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         Minerals & Crystals Geology:     more books (35)
  1. The Practical Study of Crystals, Minerals, and Rocks (McGraw-Hill European Geography and Geology Series) by K.G. Cox, N.B. Price, et all 1967
  2. Dig Into Rocks, Minerals & Crystals
  3. Crystals (Geology Rocks!/ Freestyle Express) by Rebecca Faulkner, 2008-01-15
  4. The Practical Study of Crystals, Minerals and Rocks by Keith Gordon Cox, 1988-08-01
  5. Crystals (Rocks & Minerals) by Melissa Stewart, 2002-08-27
  6. Crystal Habits of Minerals (Bulgarian Academic Monographs, 1) by Ivan Kostov, Ruslan I. Kostov, 1999-06
  7. Minerals: An entry from Thomson Gale's <i>Gale Encyclopedia of Science, 3rd ed.</i> by Sara G. B. Fishman, 2004
  8. ROCKS: An entry from Thomson Gale's <i>Science of Everyday Things</i>
  9. Crystals and Minerals, Volume III (A Family Field Collecting Guide for Northwestern Oregon and Southwestern Washington) by Jon Gladwell, 1994
  10. Crystals and Minerals, Volume II (A Family Field Collecting Guide for Northwestern Oregon and Southwestern Washington) by Jon Gladwell, 1991
  11. The world of crystals, minerals, and rocks (Individualized science activity cards) by Robert G Hoehn, 1976
  12. Geology, mineralogy, and crystallography: being a theoretical, practical, and descriptive view of inorganic nature: The form and classification of crystals, and a chemical arrangement of minerals, by D. T Ansted, 1855
  13. Mineralogy and crystal-chemistry of clay minerals related to diagenesis and very low-grade metamorphism of two Proterozoic sedimentary sequences from Sweden (UUDMP research report) by Sadoon Morad, 1982
  14. My Best Book of Fossils, Rocks and Minerals (My Best Book Of...) by Chris Pellant, 2002-02-18

81. Rockhounding Arkansas, Table Of Contents
An authoritative, comprehensive reference for Arkansas minerals and the hobby Collecting crystals, the Guide to Quartz in Arkansas is available from A I
http://rockhoundingar.com/contents.html
Rocks and minerals, quartz crystals, diamonds;
rockhounding in Arkansas offers many opportunities Helpful
beginners tip:
Bookmark this
page! You'll
want to come
back and read
more
Meet our geologist
in residence:
Mike Howard HEIGHT="31" WIDTH="88" NATURALSIZEFLAG="0" ALIGN="BOTTOM" ALT="Webtracker"> Arkansas
Weather
Read more about rockhounding with books from If you are a beginner or an accomplished mineralogist, you'll want to read through the stories and information presented here for the enjoyment of this fascinating hobby. Rockhounding Arkansas is presented by Mike and Darcy Howard, for your information and enjoyment of mineral collecting. Mike has authored numerous articles and publications for collectors as well as for the scientific community. The companion book to our website. Collecting Crystals, the Guide to Quartz in Arkansas Chapter 1. This chapter is one of the most comprehensive and authoritative references you will find on quartz, from Arkansas or otherwise. Quartz is Arkansas' most famous mineral. Known around the world, your collection is not complete without an Arkansas Quartz crystal. Chapter 2.

82. Igneous Rocks - Basic Course In Geology
Since rocks mixtures of minerals, they behave somewhat differently. The processes is called magmatic differentiation by crystal fractionation.
http://www.earthsci.org/teacher/basicgeol/igneous/igneous.html
Magmas, Igneous Rocks, Volcanoes, and Plutons Earth Science Australia...
Contents of Entire Course of "The Earth and Beyond

Kinds of Igneous Rock

Types of Magma
...
Plutons
adapted to HTML from lecture notes of Prof. Stephen A. Nelson Tulane University
Kinds of Igneous Rock

top...
Igneous Rocks are formed by crystallization from a liquid, or magma. They include two types
  • Volcanic or extrusive igneous rocks wherein the magma cools and crystallizes on the surface of the Earth
    Intrusive or plutonic igneous rocks wherein the magma crystallizes at depth in the Earth.
  • Magma is a mixture of liquid rock, crystals, and gas. Characterized by a wide range of chemical compositions, with high temperature, and properties of a liquid. Magmas are less dense than surrounding rocks, and will therefore move upward. If magma makes it to the surface it will erupt and later crystallize to form an extrusive or volcanic rock . If it crystallizes before it reaches the surface it will form an igneous rock at depth called a plutonic or intrusive igneous rock . Because cooling of the magma takes place at a different rate, the crystals that form and their interrelationship (texture) exhibit different properties.

