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Unit 2 Chapter 5 Minerals of Earth's Crust
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Minerals: Are naturally occurring, inorganic solid that has a definite chemical composition with the atoms arranged in an orderly pattern. Characteristics of Minerals There are 4 characteristics that the object must fit into Is it organic? Does it occur naturally? Is it a crystalline solid? Does it have a definite chemical composition?
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Kinds of Minerals There are approximately 4000 known minerals Approximately 20 of the minerals are called rock forming and approximately 90% makes up the earth's crust. 90% of the minerals are a combination of the common elements. The rest of the minerals are rare or in rare quantities.
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Silicate Minerals Silicate A mineral that contains a combination of silicon and oxygen. Most common minerals that make up approx 95% of the earth's crust Common ones include: quartz and the feldspars (rocksandminerals4u) Non Silicate Minerals Carbonates Contain carbon Halides Chlorine, fluorine combined with sodium, potassium or calcium Native Elements Composed of a single element Gold - Au Silver - Ag Sulfur -S Diamond - C Oxides Contain Oxygen and other elements Sulfates Contain sulfate (SO 4 ) and other elements Sulfides Contain Sulfur and other elements
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Crystalline Structure Crystal: Atoms that are arranged in a regular repeating pattern. Can be seen with your eye, microscope or x- ray
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Crystalline Structure of Silicate Minerals Silicon-Oxygen Tetrahedron Basic building block of rocks in the earth's crust 4 Oxygen 1 Silicon Hint - know this name and this shape it may come up again!!!! Hornblende -Silicon Tetrahedrons form the shape of a chain. -Oxygen will bond with Si to form a bumpy thing Mica -Si tetrahedrons form a flat sheet Pyroxene- Si tetrahedrons form a chain
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Section 2 Identifying Minerals Mineralogy The study of minerals Mineralogist The scientist who studies minerals
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Physical properties of Minerals: Color - Easy to determine but not too good because many minerals have the same color Also many minerals may have more than one color. Reasons:1.impurities may change color 2.Air may change color 3.Many different minerals may have the same color
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Streak Test By using an unglazed white tile and rubbing the mineral over the tile it can produce a powder. Each mineral's streak is always the same color no matter what the color of the mineral is.
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Luster Metallic - looks and shines like a metal Non metallic - can be shiny but does not look like a metal
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Cleavage and Fracture Cleavage The tendency of a mineral to split easily or separate along flat surfaces. Ex. Mica - one directional perfect cleavage Fracture - The mineral breaks along a surface that is not a cleavage surface. 1c. Conchoidal -shell like fracture Ex. Obsidian 2c. Fibrous -splintery - produces jagged, sharp edges Ex. Copper 3c. Uneven or irregular - generally rough surfaces
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Hardness - It is the resistance to being scratched. If a mineral scratches another mineral it is harder than the other mineral. Moh's Hardness Scale Uses objects easily found with earlier geologists. 1.Finger Nails 2.Copper penny (prior to ~1975) 3.Steel (knife) 4.Glass (watch or glasses)
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The scale Mohs (mineralogist, 1773-1839) scale is used mostly. Rosiwal shows cutting strength and Vickers shows denting strength.
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Crystal It is a shape only easily observed with large crystals.
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Density Ratio of mass of a substance to the volume of the substance Density = Mass Volume Specific Gravity: Simple definition: The objects weight in air verses its weight in water (compares densities)
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Special Properties Fluorescence -the ability to glow under Ultra violet light Phosphorescence -the ability to glow after lights are turned off Double Refraction - 2 images can be seen through the mineral Ex. Calcite Magnetism -minerals can be picked up or is attracted to a magnet. Ex. Magnetite Radioactivity -the ability to release energy and activate a Geiger counter Ex. Uranium
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Another way to determine a mineral Acid Test: Weak acids can cause calcite to fizz (bubble) like putting water on an "Alka Seltzer" tablet.
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