Pitchblende (or uraninite) is an important mineral of uranium and is of course radioactive.
The hardness on the Mohs scale is 5-6.
The density is high, between 10 and 11 g/cm3.
Streak is the property of a mineral that is determined by rubbing the mineral on a special plate to reveal the color of its powdered form. This can help identify minerals because a mineral's streak color is often different from its external color.
Pitchblende is a name for uraninite, a radioactive mineral from which uranium ore is extracted. The composition of pitchblende can include uranium oxide (UO2) and triuranium octoxide (U3O8), along with lead oxide and pockets of helium.Pitchblende is a radioactive, uranium-rich mineral and ore. It has a chemical composition that is largely UO2, but also contains UO3 and oxides of lead, thorium, and rare earth elements. It is known as pitchblende due to its black color and high density. It is also commonly referred to as Uraninite.
The special property that magnetite displays is that it is attracted by a magnet. Cleavage is the mineral property that explains why some minerals break along smooth, flat surfaces.
Color is a mineral property that can be determined simply by observation.
Luster is typically considered the least useful mineral property, as it does not provide much information about the mineral's identity or composition. Luster simply describes how light is reflected off the surface of a mineral, such as metallic, glassy, or dull, and can vary even within the same mineral species.
pitchblende
The color of pitchblende makes it easy to find it.
pitchblende was the first, but any good uranium ore will do as it is a daughter element of uranium's decay.
Pitchblende, a radioactive mineral, was first discovered by Johann Gottfried Gahn and K. A. Hauy in 1789. It was later identified as a uranium-rich mineral by Martin Heinrich Klaproth in 1789.
It's Radioactivity
Pitchblende, uraninite, carnotite, davidite, euxenite, etc.
Fracture, cleavage, luster, hardness, color ect. a property a mineral posesses.
A primary property is one that all minerals possess, whereas a special property is found in only one or a few minerals.
Examples: hematite (Fe2O3), ilmenite (FeTiO3), pitchblende (UO2). The most common such oxide mineral is silicon dioxide in sand.
Uranium was identified as an oxide in the mineral pitchblende by Martin Heinrich Klaproth in 1789.
Fluoresces
In pitchblende from Joachimow (now in Czech Republic), 1789