    83. Geology Basics: Rocks And Minerals, Plate Techtonics, Climate History
    geology Basics Rocks and minerals, Plate Tectonics, Climate History, Surface Water Because crystal structures are unique to a mineral, a mineral can be
    http://www.acad.carleton.edu/curricular/GEOL/classes/geo120/geology_basics.htm
    Geology Basics: Rocks and Minerals Plate Tectonics Climate History Surface Water and Groundwater This page is meant to serve as a preliminary source of information for geology concepts not covered in your textbook. For more complete explanations, the geology textbook Understanding the Earth by Frank Press and Raymond Siever is on closed reserve. The following information is adapted from that text. In addition, there are CD-ROMs which take you through all of the concepts and have animated demonstrations.
    Rocks and Minerals:
    Minerals –
    A mineral is a naturally occurring, solid crystalline substance, generally inorganic, with a specific chemical composition. (26) In a mineral, the constituent atoms are bonded together in a specific, ordered lattice. The way in which a combination of atoms bonds depends on the atomic properties of each element. Different minerals are classified based on a combination of their chemical composition and their crystal structure. Follow this link for more information on the chemical properties of minerals . Because crystal structures are unique to a mineral, a mineral can be identified by the shape of its faces and by its cleavage, or the planes along which it tends to break. This link has information about all the

    84. Geological Sciences 101
    Other constraints on the combination of atoms to form minerals are the size Cooling rate affects crystal size, thus the fastcooling volcanic rocks are
    http://www.geo.cornell.edu/geology/classes/Geo101/101week8_f01.html
    Introduction to Geological Sciences
    Week 8
    In Class
    In Lab
    Links to good stuff...
    Review
    Rocks and Minerals
    Most rocks are made up of silicate mineralsin fact, with the exception of limestonevirtually all rocks are silicates. The basic building block of the silicate structure is the silicate tetrahedrona pyramid-shaped unit with one Si at the center surrounded by four oxygen atoms. These tetrahedra link together and combine with additional elements such as Fe, Al, Ca etc. to form the different silicate minerals. The important silicate mineral groups are organized into a scheme called Bowen's Reaction Series. BRS indicates the order in which minerals would crystallize out of a basaltic magma, and shows that (for the most part) the early-forming, high-temperature minerals are those with simple structures, while the latest-forming, lowest-temperature minerals have the most complicated structures. Minerals that occur near each other on BRS also occur together in igneous rocks. Minerals high on BRS are called mafic and so are the rocks that they form. Mid-level minerals are intermediate; the lowest minerals are felsic and form the felsic igneous rocks.

    85. Sedimentary, Metamorphic, Igneous Rock Types [Athro, Limited: Geology]
    When a magma cools rapidly, mineral crystals do not have time to grow very large. When a magma cools slowly crystals grow to several millimeters or more in
    http://www.athro.com/earth_science/rocks.html
    Athro, Limited Earth Science Rock Types The major Rock Types and how they form
    Igneous Rocks
    Igneous rocks solidify from a liquid magma as it cools. They are described on two axies: 1) Rocks that are quartz rich ( felsic ) to magnesium rich ( mafic ) and 2) fast cooling (small crystals) to slow cooling (large crystals). When a magma cools rapidly, mineral crystals do not have time to grow very large. When a magma cools slowly crystals grow to several millimeters or more in size. Granite and basalt are opposites on these axies for the description of igneous rocks - granite is a slow cooled quartz rich rock, basalt a rapidly cooled mafic rock.
    Basaltic lava flow, Idaho
    Basalt is the stuff of the ocean floor. It comes from fresh upwellings from the mantle. Basalts are extrusive igneous rocks rich in minerals containing magnesium and other similar metallic atoms. Most of these minerals have a dark color. Basalts are thus dark in color. Basalt cools rapidly as volcanic eruptions dump magma out into the air, water or inject it in little intrusions into cold rocks, crystals never have chance to grow large. A magma with at basaltic composition that cooled slowly and had a chance to grow large mineral crystals would form an intrusive igneous rock that we would call a gabbro.

