformation during sintering. The advantages above are clearly evident when the feldspar (alkali) source is of low quality, and/or when a good quality silica source is readily available. As in our study, the thermal expansion was found to increase slightly with the use of nepheline syenite due to the increased quartz level in the formula. This increased quartz level could be attributed as the reason for the lower fired deformation observed. In situations where energy costs are high, a nepheline syenite source in sanitaryware could serve to lower firing temperatures and decrease gas consumption in the kilns. CONCLUSIONS Nepheline syenite is a powerful flux for use in virtually any ceramic formulation. The levels of alkalis found in existing nepheline syenite deposits are higher than feldspar and can help to lower the relative amount of flux used by up to 50%. This permits greater use of ground silica, which is usually more readily available, lower priced, and with lower iron-bearing contaminants than feldspathic rock. Alternatively, using higher levels of nepheline syenite, lower firing temperatures or faster firing cycles can be achieved, lowering energy consumption and increasing productivity. Commercially available with controlled, low-iron levels, this material can be utilized to produce the whitest fired colors. Combine these benefits with lower fired deformation and higher mechanical strength after sintering and you have a world-class product that is currently being shipped globally from deposits in Canada and Norway. Nepheline syenite could prove to be a tool that assists South American sanitaryware and tile producers to improve quality and export sales. REFERENCES [1] Potter, M.J. 2002, Feldspar and Nepheline Syenite, United States Geological Survey, viewed 12 August

10 << [2] Ersen, B. and Anais Klein do G. 48º 2001, Congresso (Translation) Brasileiro A de COMPARATIVE Cerâmica VIEW OF THE APPLICATION Proceedings OF of FELDSPAR the 48 th Annual Meeting AND of NEPHELIN the Brazilian Ceramic SYENITE Society RAW MATERIALS USED 28 de junho AS FLUXING a 1º de julho AGENTS de 2004 Curitiba-PR IN SILICA CERAMICS MATERIALS, Keramische Zeitschrift 53 (2001) [12] BENEFITS OF UTILIZING NEPHELINE SYENTITE IN PORCELAIN TILE AND SANITARYWARE As the porcelain tile and sanitaryware industries continue to globalize, manufacturers must continually improve the control and quality of their raw materials to effectively compete on the global scale. To do so, many manufacturers must look not only at domestic materials but also at external sources for these important requirements of quality and consistency. Nepheline Syenite is one such product that is utilized on a global basis due to these requirements. Used both in ceramic bodies and glazes, Nepheline Syenite can both reduce vitrification temperature and allow for increased usage of more economic raw materials. More importantly, Nepheline Syenite can enhance productivity and quality in most ceramic applications. This paper will investigate the uses and benefits of this valuable raw material in porcelain tile, with some additional commentary on its effect in other ceramic systems such as sanitaryware and glazes. Keywords: nepheline syenite, porcelain, tile, feldspar, sanitaryware

CERAMIC GLAZING as an IGNEOUS PROCESS

CERAMIC GLAZING as an IGNEOUS PROCESS GEOL 640: Geology through Global Arts and Artifacts CERAMIC GLAZING as an IGNEOUS PROCESS GLAZE COMPONENTS A glaze is a waterproof silica glass on the surface of a ceramic pot, and was first produced by

More information

IRUNGU PETER WACHIRA I13/3135/2008

IRUNGU PETER WACHIRA I13/3135/2008 IRUNGU PETER WACHIRA I13/3135/2008 Statement of the problem Objectives Study area Geology Materials and methods Data results and analysis Extraction mining and processing Uses and applications Recommendations

More information

Sintering behavior of feldspar rocks

Sintering behavior of feldspar rocks Research Inventy: International Journal Of Engineering And Science Vol.4, Issue 10 (October2014), PP 49-55 Issn (e): 2278-4721, Issn (p):2319-6483, www.researchinventy.com Sintering behavior of feldspar

More information

Sintering of feldspar rocks from czech quarries

Sintering of feldspar rocks from czech quarries Technical report Sintering of feldspar rocks from czech quarries Radomír SOKOLÁŘ ³ and Lucie VODOVÁ Brno University of Technology, Faculty of Civil Engineering, Institute of Technology of Building Materials

More information

23/9/2013 ENGINEERING GEOLOGY. Chapter 2: Rock classification:

23/9/2013 ENGINEERING GEOLOGY. Chapter 2: Rock classification: ENGINEERING GEOLOGY Chapter 2: Rock classification: ENGINEERING GEOLOGY Chapter 1.0: Introduction to engineering geology Chapter 2.0: Rock classification Igneous rocks Sedimentary rocks Metamorphic rocks

More information

About Earth Materials

About Earth Materials Grotzinger Jordan Understanding Earth Sixth Edition Chapter 3: EARTH MATERIALS Minerals and Rocks 2011 by W. H. Freeman and Company About Earth Materials All Earth materials are composed of atoms bound

More information

Name Class Date STUDY GUIDE FOR CONTENT MASTERY

Name Class Date STUDY GUIDE FOR CONTENT MASTERY Igneous Rocks What are igneous rocks? In your textbook, read about the nature of igneous rocks. Use each of the terms below just once to complete the following statements. extrusive igneous rock intrusive

More information

9/4/2015. Feldspars White, pink, variable Clays White perfect Quartz Colourless, white, red, None

9/4/2015. Feldspars White, pink, variable Clays White perfect Quartz Colourless, white, red, None ENGINEERING GEOLOGY Chapter 1.0: Introduction to engineering geology Chapter 2.0: Rock classification Igneous rocks Sedimentary rocks Metamorphic rocks Chapter 3.0: Weathering & soils Chapter 4.0: Geological

More information

Name Class Date. 1. In your own words, write a definition for the term rock cycle.

