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Minerals

Minerals. Fracture. Fracture is the tendency of a mineral to break along curved surfaces without a definite shape. These minerals do not have planes of weakness and break irregularly. Cleavage.

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Minerals

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  1. Minerals

  2. Fracture • Fracture is the tendency of a mineral to break along curved surfaces without a definite shape. These minerals do not have planes of weakness and break irregularly

  3. Cleavage • Cleavage is the tendency of a mineral to break along smooth planes parallel to zones of weak bonding

  4. Adamantine - very gemmy crystals Dull - just a non-reflective surface of any kind Earthy - the look of dirt or dried mud Fibrous - the look of fibers Greasy - the look of grease Gumdrop - the look a sucked on hard candy Metallic - the look of metals Pearly - the look of a pearl Pitchy - the look of tar Resinous - the look of resins such as dried glue or chewing gum Silky - the look of silk, similar to fibrous but more compact Submetallic - a poor metallic luster, opaque but reflecting little light Vitreous - the most common luster, it simply means the look of glass Waxy - the look of wax Luster • Luster is a description of the way light interacts with the surface of a crystal. This is how you would tell someone how a mineral looks. It has nothing to do with color or shape, but is related to transparency , surface conditions, crystal habit and index of refraction. Vitreous Dull Resinous Adamantine Metallic Silky

  5. Streak • The streak of a mineral is the color it displays in finely powdered form. The streak maybe completely different from the color of the hand specimen. One of the simpliest ways of determining the strak of a mineral is to rub a specimen across a piece of unglazed porcelain known as a streak plate Magnetite – Black Streak Amphibole – grey/green streak Hematite – red/brown streak

  6. Hardness • HardnessMineralTest • 1 Talc Fingernail (2.5) • 2 Gypsum  • 3 Calcite Copper coin (3) • 4 Flourite Knife blade (5.5) • 5 Apatite Glass plate (5.5+) • 6 K-feldspar  • 7 Quartz Streak plate (7) • 8 Topaz  • 9 Corundum  • 10 Diamond 

  7. Vesiculartexture Glassy texture Texture • Minerals may be rough, like sand, others may be smooth or chalky. Run your fingers on the rock. What does it feel like. rough & crystalline texture Pegmatitic Texture – big grains

  8. Specific Gravity • Density or specific gravity is the ratio of the weight of a substance to the weight of an equal volume of water. • Density = Weight/Volume

  9. Crystal System • Crystal shape can be helpful in identification. Most minerals have a crystalline structure and can form perfect crystals if allowed to grow in an unrestricted space. Crystal faces resemble cleavage faces because they are flat and reflect light as a single plane, but they are different from cleavage surfaces because crystals have complex geometric shapes. Perfect crystals are rare and are seldom encountered.

  10. Crystal System 2 • CRYSTAL SYSTEM - AXES LENGTHS - AXIAL ANGLES • CUBIC All equal All 90 • TETRAGONAL a=b not = c all 90 • HEXAGONAL two are equal 2 are 90, one 120 • ORTHORHOMBIC all unequal all are 90 • MONOCLINIC all unequal two are 90 • TRICLINIC all unequal none are 90 Isometric Monoclinic Hexagonal Orthorhombic Triclinic Tetragonal

  11. Minerals have the same chemical composition but small variations of the quantity and distribution of some elements will give the same mineral different colors. Color Quartz Quartz Quartz Quartz Malachite Pyrite Olivine Limonite

  12. Mineral Silicate • Rock Luster • Crystal Streak • Gem Hardness • Ruby Moh’s Scale • Diamond Cleavage • Sapphire Fracture • Fossil Ore • Crystal System Texture • Specific Gravity Emerald

  13. Mini-Poster • Mineral Silicate • Luster • Crystal Streak • Gem Hardness • Moh’s Scale • Cleavage • Fracture • Fossil Ore • Crystal System Texture • Specific Gravity

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