    86. Physical Geology Notes
    University of Colorado geology 1010 The basic repeat unit of a crystal or mineral is the unit cell. crystals have complex symmetries.
    http://ruby.colorado.edu/~smyth/G101-3.html
    University of Colorado GEOLOGY 1010 Class Note 3
    Minerals and Rocks
    A mineral is a naturally occurring homogeneous solid of definite chemical composition and ordered atomic arrangement. It is usually formed by inorganic processes. More than 5000 mineral species have been described and more than 100 new minerals are described every year. To describe a new mineral, the structure and composition must be described. Most of these 5000 minerals are rare, so that only about 200 are common enough to make up macroscopic rocks. Of these, the most abundant 50 make up 99.9% of the Earth's crust. Some examples of minerals that are familiar to you are quartz (SiO , silicon dioxide), calcite (CaCO calcium carbonate), pyrite (FeS , iron sulfide), gypsum (CaSO . 2 H O), gold (Au), silver (Ag), copper (Cu), diamond (C), graphite (C), garnet (Mg Al Si O ice (H O). Less familiar, perhaps, are apatite (Ca (PO OH) (teeth and bone), olivine (Mg SiO ) (the green mineral that makes up much of the upper mantle, gem variety: peridot), pyroxene (MgSiO ) (the other mineral in the upper mantle), muscovite (white)

    87. Memphis Archaeological And Geological Society‚MAGS Newsletter Index Of Feature
    RockNews0103 crystals Zeolite Crystal Growth in Space RockNews0105 Diamonds Crater of Diamonds MAGS0502 minerals Crater of Diamonds State Park, AR
    http://www.memphisgeology.org/newsletter_index.html
    The Club The Show Newsletter Youth Newsletter ... Email In order to view the MAGS Newsletter online, you must have Adobe Acrobat Reader software installed on your computer. If you do not have Reader, it is available as a free download from Adobe. Click the icon below to download reader. MAGS Rockhound News Index of Feature Articles Agates: Agate Days and Agate Ways
    Archaeology: 1200-Year-Old Village Found
    Archaeology: 5,300 Year Old Man
    Archaeology: Artifacts from the Pyramid of the Moon
    Archaeology: Clovis Points
    Archaeology: History in a Pot
    Archaeology: Napoleon's Lost Army
    Archaeology: NASA Deep Space 1 Probe
    Archaeology: Projectile Points of West Tennessee
    Archaeology: Pyramid of the Moon
    Archaeology: Sinking of the Sultana Archaeology: X-ray technology used to read inscriptions Archives: Fulton Mounds (October 1955 MAGS Article) Astronomy: The Night Sky in August

    88. Oxford Brookes University - Geology - Atlas Of Ore Minerals - Gangue
    gangue minerals can not easily be identified in reflected light microscopy Colour colourlesswhite; Streak white; Lustre vitreous; Crystal form
    http://www.brookes.ac.uk/geology/8361/1999/tracey/gangue.htm
    ATLAS OF COMMON ORE MINERALS
    Introduction
    Copper Minerals Lead Minerals Zinc Minerals ... Other Metallic Minerals Gangue Minerals Quiz
    Gangue Minerals The uses for these minerals are stated before the mineral characteristics Anhydrite/Gypsum Barite Calcite Fluorite ... Quartz gangue minerals can not easily be identified in reflected light microscopy and are better seen in transmitted light microscopy Anhydrite CaSO Gypsum CaSO O
    used in the construction industry
    • Colour : colourless, white-pink-brown Streak : white Lustre : pearly-vitreous Crystal form : massive, rose, prismatic, tabular Crystal system : monoclinic Crystal hardness Cleavage : perfect Fracture : conchoidal-fibrous Feel : smooth Associated minerals : sulphur, halite, aragonite, celestine
    Barite BaSO
    used in white paint, as a protection against x-rays and as a drilling mud
    • Colour : colourless, white, pink-brown Streak : white Lustre : pearly Crystal form : acicular-tabular Crystal system : orthorhombic Crystal hardness Cleavage : perfect Fracture : conchoidal-uneven,splintery Feel : smooth Associated minerals : calcite, fluorite, quartz, ore minerals

