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Minerals
What is a Mineral? ,[object Object],[object Object],[object Object],[object Object],[object Object]
Naturally Occurring ,[object Object],[object Object],[object Object],[object Object]
Inorganic ,[object Object],[object Object],[object Object]
Solid ,[object Object],- H 2 O as ice in a glacier is a mineral, but  water is not.
Definite Crystal Structure ,[object Object],Apatite Feldspar Diamond Quartz ,[object Object]
 
Definite Chemical Formula ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Types of minerals ,[object Object],[object Object]
Silicates ,[object Object],[object Object],[object Object],[object Object]
Feldspar ,[object Object],Feldspar ,[object Object]
Biotite Mica ,[object Object],[object Object]
Quartz ,[object Object],[object Object]
Nonsilicates ,[object Object],[object Object]
Classes of nonsilicates ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Native Elements ,[object Object],[object Object]
Carbonates ,[object Object],[object Object],[object Object]
Halides ,[object Object],[object Object],[object Object],[object Object],Fluorite
Oxides ,[object Object],[object Object],[object Object]
Sulfates ,[object Object],[object Object],[object Object],[object Object],Gypsum
Sulfides ,[object Object],[object Object],[object Object],Galena
Composition of the Earth’s Crust ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Where Do Minerals Come From? Magma Evaporation In general, minerals form in two ways: Cooling magma - Crystallization of melted materials From solution - Crystallization of materials dissolved in water At the surface Beneath the surface
Magma ,[object Object],[object Object],[object Object],[object Object]
Size of Crystals ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Minerals from Hot Water Solutions ,[object Object],[object Object],[object Object],[object Object]
Minerals formed by Evaporation ,[object Object],[object Object],[object Object],[object Object],[object Object]
Minerals formed by Metamorphism ,[object Object],[object Object]
How Are Minerals Identified? ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Color ,[object Object],- Some minerals are the same color as others - Some minerals can have many colors ,[object Object],QUARTZ ROSE QUARTZ SMOKY QUARTZ
Luster ,[object Object],Glassy- Obsidian
Examples of luster ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Hardness ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Mohs Mineral Hardness Scale ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],Softest Hardest 1 2 3 4 5 6 7 8 9 10
Streak ,[object Object],[object Object]
Density ,[object Object],[object Object]
Crystal Shape ,[object Object]
Cleavage and Fracture ,[object Object],[object Object],Obsidian No Cleavage 1 Direction of Cleavage Conchoidal Fracture BIOTITE QUARTZ
Fracture
Special Properties ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]
Economic Importance of Minerals ,[object Object]
Every American Requires 40,000 Pounds of New Minerals per Year ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]

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  • 23. Where Do Minerals Come From? Magma Evaporation In general, minerals form in two ways: Cooling magma - Crystallization of melted materials From solution - Crystallization of materials dissolved in water At the surface Beneath the surface
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