Specimen color is the least reliable method of mineral identification. Better characteristics are streak, density, and crystal structure.
Color
The same mineral can come in a variety of colors and different minerals can be the same color.
Many minerals have similar color, and mineral color can be altered by trace amounts of impurities or by weathering. A better indicator would be the mineral's streak, which is the color of the mineral when powdered, although this characteristic can't be used alone in mineral identification.
Many minerals have similar color, and mineral color can be altered by trace amounts of impurities or by weathering. A better indicator would be the mineral's streak, which is the color of the mineral when powdered, although this characteristic can't be used alone in mineral identification.
Color is the least reliable of a mineral's characteristics used in its identification.
The powder indicates the true color of the mineral and is an aid in mineral identification. That can also be called a streak.
Color.
Color, due to the effects of impurities, is the least reliable identifying mineral characteristic.
Scratching a mineral across a streak plate will result in a streak which represents the true color of a mineral without impurities or inclusions that can influence a particular specimen's color. The mineral quartz can appear in a wide variety of colors, but the streak of any colored quartz specimen will still be white. The 'streak' color is one characteristic of a mineral which will aid in its identification.
The powder indicates the true color of the mineral and mineral identification. That is also known as streak.
color
Hardness and streak color are very important. The color of the mineral helps some, as well.