    89. Oxford Brookes University - Geology - Atlas Of Ore Minerals - Iron
    Iron minerals are used in the construction industry and for alloying Colour silver grey; Streak black; Lustre metallic; Crystal form
    http://www.brookes.ac.uk/geology/8361/1999/tracey/iron.htm
    ATLAS OF COMMON ORE MINERALS
    Introduction
    Copper Minerals Lead Minerals Zinc Minerals Iron Minerals Other Metallic Minerals Gangue Minerals Quiz
    Iron Minerals Iron minerals are used in the construction industry and for alloying Arsenopyrite Hematite Magnetite Pyrite ... Pyrrhotite
    Arsenopyite FeAsS
    • Colour : silver grey Streak : black Lustre : metallic Crystal form : massive-acicular Crystal system : orthorhombic Crystal hardness Cleavage : parallel to faces of prism Fracture : uneven Smell : similar to garlic on freshly broken surfaces Associated minerals : stibnite, galena, pyrite Colour : white-light grey Birefringence/pleochroism : weak-yellowish XPL anisotropy : moderate-strong Internal reflections : none Textures : zoning Reflectivity : moderate Hardness : very hard
    Hematite Fe O
    • Colour : black with red tinge Streak : red-brown Lustre : metallic-dull Crystal form : reniform-massive-tabular-rose Crystal system : trigonal Crystal hardness Cleavage : none Fracture : conchoidal Associated minerals : siderite, limonite, magnetite, pyrite, quartz Colour : grey-white Birefringence/pleochroism : weak XPL anisotropy : distinct Internal reflections : deep red Textures : lamellar Reflectivity : low Hardness : very hard
    Magnetite Fe O
    • Colour : dark grey-black Streak : black Lustre : metallic-dull Crystal form : tabular-massive Crystal system : cubic Crystal hardness Cleavage : imperfect Fracture : uneven Associated minerals : ilmenite, apatite, augite, hematite, amphiboles

    90. Maine Geology - May Site Of The Month
    Geologic Site of the Month May 1998. Mineral Collecting in Maine - 1998 Update Figure 3 shows one of the giant andalusite crystals that were found in
    http://www.state.me.us/doc/nrimc/mgs/sites-1998/may98.htm
    Skip Maine state header navigation Agencies Online Services Web Policies ... Help State Search:
    MAINE DEPARTMENT OF CONSERVATION
    Maine Geological Survey
    Geologic Site of the Month - May 1998
    Mineral Collecting in Maine - 1998 Update
    INTRODUCTION Mineral collecting ("rockhounding") continues to be a very popular hobby in Maine. This state is world famous for the gems and rare minerals that have been found here. Tourmaline, aquamarine beryl, garnet, and amethyst are among the more desirable minerals occurring in veins of coarse-grained granite called "pegmatite." Earlier in this century pegmatite rocks in Oxford, Androscoggin, and Sagadahoc Counties were extensively mined for feldspar and mica. Gem crystals with obvious value were usually saved during these operations, but other interesting minerals were thrown onto the "dumps" of waste rock. Collectors have dug through the dump piles ever since, finding specimens for their collections. Mineral collecting has many positive aspects. It is a low-cost hobby that is ideal for people who want to combine outdoor recreation with the fun of a treasure hunt. The arranging and study of a well-labeled mineral collection can also be an enjoyable and educational activity throughout the year. Some families plan their Maine vacations around a series of day trips to collecting sites. Gold panning is a special type of mineral pursuit that has its own dedicated followers. The East Branch of the Swift River in Byron is the most popular stream for gold seekers and has yielded some big nuggets (Figure 1), but many other Maine rivers probably contain traces of gold in their gravelly sediments.