Name Class Date. 1. In your own words, write a definition for the term rock cycle. Skills Worksheet Chapter Review USING KEY TERMS 1. In your own words, write a definition for the term rock cycle. Complete each of the following sentences by choosing the correct term from the word bank.

More information

Rocks and Minerals. Tillery, Chapter 19. Solid Earth Materials

Rocks and Minerals. Tillery, Chapter 19. Solid Earth Materials Rocks and Minerals Tillery, Chapter 19 Science 330 Summer 2007 No other planet in the solar system has the unique combination of fluids of Earth. Earth has a surface that is mostly covered with liquid

More information

Name Class Date STUDY GUIDE FOR CONTENT MASTERY

Name Class Date STUDY GUIDE FOR CONTENT MASTERY Igneous Rocks What are igneous rocks? In your textbook, read about the nature of igneous rocks. Use each of the terms below just once to complete the following statements. extrusive igneous rock intrusive

More information

305 ATOMS, ELEMENTS, AND MINERALS

305 ATOMS, ELEMENTS, AND MINERALS DATE DUE: Name: Instructor: Ms. Terry J. Boroughs Geology 305 ATOMS, ELEMENTS, AND MINERALS Instructions: Read each question carefully before selecting the BEST answer. Use GEOLOGIC VOCABULARY where APPLICABLE!

More information

THE ROCK CYCLE & ROCKS. Subtitle

THE ROCK CYCLE & ROCKS. Subtitle THE ROCK CYCLE & ROCKS Subtitle 3. Three rocks that do not have minerals or are composed of nonmineral matter. Coal Pumuce Obsidian THE ROCK CYCLE Why do scientists study rocks? Rocks contain clues about

More information

10/20/2015. How is magma different from lava? Magma is molten rock below the Earth s surface. Lava is magma that flows out onto Earth s surface.

10/20/2015. How is magma different from lava? Magma is molten rock below the Earth s surface. Lava is magma that flows out onto Earth s surface. Chapter 5 What are igneous rocks? How do they form? Igneous rocks are rocks that form when molten material cools and crystallizes. Molten material can be either magma or lava. How is magma different from

More information

Minerals: Building Blocks of Rocks Chapter 2. Based on: Earth Science, 10e

Minerals: Building Blocks of Rocks Chapter 2. Based on: Earth Science, 10e Minerals: Building Blocks of Rocks Chapter 2 Based on: Earth Science, 10e Minerals: the building blocks of rocks Definition of a mineral Solid Inorganic Natural Crystalline Structure - Possess an orderly

More information

Lab 6 - Identification of Metamorphic Rocks

Lab 6 - Identification of Metamorphic Rocks Lab 6 - Identification of Metamorphic Rocks Page - Introduction Metamorphic rocks are the third great rock group. The term meta means to change and morph means form. Metamorphic rocks are rocks who have

More information

Igneous Rocks. Igneous Rocks - 1. Environment of Formation - Magma - Plutonic - rock that formed within the Earth. Intrusive - Earth s crust.

Igneous Rocks. Igneous Rocks - 1. Environment of Formation - Magma - Plutonic - rock that formed within the Earth. Intrusive - Earth s crust. Name: Date: Period: Minerals and Rocks The Physical Setting: Earth Science CLASS NOTES - Methods to classify igneous rocks: 1. Environment of Formation - Magma - Plutonic - rock that formed within the

More information

305 ATOMS, ELEMENTS, AND MINERALS

305 ATOMS, ELEMENTS, AND MINERALS DATE DUE: Name: Instructor: Ms. Terry J. Boroughs Geology 305 ATOMS, ELEMENTS, AND MINERALS Instructions: Read each question carefully before selecting the BEST answer. Use GEOLOGIC VOCABULARY where APPLICABLE!

More information

Earth Materials II Review Optical Mineralogy and Igneous Minerals

Earth Materials II Review Optical Mineralogy and Igneous Minerals Earth Materials II Review Optical Mineralogy and Igneous Minerals Refractive Index and Angle of Refraction Refractive Index(R. I. ) = velocity of light in a vacuum velocity of light in a medium The refractive

More information

A rock is a naturally occurring solid mixture of one or more minerals, or organic matter

A rock is a naturally occurring solid mixture of one or more minerals, or organic matter A rock is a naturally occurring solid mixture of one or more minerals, or organic matter Rocks are classified by how they are formed, their composition, and texture Rocks change over time through the rock

More information

Rocks Rock- A group of minerals, glass, mineroid bound together in some way.

