Monday November 02, 2009 Open your notebooks. Write down today’s questions. Today’s Theme: What is a mineral? – What are the ways that minerals can be identified? – What defines whether something is a mineral or not? – What is a crystal? – What is the difference between a rock and a mineral? Hand in any late work Progress Reports Tomorrow (Due Thursday) Science Fair Complete Write Up Due Friday!!!!!!!!! OMG Minerals Today: Use your keen powers of observation to make a list in your notebook of all of the physical properties you notice about the six samples. Think about these questions: – Are they all minerals? – Why do they look the way they do? – How did they form? – What are they composed of? – Where did they come from? Thursday November 05, 2009 Please write today’s lesson and date written in your notebook. – Today’s lesson: Properties of Minerals • What are the physical properties of minerals? • How do we tell minerals apart? New Red Books Open to Page 70 Please do not touch equipment yet!!!! Progress Reports Due TODAY (signed by parent) Science Fair Complete Write Up is due Tomorrow. Properties of Minerals Learning Objectives – What are the ways that minerals can be identified? – What is Moh’s Hardness Scale? – What is the difference between cleavage and fracture? – What are some common uses for minerals? What is a mineral? A mineral is – – – – Naturally Occurring (made by earth-not man made), Inorganic (never was alive), Solid (atoms in fixed position, definite volume/shape), with a definite crystal structure (repeating pattern of minerals atoms), – and a definite chemical composition (same elements throughout in a certain proportion) Which of these are minerals? AMBER COAL MICA PEARL SUGAR QUARTZ HALITE Salesite Gold Fluorite Tiptopite (clear) & Montgomeryite Acanthite Asbestos Gypsum Pyrite Feldspar Physical Properties of Minerals These properties are used to identify minerals 1. Color Color is the most noticeable physical property of a mineral but is THE LEAST reliable. This is because the same mineral can come in many colors. Example: Mineral Identification Color is one physical property that can be used to identify minerals but beware…… rhodochrosite malachite azurite turquoise The many colors of Calcite The many colors of Quartz Streak: The color of the powdered form of a mineral when rubbed on an unglazed porcelain plate Streak The mineral is rubbed on an unglazed porcelain plate to determine the color of the streak powder. Not all minerals have a streak. Any mineral harder than the plate (7+) will leave a scratch instead. Streak Example: Same Mineral! 3. Luster Luster describes how light is reflected from a mineral’s surface. A mineral has either – Metallic Luster (shines like a metal) or – Non-Metallic Luster. • Dull, earthy, waxy, greasy, pearly, silky or vitreous (glassy) Luster: The mineral Galena has a metallic luster Examples of Luster Metallic Luster Non-Metallic Luster Metallic or Nonmetallic? Metallic or Nonmetallic? Metallic or Nonmetallic? Density Density is the comparison of mass to volume. – It’s really how well packed are the atoms in the object. Mass divided by volume 5. Hardness Hardness is a measure of how easily a mineral is scratched. – determined by arrangement of the mineral’s atoms. Mohs Hardness Scale: a relative scale used to determine the mineral’s hardness 5.5 2.5 Fingernail 3.5 Penny 4.5 Iron Nail 6.5 Glass Streak Plate Crystal Systems The way the mineral grows atom by atom makes a shape we call a crystal. – Most of the time you can’t see them. – More time and space it had to grow = bigger crystals Crystal Forms These are Quartz Crystals These are Quartz Crystals Texture Texture describes how a mineral feels to the touch. Texture can be described as greasy, soapy, glassy, rough, ragged or smooth. Graphite has a greasy texture. Cleavage or Fracture Cleavage - When Minerals break along planes (layers) where bonding between atoms is weak. A mineral that splits or breaks easily along smooth, flat surfaces is said to have cleavage. •Mica has perfect cleavage in one direction (plane). •Halite has cubic cleavage (3 planes). Three Examples of Perfect Cleavage – Fluorite, Halite & Calcite Cleavage of Minerals Cleavage Cleavage or Fracture Minerals that break along rough, jagged or uneven edges and surfaces are said to have fracture. – conchoidal (shell-like), splintery, uneven, jagged or earthy Conchoidal Example : Quartz Don’t be confused between Crystal Faces (sides) and Cleavage Planes! - Both minerals in these pictures show Fracture (not cleavage) These are Quartz Crystals These are Quartz Crystals Special Properties Specific gravity Reaction to acid Striations (lines) Magnetism Fluorescence Uses of Minerals Gems or Gemstones are highly prized minerals because they are rare and beautiful. An Ore is a mineral that contains a useful substance that can be mined at a profit. Ore Name Gives Us Hematite Iron Chalcopyrite Copper Bauxite Aluminum Sphalerite Zinc Uses of Minerals Gems: Valuable minerals prized for rarity and beauty. Ores: Minerals that can be mined at a profit. Uses of Minerals http://www.minsocam.org/MSA/K12/uses/uses.html http://www.emporia.edu/earthsci/amber/go336/talkingt/ The Copper Queen Mine in Bisbee, AZ An Underground Halite Mine Birthstones January February March April May June July August September October November December Garnet or Rose Quartz Amethyst or Onyx Aquamarine or Bloodstone Diamond or Quartz Crystal Emerald or Crysoprase Alexandrite or Moonstone or Pearl Ruby or Carnelian Peridot or Sardonyx Sapphire or Lapis Opal or Tourmaline Topaz or Citrine Tanzanite, Zircon or Turquoise History of Birthstones In early times, gemstones were believed to possess magical properties. Some minerals were thought to contain a force or hold certain values and powers. Tradition associates a gem with each sign of the zodiac based on a color system. Color was thought to unleash the power attributed to the stone. The Roman, Arabic, Jewish, Polish, Russian and Italian birthstone lists were all different. In time, birthstones became associated with calendar months rather than the zodiac. And people began to select birthstones in colors other than the original. This list of birthstones, which is the one commonly used today, was adopted in 1912 by the American National Association of Jewelers, which later evolved into the Jewelers of America. Mineral Compositions and Groups Minerals are grouped based on their chemical composition (the elements that make up the minerals). Almost 98% of the Earth’s crust is made of only 8 common elements (O, Si, Al, Fe, Ca, Na, K, Mg). Mineral Compositions and Groups Silicon (Si) and Oxygen (O) are the most common elements in the Earth’s crust. Major groups are….(In order of size) • • • • • • • • • Silicates (Si, O) (Largest rock forming group) Carbonates (CO3) Oxides (O3, O4) Sulfides (SO4) Sulfates (SO3) Halides (F, Cl, I, Br) Hydroxides (OH)2 Phosphates (PO3) Native Elements (Au, Ag, Cu) Mineral Compositions and Groups Examples of Silicates Hornblende Examples of Silicates Orthoclase Feldspar Examples of Silicates Plagioclase Feldspar Carbonates Sulfates Halides Native Element Copper