    91. Northwest Geological Society : Calendar
    Far out fossils, minerals and crystals A family adventure; Alberta August 811 Geological Society of America AND Geological Association of
    http://www.scn.org/nwgs/joust/calendar.htm
    Menu Pacific Northwest Region GeoScience Calendar Please query links or contacts of non-NWGS events to confirm information before attending events. We are not notified of program changes or errors for some functions, and thus are not responsible for calendar inaccuracies related to non-NWGS listings. This web page is updated periodically. Contact: Dave Knoblach Location Key WA Washington, OR Oregon, BC British Columbia, ID Idaho, MT Montana, CA California, Other Other Locations (select functions only) Event Symbols Lecture: Field Trip: Conference: Recurring GeoScience Functions July, 2005 WA July 17- 23: Geological Society of AmericaField Forum Mt. St. Helens (For teachers)
    WA July 18 - 22: Northwest Natural Resources Institute Natural Resources Teacher Workshop OR July 23: Geological Society of the Oregon Country ): Pat Pringle (Washington Division of Geology and Earth Resources), Mt. St. Helens WA July 27 - 31: North Cascades Institute : Art Kruckeberg, Chris Morgan, Jon Riedel, and Rainer Stahlberg, North Cascades Naturalists Retreat: Glaciers, Rivers, Rare Plants and Wildlife

    92. Bob's Rock Shop: Books About Rocks And Minerals
    Hundreds of minerals are descrived, with details such as geologic distribution, Rocks, minerals, Gems, crystals, Fossils is a sure to be appreciated
    http://www.rockhounds.com/rockshop/books/minerals.shtml
    Bead Work
    Buyer's Guides

    Casting

    Chain Making
    ...
    Wire Work

    References for Rockhounds
    Rocks and Minerals Order This Book
    1000 Photos of Minerals and Fossils
    by Alain Eid

    Order This Book

    Amber Window to the Past by David A. Grimalsi The unique properties of amber (fossilized tree resin) have long intrigued many people and never more so than now, in the wake of Michael Chriton's fictional Jurassic Park and real scientific breakthroughs in achieving what Chriton theorized: the cloning of an ancient DNA sequence of amber. Originally published to accompany the hugely popular 1996 exhibition organized by the American Museum of Natural History in New York, Amber: Window to the Past explores thoroughly the various aspects of this remarkable material, from its part in delineating evolutionary history, through the study of folklore surrounding it, to is use in decorative arts and jewelry. The 230 gorgeous and amazingly varied photographs and drawings, 115 in color and never before published, vividly illuminate the roles of amber in both nature and art. This engrossing and readable book will delight lovers of science, history and art as well as anyone intrigued by stories of how we and our world have evolved. Soft cover, 9" x 11", 216 pages. Order This Book The Encyclopedia of Gemstones and Minerals by Martin Holden Lavishly illustrated with over 400 color photographs and illustrations

    93. Geology 111G/Lecture 3
    geology 111G/ 1/14/2005. Lecture 4. minerals. Definition. Properties A. Crystal structure is characteristic of a specific mineral.
    http://www.nmsu.edu/~geology/lawton/Lec4minerals.html
    Geology 111G/ Lecture 4. Minerals Definition Properties Rock-forming minerals Rocks I. Mineral Naturally occurring, solid crystalline substance, generally inorganic, with a specific chemical composition. A. Crystal structure is characteristic of a specific mineral. B. Chemical composition may vary within limits. C. Minerals form by crystallization , which is crystalline assembly of atoms in a gas or liquid. This may take place during cooling of a hot melt or by precipitation from a concentrated solution. II. Mineral properties Physical properties of minerals determined by internal arrangement of atoms, chemical formula and bond types. A. Crystal habit Shape of a crystal is determined by atomic structure. The atomic structure repeats itself throughout the mineral; this is the crystal lattice Crystal faces are the planar surfaces that develop during crystal growth. Cubic habit of halite (NaCl) is determined by the equally spaced disposition of sodium and chlorine ions in the crystal lattice. B. Polymorphs Different crystal structures with the same chemical composition. The classic example is carbon.

    94. PtyS/LPL Laserdisc Collection: Geology And Meteorology
    Mineral Properties Bowen s reaction series Crystal forms Crystal lattice diagrams minerals in thin section Hardness Cleavage Streak Luster Fracture Tenacity
    http://www.lpl.arizona.edu/resources/visuals/geology_disc.html
    Department of Planetary Sciences
    Lunar and Planetary Laboratory
    Resources
    Planetary Sciences Laserdisc Collection: Geology and Meteorology
    All Laserdiscs are stored in the podium. Please return after use and lock them up!
    Earth Science - Geology and Meteorology
    ODC Living Textbook Series
    (The catalog listing the still frames and movie clips is in the podium.)

