Topaz will leave a streak, it is just that the streak is white and will therefore not be apparent against the white background of the standard streak plate.
ALSO
Topaz is harder than unglazed porcelain (the streak plate), and therefore normally leaves a scratch rather than a streak.
Yes... It's streak is clear, or colorless.
Topaz's streak may either be colorless or white. Other than that, no, topaz really does not have a streak.
:)
Lazia Marcuss, lazia.m3@gmail.com
White
Those minerals that are harder than the unglazed porcelain streak plate will scratch it rather than leave a streak.
it is used to test streak, for rocks and minerals
The streak of a mineral can distinguish between two samples that have the same color. The streak is often a different color. To test streak, use a streak plate. This is a piece of unglazed porcelain, like the back side of a tile.
Streak is the color of powder of a mineral on a porcelain plate.
Regardless of the color of the garnet specimen, it would leave a white streak.
Those minerals that are harder than the unglazed porcelain streak plate will scratch it rather than leave a streak.
A streak plate
It's called a streak plate.
Minerals with a hardness greater than around 7 on the Mohs hardness scale will not leave a streak on a standard unglazed porcelain streak plate. They will instead scratch and powder the streak plate.
streak
Diamond will not leave a streak on a porcelain streak plate because diamond is harder than the streak plate. It will leave a scratch on the streak plate for the same reason.
Which mineral leaves a green-black powder when rubbed against an unglazed porcelain plate?
Streak color is determined by scraping the mineral across a a streak plate, (which is made of unglazed porcelain), and then observing the color of the streak, which is left on the plate. Note that some minerals do not leave a streak, as they are too hard. Thus, it is important to learn other identification methods, to use in conjunction with streak color, in order to identify minerals.
it is used to test streak, for rocks and minerals
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. Coloration of mineral specimens is sometimes due to impurities. In a powdered form, the impurities are not abundant enough to cause coloration in the streak, thus revealing the true color of the mineral. The streak is used as an aid in the identification of a mineral.a streak mark on a flat surface
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. Coloration of mineral specimens is sometimes due to impurities. In a powdered form, the impurities are not abundant enough to cause coloration in the streak, thus revealing the true color of the mineral. The streak is used as an aid in the identification of a mineral.a streak mark on a flat surface
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. Coloration of mineral specimens is sometimes due to impurities. In a powdered form, the impurities are not abundant enough to cause coloration in the streak, thus revealing the true color of the mineral. The streak is used as an aid in the identification of a mineral.a streak mark on a flat surface