they all could be different colors it just depends on the texture of them
Color is the observable color of a mineral specimen in natural light. Streak is the color of a mineral when powdered. The color of a specific mineral specimen may be different than its streak color. Because many impurities can alter the color of a mineral, but not the streak, streak is a more accurate predictor in mineral identification.
Color is the least reliable of a mineral's characteristics used in its identification.
Color
The powder indicates the true color of the mineral and is an aid in mineral identification. That can also be called a streak.
A mineral's color may be influenced by inclusions of other elements or minerals, or even exposure to heat, light, and radiation. A more reliable identification based on color would be the streak, or color of the powdered mineral.
Color is the observable color of a mineral specimen in natural light. Streak is the color of a mineral when powdered. The color of a specific mineral specimen may be different than its streak color. Because many impurities can alter the color of a mineral, but not the streak, streak is a more accurate predictor 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.
Specimen color is the least reliable method of mineral identification. Better characteristics are streak, density, and crystal structure.
Color
The powder indicates the true color of the mineral and mineral identification. That is also known as streak.
Hardness and streak color are very important. The color of the mineral helps some, as well.
because it is not the color that matters but the jedbots that matters.
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.
streak
Believe it or not color is the least reliable identification method for a mineral. While it can be very helpful when used along with other types of identification tests, color alone proves nearly useless. This is because several different minerals can have the same color or one mineral can be several different colors. Generally this is due to the varying chemical compositions a single mineral can take on. For example, iron, depending on its oxidation state, can cause the same mineral to be several different colors, leaving the examiner with a large list of possibilities. Also, in another example, there are hundreds of minerals that are known to be green so again the possibilities are endless.