The rock used to find a mineral's streak color is unglazed porcelain.
To measure the streak color of a mineral, the first step is to obtain a sample of the mineral you want to test. Step 2, find a nice, clean ceramic tile with a white unglazed back. Step 3, using a corner of your mineral, move it across the back of the tile while pushing down enough to see the streak and its color. Step 4, compare the streak color with samples of known minerals, from color photos in a book of minerals, or from a written description of minerals and their streak colors.
It means the color of a minerals powder. When you rub a mineral against a piece of unglazed porcelain tile, the minerals powder is left behind, although the powder's color may seem a little bit lighter than the mineral's color..............
to find the minerals streak, what i the mineral rubbed in
The streak of a mineral refers to the color left on a streak plate after rubbing a mineral across its surface. A streak plate can be as simple as the unglazed side of a porcelain tile. The streak is the mineral in a powdered form from abrasion with the hard, slightly textured surface of the unglazed porcelain streak plate. The streak color may differ from the color observed in a specimen. The streak is used as an aid in the identification of minerals.
The characteristic used to determine the color of a mineral's powder is known as its "streak color." This is achieved by scratching the mineral against an unglazed porcelain plate to observe the color of the powdered residue left behind. Streak color can sometimes differ from the visible color of the mineral.
What you are referring to is called a streak test. It's used as an aid to mineral identification. As a mineral is drawn over the unglazed tile surface, it is reduced to a streak of dust which reveals the true color of the mineral. If no color is revealed, the streak color is called white. An amethyst crystal which appears purplish will actually have a white streak, because the streak color of the constituent quartz is white. The purplish color of amethyst is due to other reasons.
To find the streak of a rock, you can rub the rock against an unglazed white porcelain tile to observe the color of the powder left behind. The color of the streak can help identify the minerals present in the rock.
It can be helpful because when you try to find Hemiatite it has various colors. But when you do a streak test the color always turns out red. So it depends on the kind of rock in the groups.
You're testing it's hardness.
a streak test is a test wheree you rub a mineral across a streak plate to see the color of its streak, which is a better indentifying factor of the mineral than the external color. A scratch test is when you scratch a mineral to find out its hardness on the Mohs Scale of Hardness. This is also another useful identifying factor
One characteristic used to identify minerals is their hardness, which is determined by the Mohs scale. Another characteristic is the mineral's color, although this can sometimes be misleading due to impurities. Other identifying factors include a mineral's streak (the color of its powdered form), cleavage (the way it breaks along planes), and luster (how it reflects light). By examining these properties, geologists and mineralogists can accurately identify different minerals.
Hardness: Try to use it to scratch other minerals and have other minerals scratch it. Take for example quartz. It's a 7.0 and will scratch every mineral below a 7.0 on the Mohs hardness scale. However, it will be scratched by everything above it such as Diamond (10.0) and Corundum( rubies andsapphires, 9.0)Streak: Use a streak plate and simply run the mineral down the plateDensity: Find the mass and volume of the mineral. For volume you'll more than likely, have a mineral that will beirregularlyshaped. You'll have to use the displacement method by filling a graduatedcylinderwith x amount of water and put the mineral inside subtracting and before and after water placement and find the difference. After this, you'll divide the mass by volume and you'll get your answer to the density of the mineral.