The stripe, and color
luster streak shape density color (not always reliable tho mulltiple types of minerals can have the same color) odor tenacity reaction to acid cleavage magnetism electrical properties
The color of many minerals is highly variable. Many minerals are found in many different colors. Eg. while malachite is always green, and sulfur always yellow, quartz can come in shades of purple, green, blue, red, yellow, brown, pink, etc., and tourmaline, garnet, calcite, and fluorite are equally color variable.
The minerals that make up Gneiss are almost always: feldspars, quartz, and mica. Sometimes: kyanite, garnet, hornblende, tourmaline, magnetite, and many others. Source: Geology University Student
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The stripe, and color
luster streak shape density color (not always reliable tho mulltiple types of minerals can have the same color) odor tenacity reaction to acid cleavage magnetism electrical properties
Well minerals is in earth inorganic solid material found in nature that always has the same chemical makeup atoms arranged in an orderly pattern and properties such as cleavage and fracture color hardness and streak and luster.
When geologists say that a mineral always contains certain elements in definite proportions, they mean that the mineral always has a specific chemical composition. This composition is a key characteristic that helps identify and classify minerals. Minerals are composed of specific elements arranged in a precise crystal lattice structure.
A chemical change always changes the chemical composition of the reactants to produce products with new and unique properties, different from the reactants.
A mineral may consist of a specific element, but is most likely a combination of elements. A mineral is an inorganic solid material found in nature that always has the same chemical makeup, atoms arranged in an orderly pattern, and properties such as cleavage, streak color, hardness and luster.
Yes, all substances have inherent properties such as mass, volume, and density. These properties may not always be easily observable without specialized equipment or techniques.
Chemical change always results in the formation of new substances with different chemical properties than the original substances. This can involve the rearrangement of atoms and the breaking or formation of chemical bonds.
Granite always contains the minerals quartz, feldspar (potassium feldspar or plagioclase feldspar), and mica (biotite or muscovite). These minerals give granite its characteristic appearance and properties.
Changes in properties are not always evidence of a chemical change. Physical changes, such as changes in state (solid to liquid) or appearance, can occur without any change in the chemical composition of a substance. Chemical changes involve the rearrangement of atoms and result in the formation of new substances with different properties.
Color is not always a good way to identify minerals because some minerals change colors at certain temperatures. Some minerals have several colors and some are found in varied colors.
Chemical weathering always forms new minerals through the breakdown and alteration of pre-existing rocks due to chemical reactions with water, oxygen, or other substances in the environment.