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Published byDonald McBride Modified over 9 years ago
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Ch. 4: Minerals
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Earth’s crust is composed of about 3000 minerals!
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Minerals Help form rocks Shape earth’s surface Shape our civilization Mineral: naturally occurring inorganic solid with specific chemical composition and definite crystalline structure
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Salt vs. Sugar
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Crystal Solid in which atoms are arranged in repeating patterns
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Identifying Minerals Color: least reliable Luster: the way it reflects light –Metallic, shiny or non-metallic, dull, or pearly.. Texture: how does it feel? –Smooth, soapy, rough, greasy
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Streak: color of a mineral when it’s broken up and powdered –Very consistent, only useable on softer minerals Hardness: how easily it can be scratched –Friedrich Moh’s scale –Very reliable
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http://geology.com/rocks/
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Density –How tightly compacted a substance’s molecules are D = m/v –Less dense than liquid: floats –More dense than liquid: sinks
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Special properties Calcite bends light, gives a double image Magnetite: a natural magnet
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Mineral uses Ore: a mineral is an ore if it… –contains a useful substance AND –can be mined for a profit
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Gem – valuable mineral prized for beauty and rarity
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Find the answers in ch. 4 What mineral forms rubies and sapphires? What’s the difference between them? Which is more valuable – a diamond or emerald? Why?
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Matter: anything that has volume and mass –Made of elements Elements: substance that connot be broken down into smaller substances by physical or chemical means –Purely and completely ______________
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Elements 92 naturally occuring elements on earth or in stars Hydrogen and Helium are the most abundant elements in the universe! Why?
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Elements that are also minerals: Copper Silver Sulfur Most minerals are compounds
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In Earth’s crust… Silicon and oxygen are the most abundant
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In the atmosphere: 78% nitrogen 21% oxygen 1% ozone, water vapor
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In the oceans: What do you think? Sodium Chloride Hydrogen Oxygen Why? 97% of all water on earth is salt water!
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Back to Earth’s crust… Continental crust: granite Oceanic crust: basalt –More dense
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