Rocks Rock- A group of minerals, glass, mineroid bound together in some way. Rocks Rock- A group of minerals, glass, mineroid bound together in some way. All rocks fit into one of three categories: Igneous- formed by the cooling and hardening of hot molten rock Sedimentary- formed

More information

Student Name: College: Grade:

Student Name: College: Grade: Student Name: College: Grade: Physical Geology Laboratory IGNEOUS MINERALS AND ROCKS IDENTIFICATION - INTRODUCTION & PURPOSE: In this lab you will learn to identify igneous rocks in hand samples from their

More information

Practice Test Rocks and Minerals. Name. Page 1

Practice Test Rocks and Minerals. Name. Page 1 Name Practice Test Rocks and Minerals 1. Which rock would be the best source of the mineral garnet? A) basalt B) limestone C) schist D) slate 2. Which mineral is mined for its iron content? A) hematite

More information

IGNEOUS ROCKS. SECTION 5.1 What are igneous rocks?

IGNEOUS ROCKS. SECTION 5.1 What are igneous rocks? Date Period Name IGNEOUS ROCKS SECTION.1 What are igneous rocks? In your textbook, read about the nature of igneous rocks. Use each of the terms below just once to complete the following statements. basaltic

More information

LAB 5: COMMON MINERALS IN IGNEOUS ROCKS

LAB 5: COMMON MINERALS IN IGNEOUS ROCKS EESC 2100: Mineralogy LAB 5: COMMON MINERALS IN IGNEOUS ROCKS Part 1: Minerals in Granitic Rocks Learning Objectives: Students will be able to identify the most common minerals in granitoids Students will

More information

Engineering Geology ECIV 2204

Engineering Geology ECIV 2204 Engineering Geology ECIV 2204 Instructor : Dr. Jehad Hamad 2017-2016 Chapter (3) Igneous Rocks Chapter 3: Rocks: Materials of the Solid Earth Igneous Rocks Chapter 3: Rocks: Materials of the Solid Earth

More information

305 ATOMS, ELEMENTS, AND MINERALS

305 ATOMS, ELEMENTS, AND MINERALS DATE DUE: Name: Instructor: Ms. Terry J. Boroughs Geology 305 ATOMS, ELEMENTS, AND MINERALS Instructions: Read each question carefully before selecting the BEST answer. Use GEOLOGIC VOCABULARY where APPLICABLE!

More information

Wikipedia.org BUILDING STONES. Chapter 4. Materials of Construction-Building Stones 1

Wikipedia.org BUILDING STONES. Chapter 4. Materials of Construction-Building Stones 1 Wikipedia.org BUILDING STONES Chapter 4 Materials of Construction-Building Stones 1 What is Stone? Stone is a concretion of mineral matter. Used either as a; Construction material, Manufacture of other

More information

Chapter: Earth Materials

Chapter: Earth Materials Table of Contents Chapter: Earth Materials Section 1: Minerals Section 2: Igneous Rocks Section 3: Sedimentary Rocks Section 4: Metamorphic Rocks and the Rock Cycle 1 Minerals Common Elements Composition

More information

Physical Geology 101 Laboratory MINERALS II Silicate and Carbonate Rock-Forming Minerals

Physical Geology 101 Laboratory MINERALS II Silicate and Carbonate Rock-Forming Minerals Student Name: College: Grade: Physical Geology 101 Laboratory MINERALS II Silicate and Carbonate Rock-Forming Minerals I. INTRODUCTION: The purpose of this lab is you will improve your mineral identification

More information

305 ATOMS, ELEMENTS, AND MINERALS

305 ATOMS, ELEMENTS, AND MINERALS DATE DUE: Name: Instructor: Ms. Terry J. Boroughs Geology 305 ATOMS, ELEMENTS, AND MINERALS Instructions: Read each question carefully before selecting the BEST answer. Use GEOLOGIC VOCABULARY where APPLICABLE!

More information

300 ATOMS, ELEMENTS, AND MINERALS

300 ATOMS, ELEMENTS, AND MINERALS DATE DUE: Name: Instructor: Ms. Terry J. Boroughs Geology 300 ATOMS, ELEMENTS, AND MINERALS Instructions: Read each question carefully before selecting the BEST answer. Use GEOLOGIC VOCABULARY where APPLICABLE!

More information

Liz LaRosa Images from Geology.com unless otherwise noted

Liz LaRosa Images from Geology.com unless otherwise noted Liz LaRosa http://www.middleschoolscience.com 2010 Images from Geology.com unless otherwise noted A rock is a naturally occurring solid mixture of one or more minerals, or organic matter Rocks are classified

More information

Lecture Outlines PowerPoint. Chapter 2 Earth Science 11e Tarbuck/Lutgens

Lecture Outlines PowerPoint. Chapter 2 Earth Science 11e Tarbuck/Lutgens Lecture Outlines PowerPoint Chapter 2 Earth Science 11e Tarbuck/Lutgens 2006 Pearson Prentice Hall This work is protected by United States copyright laws and is provided solely for the use of instructors