    Introduction and Credits
    Side One/Side Two Directory
    Plate Tectonics
    Geologic Time Scale
    Diagrams
    Computer generated image of Earth topography
    Earth's Atmosphere
    Diagrams Cloud catalog Meteorology from space Ground weather Nimbus GOES weather patrol GOES views of Hurricane Allen Aurorae Ground observations Aurora Borealis Aurora Australis Mt. St. Helens USGS archives May 18, 1980 Ash cloud Hawaiian Volcanoes Hawaiin Volcanoes Nat'l Park HVO superset Volcanoes of the World North America Iceland International The African Rift Valley Yellowstone Nat'l Park Earthquakes Diagrams North American earthquakes Earthquake lights Glacial processes Glaciers Glacial erosion Glacial surfaces Glacial termini Moraines Glacial lakes Glacial outwash Glacial ice Ice rafting Icebergs Fluvial processes Weathering and erosion General fluvial processes Ripple marks Braided streams Meanders and oxbows Drainage patterns Flooding Falls Dams

    95. PSIgate - Physical Sciences Information Gateway Search/Browse Results
    The site also provides images of mostly uncommon minerals, and links to other Educational material Crystal Chemistry Lecture 5 geology 311 Earth
    http://www.psigate.ac.uk/roads/cgi-bin/psibrowse.pl?toplevel=earth&limit=0&subje

    96. UWRF Geology - Dr. Bill Cordua
    Why do pyrite crystals show different faces Moganite a common mineral Minnesota Twin crystals Moonstone - An exsolution to its mystery geology and
    http://www.uwrf.edu/~wc01/leaverite.html
    LEAVERITE NEWS ARTICLES
    BY
    WILLIAM S. CORDUA
    These are one-page popular science articles written on mineralogical and geological subjects for the Leaverite News newsletter of the St. Croix Rockhounds. They have been reprinted by other newsletters. Some have won regional and national awards through the Midwest Federation and American Federation. Copies of those not linked yet from this page can be obtained from me. E-MAIL ** indicates award-winning articles
    What are those fibers in my rose quartz?

    Pieces of eight minerals

    Cave spar

    Disorderly opal
    ...
    Floating Copper

    The Great St. Croix Meteorite Hunt 1997
    Wisconsin Wavellite

    **Minerals from Kidney Stones

    Agates - Full of Fiber

    Rust Minerals
    ... Mellen Black Granite A mineral from giant red suns A Lake Full of Lead Blue, Blue, My Quartz is Blue Why do pyrite crystals show different faces Moganite - a common mineral with a disapproved name Book review : Gene LaBerge, Geology of Lake Superior Epidote Hibbingite - swimming pool mineral A new place to look for diamonds Hourglass gypsum Wisconsin talc Geology and the Growth of Downtown Stillwater Moon minerals found on earth Moonmilk The fire of opal 1992 A St. Croix Meteorite

    97. BC Education - Geology 12 - Earth Materials (Minerals)
    geology 12 Earth Materials (minerals). This sub-organizer contains the Have students describe, sketch, or make models of simple crystal shapes (eg,
    http://www.bced.gov.bc.ca/irp/esg/12earmin.htm
    Geology 12 - Earth Materials (Minerals)
    This sub-organizer contains the following sections:
    Prescribed Learning Outcomes

    Suggested Instructional Strategies

    Suggested Assessment Strategies

    Recommended Learning Resources
    PRESCRIBED LEARNING OUTCOMES
    It is expected that students will:
    • outline the importance and abundance of various elements in the earth's crust
    • demonstrate an ability to use the following properties in identifying minerals:
      • simple crystal shape
      • cleavage
      • fracture
      • hardness
      • specific gravity (relative density)
      • colour
      • streak
      • lustre
      • special properties, such as reaction to dilute HCl
      • magnetism
    • use appropriate references and tests to describe and identify the following minerals: silicates and aluminosilicates:
      • quartz and varieties of quartz
      • potassium feldspar and plagioclase feldspar
      • muscovite, biotite, and talc
      • augite (pyroxene) and hornblende (amphibole)
      • garnet
      • asbestos
      • olivine
      oxides:
      • hematite, limonite, magnetite
      sulphides:
      • pyrite, chalcopyrite, galena, sphalerite, molybdenite, bornite
      carbonates and sulphates:
      • calcite, malachite, azurite, gypsum

