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Identifying Minerals Geologists rely on several relatively simple tests to identify minerals These tests are based upon a mineral’s physical and chemical.

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Presentation on theme: "Identifying Minerals Geologists rely on several relatively simple tests to identify minerals These tests are based upon a mineral’s physical and chemical."— Presentation transcript:

1 Identifying Minerals Geologists rely on several relatively simple tests to identify minerals These tests are based upon a mineral’s physical and chemical properties

2 Identifying Minerals Color
Many times the color of a mineral is caused by the presence of trace elements or compounds. One of the least reliable clues to a mineral’s identity Example: Quartz can be found in a variety of colors, including red jasper, purple amethyst, and orange citrine.

3 Identifying Minerals Luster The way a mineral reflects light
Luster can be either metallic or nonmetallic Silver, gold, copper, and galena have shiny surfaces that reflect light; they are said to have a metallic luster Nonmetallic minerals such as calcite, gypsum, sulfur, and quartz to not shine like metals; they are described as being dull, pearly, waxy or silky

4 Identifying Minerals Texture
Texture describes how a mineral feels to the touch The texture of a mineral might be described as smooth, rough, ragged, greasy, soapy, or glassy. Texture is usually used in combination with other tests

5 Identifying Minerals Streak
Streak is the color of a mineral when it is broken up and powdered A mineral’s streak does not always match its external color The mineral is rubbed across an unglazed porcelain plate in order to produce a colored powdered streak on the surface of the plate

6 Identifying Minerals Hardness
Hardness is a measure of how easily a mineral can be scratched The Mohs Hardness Scale rates minerals on whether they can scratch other minerals. Example: Diamond is a 10 on the Mohs scale, since it cannot be scratched and can scratch all other minerals

7 Identifying Minerals Cleavage and Fracture
A mineral that splits relatively easily and evenly along one or more flat planes is said to have cleavage Examples: mica breaks in sheets, halite breaks in three directions Minerals that break with rough or jagged edges are said to have fracture Examples: Flint, obsidian have an arclike fracture pattern resembling chain shells

8 Identifying Minerals Density and Specific Gravity
Density is the ratio of mass to volume of a substance Density reflects the atomic weight and structure of a material Specific gravity is the ratio of the weight of a substance to the weight of an equal volume of water at 4 degrees Celsius


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