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How to Classify a Mineral


Color and luster may seem like the easiest way to identify a mineral, but it is important to consider other factors because many minerals can be a wide variety of colors.
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             The color of a mineral in powder form is called its streak, which is more useful in classifying a mineral than its overall coloring. Streak can be found by rubbing the mineral sample across a small piece of unglazed porcelain, which is called a streak plate (Ludman and Marshak 55). One of the best examples of the usefulness of a streak plate is when classifying the mineral pyrite. Pyrite, often called "fool's gold, " has a black streak while actual gold has a gold streak. It is important to remember that a streak plate has a hardness of about 7, which leads to the next important characteristic when classifying a mineral: hardness and breakage (Neyman 2).
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             The ability of a mineral to resist scratching and abrasion is known as its hardness. Hardness is one of the most useful properties for identifying minerals, because it relates to its unique atomic structure. According to Stephen Marshak, "The atoms or ions of crystals in a hard mineral are more strongly bonded than those in a soft mineral". Friedrich Mohs, a German mineralogist, worked out a scale of hardness for minerals ranging from 1 to 10 (Neyman 2). The number one is assigned to the softest mineral, Talc and 10 is assigned to the hardest mineral, Diamond. Minerals that are harder than 7 will scratch a streak plate, rather than leave colored powder behind. The softest minerals such as Talc and Kaolinite are used for things like powder and clay, while harder minerals such as Quartz are used for things like watch settings to ensure that they do not scratch easily (Ludman 56). .
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             Along with hardness, breakage is a characteristic unique to each mineral. The terms cleavage and fracture are used to describe the way a mineral breaks. Cleavage is the tendency of a mineral to split along smooth, definite surfaces, while fracture is used to describe minerals that break with no smooth planes or patterns (Marshak 133).


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