More information

2. REPLACEMENT OF PRIMARY PLAGIOCLASE BY SECONDARY K-FELDSPAR AND MYRMEKITE

2. REPLACEMENT OF PRIMARY PLAGIOCLASE BY SECONDARY K-FELDSPAR AND MYRMEKITE 1 ISSN 1526-5757 2. REPLACEMENT OF PRIMARY PLAGIOCLASE BY SECONDARY K-FELDSPAR AND MYRMEKITE Lorence G. Collins email: lorencec@sysmatrix.net November 21, 1996; revised February 17, 1997 The following

More information

Earth Science 11: Earth Materials: Rock Cycle

Earth Science 11: Earth Materials: Rock Cycle Name: Date: Earth Science 11: Earth Materials: Rock Cycle Chapter 2, pages 44 to 46 2.1: Rock Cycle What is a Rock? A solid mass of mineral or mineral-like matter that occurs naturally as part of our planet

More information

Soil Mechanics/Geotechnical Engineering I Prof. Dilip Kumar Baidya Department of Civil Engineering Indian Institute of Technology, Kharagpur

Soil Mechanics/Geotechnical Engineering I Prof. Dilip Kumar Baidya Department of Civil Engineering Indian Institute of Technology, Kharagpur Soil Mechanics/Geotechnical Engineering I Prof. Dilip Kumar Baidya Department of Civil Engineering Indian Institute of Technology, Kharagpur Lecture - 01 Rock Cycle Good morning. I welcome you to this

More information

Lorence G. Collins. July 9, 1997

Lorence G. Collins.   July 9, 1997 1 ISSN 1526-5757 20. FAILURE OF THE EXSOLUTION SILICA-PUMP MODEL FOR THE ORIGIN OF MYRMEKITE: EXAMINATION OF K-FELDSPAR CRYSTALS IN THE SHARPNERS POND TONALITE, MASSACHUSETTS, USA Introduction Lorence

More information

To get you thinking What natural process is responsible for the appearance of these rocks? Rocks and the Rock Cycle

To get you thinking What natural process is responsible for the appearance of these rocks? Rocks and the Rock Cycle To get you thinking What natural process is responsible for the appearance of these rocks? Rocks and the Rock Cycle Bell Ringer Name the 3 types of rock. Is one type of rock able to change into a different

More information

Review - Unit 2 - Rocks and Minerals

Review - Unit 2 - Rocks and Minerals Review - Unit 2 - Rocks and Minerals Base your answers to questions 1 and 2 on the diagram below, which shows the results of three different physical tests, A, B, and C, that were performed on a mineral.

More information

Unit 2 Exam: Rocks & Minerals

Unit 2 Exam: Rocks & Minerals Name: Date: 1. Base your answer(s) to the following question(s) on the 2001 edition of the Earth Science Reference Tables, the map and cross section below, and your knowledge of Earth science. The shaded

More information

Evaluation and Beneficiation of Feldspar from Arkosic Sandstone in South Jordan for Application in the Ceramic Industry

Evaluation and Beneficiation of Feldspar from Arkosic Sandstone in South Jordan for Application in the Ceramic Industry American Journal of Applied Sciences 3 (1): 1655-1661, 26 ISSN 1546-9239 26 Science Publications Evaluation and Beneficiation of Feldspar from Arkosic Sandstone in South Jordan for Application in the Ceramic

More information

Igneous, Metamorphic & Sedimentary. Chapter 5 & Chapter 6

Igneous, Metamorphic & Sedimentary. Chapter 5 & Chapter 6 Igneous, Metamorphic & Sedimentary Chapter 5 & Chapter 6 Section 5.1 What are Igneous Rocks? Compare and contrast intrusive and extrusive igneous rocks. Describe the composition of magma Discuss the factors

More information

EARTH SCIENCE. Geology, the Environment and the Universe. Chapter 5: Igneous Rocks

EARTH SCIENCE. Geology, the Environment and the Universe. Chapter 5: Igneous Rocks EARTH SCIENCE Geology, the Environment and the Universe Chapter 5: Igneous Rocks CHAPTER 5 Igneous Rocks Section 5.1 What are igneous rocks? Section 5.2 Classification of Igneous Rocks Click a hyperlink

More information

Rocks. 3.1 The Rock Cycle. 3.1 The Rock Cycle. 3.1 The Rock Cycle. The Rock Cycle. I. Rocks

Rocks. 3.1 The Rock Cycle. 3.1 The Rock Cycle. 3.1 The Rock Cycle. The Rock Cycle. I. Rocks Rocks Tarbuck Lutgens 3.1 The Rock Cycle 3.1 The Rock Cycle I. Rocks Rocks are any solid mass of mineral or mineral-like matter occurring naturally as part of our planet. Types of Rocks 1. Igneous rock

More information

Topics that will be discussed

Topics that will be discussed Topics that will be discussed The Rock Cycle Igneous Rock Sedimentary Rock Metamorphic Rock The Rock Cycle -Rocks The parent material for all rocks is MAGMA. What is MAGMA? -Rock forming Minerals Are:

More information

Lab 4 - Identification of Igneous Rocks

Lab 4 - Identification of Igneous Rocks Lab 4 - Identification of Igneous Rocks Page - Introduction A rock is a substance made up of one or more different minerals. Thus an essential part of rock identification is the ability to correctly recognize