    98. Gems Minerals Bibliography
    minerals, crystals, and Gems Stepping Stones to Inquiry The Care and Conservation of Geological Material minerals, Rocks, Meteorites, and Lunar Finds.
    http://www.calacademy.org/research/library/naturalist_center/biblio/gems.htm
    California Academy of Sciences Library World Wide Web Books Children's Books Video WORLD WIDE WEB Chemical Compositions of Minerals and Gems http://www.geology.wisc.edu/~jill/mineral.html It’s just like the title sounds. Desert Environment: Minerals and Geology Index http://www.desertusa.com/Thingstodo/geo/geology.html Click on a mineral to find more information. Gemology http://www.geocities.com/Y o semite/trails/3085/Gemmology.htm Links, links, and more links about gemology, the study of gems. Gems and Precious Stones http://www.geology.wisc.edu/~jill/306.html Many images and resources. GeoGem: Gemology Overview http://www.geogem.com/gemmology.htm Very useful information on the gemological properties of gem stones. The Image http://www.theimage.com/ Pictures of minerals and gemstones. The Mineral Gallery http://www.themineralgallery.com/ Descriptions, pictures and information on gemstones and minerals, by name, class, groupings and physical properties. Mineralogy Database http://www.webmineral.com/

    99. Glossary Of Selected Terms
    minerals not bounded by crystal faces. Metamorphism (geological)..Changes in rocks brought about by heat and pressure acting in the rocks just below the
    http://ist-socrates.berkeley.edu/~eps2/wisc/glossary.html
    Glossary of Selected Terms
    (An index is also available Absorption Spectrum ....Colors of light least absorbed combining to produce the color of the stone. The stone, when viewed by spectroscope, will show as dark bands in characteristic positions the colors most strongly absorbed.
    Acicular...Needlelike; refers to the growth of a mineral in long and slender crystals. Adamantine... Very high luster. Aggregate...Intergrowth of several crystals, these may be globular, fibrous, reniform, or radiating fibrous. Adularescence...The sheen of color seen in moonstone and other feldspars of the adularia variety. Allochromatic Minerals...Minerals that are colorless when pure, the color coming from coloring agents, most of which are, cobalt, copper, chromium, titanium, vanadium, manganese, and iron. Examples of this are beryl,corundum, quartz, and spinel.
    Alluvium...Continental sediments due to transport and deposition of gravel, sand, and clay by running water, rivers, and streams. (See alluvial
    Alpha rays...Helium atoms with double positive charge.

    100. Memphis Archaeological And Geological Society‚Lapidary Arts: The Color Of Cryst
    06.21.00The color of a crystal can be its most striking feature. The causes of color are varied, and many minerals occur in a range of colors.
    http://www.memphisgeology.org/l_color.html
    The Club The Show Newsletter Archaeology ... Email LAPIDARY ARTICLES Color of Crystals Sawing Gemstones A Visit to the Mineral and Lapidary Museum of Henderson County, NC The Color of Crystals Idiochromatic: Some minerals are nearly always the same color because certain light-absorbing atoms are an essential part of their crystal structure. These minerals are described as idiochromatic. For example, copper minerals are nearly always red, green or blue according to the nature of the copper present.: Allochromatic: A large number of minerals occur in a wide range of colors caused by impurities or light-absorbing defects in the atomic structure. For example, quartz, diamond, beryl, and corundum can be red, green, yellow, and blue. These minerals are described as allochromatic. Play of colors: The color os some minerals is really a play of colors like that seen in an oil slick or a soap bubble. This may be produced when the light is affected by the physical structure of the crystals, such as twinning or cleavage planes, or by the development duirng growth of thin films. Microscopic "intergrowths" of plate-like inclusions also interfere with the light.

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