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Minerals. Chapter 2. Mineral: a naturally occurring substance formed in the Earth. Inorganic Solid substance Definite chemical composition. How Minerals Form. 1. Crystallization from magma . 2. Precipitation. 3. Pressure and temperature. 4. Hydrothermal solutions.
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Minerals Chapter 2
Mineral: a naturally occurring substance formed in the Earth • Inorganic • Solid substance • Definite chemical composition
How Minerals Form 1. Crystallization from magma 2. Precipitation 3.Pressure and temperature 4. Hydrothermal solutions
Mineral Groups • Can be classified based on their composition 1. Silicates • Silicon and oxygen combine to form a structure called the silicon-oxygen tetrahedron. 2. Carbonates • Minerals that contain the elements carbon, oxygen, and one or more other metallic elements 3. Oxides • Minerals that contain oxygen and one or more other elements, which are usually metals
Mineral Groups 4. Sulfates and Sulfides • Minerals that contain the element sulfur 5. Halides • Minerals that contain a halogen ion plus one or more other elements 6. Native elements • Minerals that exist in relatively pure form
Identifying Minerals: 1. Color • Most easily observed property • Yet, least useful property
Identifying Minerals:ColorWhy it is the least useful property… • Different minerals have the same color • One mineral can have different colors • Impurities can alter color • Some change color when exposed to air • Light can distort color
Identifying Minerals: 2. Luster • Way a mineral shines
Identifying Minerals: Luster Metallic: shines like polished metal Pyrite “Fool’s Gold”
Identifying Minerals: Luster Nonmetallic: does not shine like metal
Identifying Minerals: Luster Pearly like a pearl Talc
Identifying Minerals: Luster Greasy Turquoise
Identifying Minerals: Luster Vitreous like shining glass Amethyst
Identifying Minerals: Luster Resinous like wax
Identifying Minerals: Luster Dull or Earthy Bauxite
Identifying Minerals: 3. Crystal Shape • The shape of a crystal results from the way the atoms of a mineral come together as the mineral forms
Identifying Minerals: 4. Streak Test • Color of a mineral’s powder form • Usually, streak is not the same color as the mineral • Streak doesn’t vary
Identifying Minerals: Streak Test • Metallic mineral has dark streak • Nonmetallic – colorless or light streak
Identifying Minerals: 5. Cleavage • The splitting of a mineral along certain flat surfaces • Related to the types of bonds in the internal structure of the mineral
Identifying Minerals: 6. Fracture • the way a mineral tends to break –unevenly!!!
Identifying Minerals: Fracture Splintery jagged
Identifying Minerals: 7. Hardness • Resistance to being scratched • Moh’s hardness scale
Mohs Scale, identified numerically by standard minerals, from 1 (softest) to 10 (hardest): 1. Talc 2. Gypsum 3. Calcite 4. Fluorite 5. Apatite 6. Orthoclase 7. Quartz 8. Topaz 9. Corundum 10. Diamond
To remember the Mohs scale try remembering this phrase: The Geologist Can Find An Ordinary Quartz, (that) TouristsCall Diamond!
Tools for Testing Hardness • You typically do not carry around a supply of the 10 minerals on the hardness scale. However, you can use the following items to help estimate the hardness of a mineral:
Tools for Testing Hardness • finger nail (H = 2.5) • penny (H = 3.5) • common nail (H = 4.5) • glass plate (H = 5.5)
Identifying Minerals: Special Properties • Acid test http://www.westhamptonbeach.k12.ny.us/Teachers/Cohen/sciweb/earthscience/sedimentary/Mvc-327w.mpg
Identifying Minerals: Special Properties • Magnetic test
Identifying Minerals: Special Properties • Taste test Some minerals have a distinct taste. Never do this test after the acid test!
Common Rock-forming Minerals Quartz
Feldspar Mica
Talc Amphiboles
Galena Halite
Biotite Calcite
Hematite Pyrite
Magnitie Olivine