More information

Lab 3 - Identification of Igneous Rocks

Lab 3 - Identification of Igneous Rocks Lab 3 - Identification of Igneous Rocks Page - 1 Introduction A rock is a substance made up of one or more different minerals. Thus an essential part of rock identification is the ability to correctly

More information

Chapter 10. Chapter Rocks and the Rock Cycle. Rocks. Section 1 Rocks and the Rock Cycle

Chapter 10. Chapter Rocks and the Rock Cycle. Rocks. Section 1 Rocks and the Rock Cycle Chapter 10 Rocks 1 Chapter 10 Section 1 Rocks and the Rock Cycle 2 10.1 Rocks and the Rock Cycle Magma is the parent material for all rocks. Once the magma cools and hardens, many changes can occur. Geology:

More information

Prentice Hall EARTH SCIENCE

Prentice Hall EARTH SCIENCE Prentice Hall EARTH SCIENCE Tarbuck Lutgens Chapter 3 Rocks 3.1 The Rock Cycle Rocks Rocks are any solid mass of mineral or mineral-like matter occurring naturally as part of our planet. Types of Rocks

More information

GEOL3313 Petrology of Igneous and Metamorphic Rocks G. Mattioli, Dept. of Geosciences, Univ. of Arkansas, Spring 2008

GEOL3313 Petrology of Igneous and Metamorphic Rocks G. Mattioli, Dept. of Geosciences, Univ. of Arkansas, Spring 2008 GEOL3313 Petrology of Igneous and Metamorphic Rocks G. Mattioli, Dept. of Geosciences, Univ. of Arkansas, Spring 2008 Homework Assignment 3 Calculation of CIPW Norm Due in Class February 13, 2008 Problem

More information

Igneous Rock Classification, Processes and Identification Physical Geology GEOL 100

Igneous Rock Classification, Processes and Identification Physical Geology GEOL 100 Igneous Rock Classification, Processes and Identification Physical Geology GEOL 100 Ray Rector - Instructor Major Concepts 1) Igneous rocks form directly from the crystallization of a magma or lava 2)

More information

Minerals. What are minerals and how do we classify them?

Minerals. What are minerals and how do we classify them? Minerals What are minerals and how do we classify them? 1 Minerals! Minerals are the ingredients needed to form the different types of rocks! Rock - is any naturally formed solid that is part of Earth

More information

Rocks: Materials of the Solid Earth

Rocks: Materials of the Solid Earth 1 Rocks: Materials of the Solid Earth Presentation modified from: Instructor Resource Center on CD-ROM, Foundations of Earth Science,, 4 th Edition, Lutgens/Tarbuck, Rock Cycle Igneous Rocks Today 2 Rock

More information

Name Class Date. In your textbook, read about the nature of igneous rocks. Use each of the terms below just once to complete the following statements.

Name Class Date. In your textbook, read about the nature of igneous rocks. Use each of the terms below just once to complete the following statements. CHAPTER 5 Igneous Rocks SECTION 5.1 What are igneous rocks? In your textbook, read about the nature of igneous rocks. Use each of the terms below just once to complete the following statements. basaltic

More information

Directed Reading. Section: Rocks and the Rock Cycle. made of a. inorganic matter. b. solid organic matter. c. liquid organic matter. d. chemicals.

Directed Reading. Section: Rocks and the Rock Cycle. made of a. inorganic matter. b. solid organic matter. c. liquid organic matter. d. chemicals. Skills Worksheet Directed Reading Section: Rocks and the Rock Cycle 1. The solid part of Earth is made up of material called a. glacial ice. b. lava. c. rock. d. wood. 2. Rock can be a collection of one

More information

SAMREC 2009 Table 1, Section 5.5 Treatment / Processing

SAMREC 2009 Table 1, Section 5.5 Treatment / Processing Volume 58 ~ Number TWO ~ JUNE 2015 SAMREC 2009 Table 1, Section 5.5 Treatment / Processing ASSESSMENT CRITERION: T 5.5 Treatment / Processing EXPLORATION RESULTS (A) (i) Describe any obvious processing

More information

Earth Science 11: Minerals

Earth Science 11: Minerals lname: Date: Earth Science 11: Minerals Purpose: Text Pages: I can identify and classify minerals using their physical and chemical properties 90-111 *This is recommended reading! Matter and Atoms (5.1)

More information

The most common elements that make up minerals are oxygen, silicon, aluminum, iron, calcium, potassium, and magnesium

The most common elements that make up minerals are oxygen, silicon, aluminum, iron, calcium, potassium, and magnesium Mineralogy: The Study of Minerals and their Properties A Mineral! Occurs! Is a! Is a substance (element or compound)! Has atoms arrange in an orderly pattern ( )! Is (not formed by any process involving

More information

Page 1. Name:

Page 1. Name: Name: 1) What is the approximate density of a mineral with a mass of 262.2 grams that displaces 46 cubic centimeters of water? A) 6.1 g/cm 3 C) 1.8 g/cm 3 B) 5.7 g/cm 3 D) 12.2 g/cm 3 2) In which two Earth

More information

Rocks and the Rock Cycle notes from the textbook, integrated with original contributions

