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Minerals CH 2 Prentice Hall p. 47-54 CH 2 Prentice Hall p. 47-54
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What is a Mineral? A naturally occurring, inorganic solid that has a crystal structure and definite chemical composition. – Over 3,000 – 20 minerals form Earth’s crust. Rock forming minerals.
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Naturally Occurring Must form through Earth’s processes. – Cement, Brick, Steel and Glass all come from substances in Earth’s crust. – But they are manufactured by people.
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Cannot come from materials that were once part of living things. – Coal- forms naturally, comes from the remains of plants and animals. Inorganic
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Always solid, with a definite volume and shape. – Particles can’t flow freely. Solid
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Crystal Structure Particles of a mineral line up in a repeating pattern. Forms a solid called a crystal. – Has flat sides called faces, that meet at sharp edges and corners.
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A mineral always contains certain elements in definite proportions. Element- a substance composed of a single kind of atom. – All atoms have the same chemical and physical properties. Definite Chemical Composition
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Compound- Two or more elements combined. – Most minerals are compounds. – Chemically joined. Definite Chemical Composition
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Mixture- consists of two or more substances that are mixed together but not chemically combined.
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Crystal Structure Each mineral grows atom to atom to form that mineral’s particular structure. – Classified into six groups (crystal systems) based on the number and angle of the crystal faces. Identifying Minerals
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Identifying MineralsCrystal SystemsCleavageCleavage/FractureFractureSpecial PropertiesDensityHardnessColorStreakLuster
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Color 1. Color is an easily observed physical property. Not the best property to use to identify because many minerals like quartz can come in a variety of colors. Identifying Minerals
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Streak Streak is the color of the minerals powder when it is rubbed against a Streak Plate – This property does not vary like the color of the mineral can. Identifying Minerals
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Luster Metallic luster- looks like a metal. Non-Metallic Luster- does not look like a metal, can be glassy, dull, earthy, waxy and pearly. Luster is used to describe how a mineral reflects light from its surface. Identifying Minerals
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Crystal Structure Each mineral grows atom to atom to form that mineral’s particular structure. – Classified into six groups (crystal systems) based on the number and angle of the crystal faces. Identifying Minerals
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Crystal Structure Particles of a mineral line up in a repeating pattern. Forms a solid called a crystal. – Has flat sides called faces, that meet at sharp edges and corners.
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5. Cleavage Cleavage- is a mineral that easily splits along flat surfaces. Identifying Minerals
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6 Fracture Fracture- describes how a mineral looks when it breaks apart in an irregular way. Identifying Minerals
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Special Properties Fluorescence- glows under UV (ultraviolet light) Fluorescence Magnetic- acts like a magnet Radioactive- give off radiation- Uraninite Reacts to Acid- reacts by fizzing. Electrical Properties- electric current can be produced (Quartz) – Used in watches Identifying Minerals
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The resistance to being scratched. One of the best clues. Mohs hardness scale. – A scale from 1 to 10. Hardness Identifying Minerals
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s s Mohs Hardness Scale see p150 to label boxes with minerals 10. Other Hardness’s 7.8.9. Can scratch steel and hard glass easily. Can scratch quartz.Can scratch topaz. 4.5.6. A steel nail can easily scratch it. A steel nail can scratch it.Cannot be scratched by a steel nail, but it can scratch window glass. 1.2.3. Softest known mineral. It flakes when scratched by a fingernail. A fingernail can easily scratch it. A fingernail cannot scratch it, but a copper penny can. Hardest known mineral, Diamond can scratch all other surfaces. Identifying Minerals
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It is the mass in a given volume. It always remains the same for any given mineral. Density Identifying Minerals
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A balance would be used to measure the mass of a sample. The sample can be placed in a graduated cylinder to determine the volume. Density Identifying Minerals
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Water Displacement (how much water is moved, is equal to the volume of the sample) is used to determine the volume of the sample Density Identifying Minerals
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