The colour of the streak left by a mineral is one of the features used to identify it. For instance, haematite leaves a red streak, malachite leaves a light green streak, while quartz, calcite and gypsum all leave a white streak.
By scraping it across a tile of unglazed porcelain.
For demonstration purposes, hematite, pyrite, galena, and sulfur are all good for displaying a range of streak colors.
The softer the mineral, the more likely it is to leave a distinct streak that you can examine.
everywhere
silicates
hardness, luster, cleavage and fracture, color (not quite useful) and streak
though there are thousands of different minerals only about 30 are common in earths crust. these 30 minerals make up most rocks in thee crust. i hope that helped :)
Streak
either color, cleavage, and crystal form or crystal form, cleavage, and streak
Most of the constituent minerals of granite would have a white streak, although streak is not normally used as an identification aid in rocks because they are composed of a variety of minerals that may have different streak colors.
There are many properties useful in identifying minerals. The five that are most useful are cleavage, crystal habit, hardness, luster, and streak.
Streak is one of the most useful tests
The second most common group of minerals is Sedimentary rockk.
streak
fdyry
In ores
coal and iron
everywhere
The silicate group. The silicate group includes these minerals; quartz, feldspars, and micas.
The silicate group of minerals are the most abundant on the Earth.