Rocks and the Rock Cycle notes from the textbook, integrated with original contributions Rocks and the Rock Cycle notes from the textbook, integrated with original contributions Alessandro Grippo, Ph.D. Gneiss (a metamorphic rock) from Catalina Island, California Alessandro Grippo review Rocks

More information

6/20/2018. Lesson 1 (Properties of Minerals) 6 th Grade. Earth s Structure Chapter 2: Minerals and Rocks. density =

6/20/2018. Lesson 1 (Properties of Minerals) 6 th Grade. Earth s Structure Chapter 2: Minerals and Rocks. density = 6 th Grade Earth s Structure Chapter 2: Minerals and Rocks Mineral Lesson 1 (Properties of Minerals) a mineral must meet all four of the following requirements: 1. must be naturally-occurring (formed by

More information

This is how we classify minerals! Silicates and Non-Silicates

This is how we classify minerals! Silicates and Non-Silicates Why are some minerals harder than others? Their atomic structure and chemical formula. This is how we classify minerals! Silicates and Non-Silicates Part #1 - Silicates: Silicon and Oxygen make up 70%

More information

Igneous Rocks. Sedimentary Rocks. Metamorphic Rocks

Igneous Rocks. Sedimentary Rocks. Metamorphic Rocks Name: Date: Igneous Rocks Igneous rocks form from the solidification of magma either below (intrusive igneous rocks) or above (extrusive igneous rocks) the Earth s surface. For example, the igneous rock

More information

The Production of Sediment. Contents. Weathering. Chapters 1, 3

The Production of Sediment. Contents. Weathering. Chapters 1, 3 The Production of Sediment Chapters 1, 3 Contents Weathering Physical, chemical, biogeochemical processes Rates Products Carbon cycle and global change Erosion/Soils Sediment Texture Weathering General

More information

I m good. Thank you.

I m good. Thank you. I m good. Thank you. The Rock Cycle Ag Earth Science Chapter 3.1 A natural occurring, inorganic crystalline material with a unique chemical composition. mineral A consolidated mixture of minerals rock

More information

Lab 2: The rock cycle, minerals and igneous rocks. Rocks are divided into three major categories on the basis of their origin:

Lab 2: The rock cycle, minerals and igneous rocks. Rocks are divided into three major categories on the basis of their origin: Geology 101 Name(s): Lab 2: The rock cycle, minerals and igneous rocks Rocks are divided into three major categories on the basis of their origin: Igneous rocks (from the Latin word, ignis = fire) are

More information

Classification of Igneous Rocks

Classification of Igneous Rocks Classification of Igneous Rocks Textures: Glassy- no crystals formed Aphanitic- crystals too small to see by eye Phaneritic- can see the constituent minerals Fine grained- < 1 mm diameter Medium grained-

More information

Mineral Marketing, Inc.

Mineral Marketing, Inc. Mineral Marketing, Inc. P.O. Box 343 Rough & Ready, Calif. 95975 Telephone (916) 273-8819 (916) 273-8811 0005032857 A STUDY OF MARKETS FOR BRITISH COLUMBIA'S NEPHELINE SYENITE AND FELDSPATHIC MINERALS

More information

PLATE TECTONICS, VOLCANISM AND IGNEOUS ROCKS

PLATE TECTONICS, VOLCANISM AND IGNEOUS ROCKS PLATE TECTONICS, VOLCANISM AND IGNEOUS ROCKS PLATE TECTONICS TO IGNEOUS ROCKS Internal Heat Seafloor Spreading/Plate Tectonics Volcanism Plate Boundary Intra-plate (hot spot) Divergent Convergent Igneous

More information

What Do You See? Learning Outcomes Goals Learning Outcomes Think About It Identify classify In what kinds of environments do igneous rocks form?

What Do You See? Learning Outcomes Goals Learning Outcomes Think About It Identify classify In what kinds of environments do igneous rocks form? Section 2 Igneous Rocks and the Geologic History of Your Community What Do You See? Learning Outcomes In this section, you will Goals Text Learning Outcomes In this section, you will Identify and classify

More information

Economic Ores. - Mostly metals

Economic Ores. - Mostly metals Economic Ores - Mostly metals Intro points An ore is a naturally occurring solid material from which a metal or valuable mineral can be profitably extracted. Gangue is the commercially valueless material

More information

CERAMIC MATERIALS I. Asst. Prof. Dr. Ayşe KALEMTAŞ

CERAMIC MATERIALS I. Asst. Prof. Dr. Ayşe KALEMTAŞ CERAMIC MATERIALS I akalemtas@mu.edu.tr, akalemtas@gmail.com, Phone: 211 19 17 Metallurgical and Materials Engineering Department Traditional Ceramics Clay products Main Components Clay Feldspar Silica

More information

LAB 2: SILICATE MINERALS

LAB 2: SILICATE MINERALS GEOLOGY 640: Geology through Global Arts and Artifacts LAB 2: SILICATE MINERALS FRAMEWORK SILICATES The framework silicates quartz and feldspar are the most common minerals in Earth s crust. Quartz (SiO

More information

organisms CaCO 3 + H 2 O + CO 2 shallow water

organisms CaCO 3 + H 2 O + CO 2 shallow water Weathering and Reverse weathering Step I:Weathering of igneous rocks 1. Igneous rocks are mainly composed of Al, Si and O 2 with minor and varying quantities of Na, K, Ca and Mg composing pheldspar minerals

More information

A Rock is a solid aggregate of minerals.

