They show you the true color of the mineral. Small impurities can cause big changes in the color of a mineral.
Mineralogists use various tests to identify minerals, including the Mohs hardness scale, streak test, color, luster, cleavage, and specific gravity. These tests can help in determining the physical and chemical properties of a mineral, which are then compared to known mineral data to make an identification.
Geologists use the Mohs scale of mineral hardness to determine the relative hardness of a mineral by scratching it with minerals of known hardness. The scale ranks minerals from 1 (softest) to 10 (hardest) based on their ability to scratch or be scratched by other minerals.
You should perform a scratch test or a streak test to help identify the different minerals. Additionally, you can use a hand lens to examine the crystals and mineral structure of each rock to further differentiate the minerals. It may also be helpful to consult a mineral identification guide or seek assistance from a professional geologist.
Rubbing the mineral against an unglazed ceramic tile, called a streak plate, leaves a streak of the powdered mineral. This powder reflects the true color of the mineral. It's called a streak test, and the resultant line of color is called the streak. A link can be found below to check facts and learn more.
Mineral streak refers to the color of a mineral when it is powdered and left as a trail on a porcelain streak plate. It helps identify minerals because different minerals produce distinct streak colors.