A Rock is a solid aggregate of minerals. Quartz A Rock is a solid aggregate of minerals. Orthoclase Feldspar Plagioclase Feldspar Biotite Four different minerals are obvious in this piece of Granite. The average automobile contains: Minerals

More information

Minerals. Atoms, Elements, and Chemical Bonding. Definition of a Mineral 2-1

Minerals. Atoms, Elements, and Chemical Bonding. Definition of a Mineral 2-1 Minerals In order to define a what we mean by a mineral we must first make some definitions: 2-1 Most of the Earth s surface is composed of rocky material. An element is a substance which cannot be broken

More information

Happy Tuesday. Pull out a ½ sheet of paper

Happy Tuesday. Pull out a ½ sheet of paper Happy Tuesday Pull out a ½ sheet of paper 1. Physical properties of a mineral are predominantly related to 1. the external conditions of temperature, pressure, and amount of space available for growth.

More information

The 3 types of rocks:

The 3 types of rocks: Igneous Rocks and Intrusive Igneous Activity The 3 types of rocks:! Sedimentary! Igneous! Metamorphic Marble 1 10/7/15 SEDIMENTARY ROCKS Come from rocks sediments (rock fragments, sand, silt, etc.) Fossils

More information

Matter and Minerals Earth: Chapter Pearson Education, Inc.

Matter and Minerals Earth: Chapter Pearson Education, Inc. Matter and Minerals Earth: Chapter 3 Minerals: Building Blocks of Rocks By definition a mineral is: Naturally occurring An inorganic solid Ordered internal molecular structure Definite chemical composition

More information

LAB 2 IDENTIFYING MATERIALS FOR MAKING SOILS: ROCK AND PARENT MATERIALS

LAB 2 IDENTIFYING MATERIALS FOR MAKING SOILS: ROCK AND PARENT MATERIALS LAB 2 IDENTIFYING MATERIALS FOR MAKING SOILS: ROCK AND PARENT MATERIALS Learning outcomes The student is able to: 1. understand and identify rocks 2. understand and identify parent materials 3. recognize

More information

GLY 155 Introduction to Physical Geology, W. Altermann

GLY 155 Introduction to Physical Geology, W. Altermann Earth Materials Systematic subdivision of magmatic rocks Subdivision of magmatic rocks according to their mineral components: Content of quartz SiO 2 ( free quartz presence) Quartz with conchoidal breakage

More information

Chapter 4 8/27/2013. Igneous Rocks. and Intrusive Igneous Activity. Introduction. The Properties and Behavior of Magma and Lava

Chapter 4 8/27/2013. Igneous Rocks. and Intrusive Igneous Activity. Introduction. The Properties and Behavior of Magma and Lava Introduction Chapter 4 Igneous rocks form by the cooling of magma (or lava). Large parts of the continents and all the oceanic crust are composed of. and Intrusive Igneous Activity The Properties and Behavior

More information

Rocks and Minerals (rocksandminerals)

Rocks and Minerals (rocksandminerals) Name: Date: 1. Cleavage of a mineral is related to a mineral's A. chemical composition. B. streak color. C. luster. D. crystalline structure. 2. Which is not part of the definition of a mineral? A. naturally

More information

Quartz. ! Naturally occurring - formed by nature. ! Solid - not liquid or gas. Liquid water is not a mineral

Quartz. ! Naturally occurring - formed by nature. ! Solid - not liquid or gas. Liquid water is not a mineral GEOL 110 - Minerals, Igneous Rocks Minerals Diamond Azurite Quartz Why Study Minerals?! Rocks = aggregates of minerals! Importance to Society?! Importance to Geology? 5 part definition, must satisfy all

More information

(Investment Opportunities) Mian K. Habib Industrial Minerals Canada Consulting Inc. Hamilton, ON L9A 2M2 Canada

(Investment Opportunities) Mian K. Habib Industrial Minerals Canada Consulting Inc. Hamilton, ON L9A 2M2 Canada (Investment Opportunities) Mian K. Habib Industrial Minerals Canada Consulting Inc. Hamilton, ON L9A 2M2 Canada Mian@indmin.ca Industrial Minerals Congress 24, 57 June 2018 Barcelona, Spain Proterozoic

More information

UNIT TOPICS TOPIC 1: MINERALS TOPIC 2: IGNEOUS ROCKS TOPIC 3: SEDIMENTARY ROCKS TOPIC 4: METAMORPHIC ROCKS TOPIC 5: THE ROCK CYCLE

UNIT TOPICS TOPIC 1: MINERALS TOPIC 2: IGNEOUS ROCKS TOPIC 3: SEDIMENTARY ROCKS TOPIC 4: METAMORPHIC ROCKS TOPIC 5: THE ROCK CYCLE UNIT TOPICS TOPIC 1: MINERALS TOPIC 2: IGNEOUS ROCKS TOPIC 3: SEDIMENTARY ROCKS TOPIC 4: METAMORPHIC ROCKS TOPIC 5: THE ROCK CYCLE TOPIC 1: MINERALS ESSENTIAL QUESTION: WHAT ARE MINERALS AND HOW DO WE

More information

Science for Potters. Linda Bloomfield

Science for Potters. Linda Bloomfield Science for Potters Linda Bloomfield Table of Contents Acknowledgements... v Introduction... x Chapter 1. Chemistry for Potters.... 1 Elements.... 2 Structure of the Atom.... 2 Symbols... 3 Molecules....

More information

Block: Igneous Rocks. From this list, select the terms which answer the following questions.

Block: Igneous Rocks. From this list, select the terms which answer the following questions. Geology 12 Name: Mix and Match: Igneous Rocks Refer to the following list. Block: porphyritic volatiles mafic glassy magma mixing concordant discontinuous reaction series igneous vesicular partial melting

More information

GEOCHEMISTRY AND MINERALOGICAL EVALUATION OF QUARTZITE BEARING KYANITE IN KUTA, NORTHWESTERN NIGERIA. Omang, B. O. 1 and *Alabi, A. A.

GEOCHEMISTRY AND MINERALOGICAL EVALUATION OF QUARTZITE BEARING KYANITE IN KUTA, NORTHWESTERN NIGERIA. Omang, B. O. 1 and *Alabi, A. A. GEOCHEMISTRY AND MINERALOGICAL EVALUATION OF QUARTZITE BEARING KYANITE IN KUTA, NORTHWESTERN NIGERIA. Omang, B. O. 1 and *Alabi, A. A. 2 Abstract DOI:http://dx.doi.org/10.4314/ejesm.v4i3.11 Received October

More information

SAGE GOLD INC. MINERAL BENEFICIATION ON CANE GOLD ORE. RPC Reference No.: PET-J1557. Prepared for:

SAGE GOLD INC. MINERAL BENEFICIATION ON CANE GOLD ORE. RPC Reference No.: PET-J1557. Prepared for: SAGE GOLD INC. MINERAL BENEFICIATION ON CANE GOLD ORE Prepared for: Mr. Bill Love Sage Gold Inc. 365 Bay Street, Suite 500 Toronto, Ontario Canada, M5H 2V1 Prepared by: Ross Gilders Section Head, Process

More information

Igneous Rock Notes. Page #:

Igneous Rock Notes. Page #: Page #: Igneous Rock Notes Magma and lava form very different types of igneous rocks. Igneous rocks form from molten rock, but where does molten rock come from? The temperature inside Earth with depth.

More information

ESS Minerals. Lee. 1. The table below shows some properties of four different minerals.

ESS Minerals. Lee. 1. The table below shows some properties of four different minerals. Name: ESS Minerals Pd. 1. The table below shows some properties of four different minerals. The minerals listed in the table are varieties of which mineral? (A) garnet (B) magnetite (C) olivine (D) quartz

More information

Plate tectonics, rock cycle

Plate tectonics, rock cycle Dikes, Antarctica Rock Cycle Plate tectonics, rock cycle The Rock Cycle A rock is a naturally formed, consolidated material usually composed of grains of one or more minerals The rock cycle shows how one

More information

Rock Cycle and Rock Types Homework

Rock Cycle and Rock Types Homework Rock Cycle and Rock Types Homework Completion Complete each statement. 1. A(n) is a solid mass of mineral or mineral-like matter that occurs naturally. 2. Rocks are generally classified as igneous,, or

More information

Examining Minerals and Rocks

Examining Minerals and Rocks Examining Minerals and Rocks What is a mineral? A mineral is homogenous, naturally occurring substance formed through geological processes that has a characteristic chemical composition, a highly ordered

More information

Upgrading Feldspar by WHIMS and Flotation Techniques

Upgrading Feldspar by WHIMS and Flotation Techniques Article Upgrading Feldspar by WHIMS and Flotation Techniques Somsak Saisinchai a, *, Thitisak Boonpramote b, and Pinyo Meechumna c Department of Mining and Petroleum Engineering, Faculty of Engineering,

More information

Minerals II: Physical Properties and Crystal Forms. From:

Minerals II: Physical Properties and Crystal Forms. From: Minerals II: Physical Properties and Crystal Forms From: http://webmineral.com/data/rhodochrosite.shtml The Physical Properties of Minerals Color Streak Luster Hardness External Crystal Form Cleavage The

More information

OCEAN/ESS 410. Lab 8. Igneous rocks

OCEAN/ESS 410. Lab 8. Igneous rocks Lab 8. Igneous rocks Today s exercise is an introduction to rock identification and the crustal structure of the seafloor. All rocks are composed of two or more minerals, and can be classified based on

More information

O and Si make up % of all atoms available to make minerals in the Earth's crust.

O and Si make up % of all atoms available to make minerals in the Earth's crust. 7. Minerals III (p. 87-97) Mineral Families O and Si make up % of all atoms available to make minerals in the Earth's crust. Minerals in which cations combine with O 2- anions are called. If Si gets added,

More information