cleavage
The color of a mineral in powdered form is called the mineral's Streak
That property is called cleavage or fracture, depending on how the mineral breaks.
The texture of metamorphic rocks composed of only one mineral with equidimensional crystals is called a granular texture. This texture indicates that the mineral grains have crystallized under conditions where there was no preferred orientation of the crystals.
The melted mineral material in the mantle is called magma.
The color of a mineral in powdered form is called its streak color. It is determined by rubbing the mineral against an unglazed porcelain plate to produce a streak.
The ability of a mineral to break along preferred directions is called cleavage. Cleavage is a result of the arrangement of atoms within the mineral structure, which causes it to break in certain directions more easily than others.
The metamorphic rock that lacks mineral grains with long axes in one direction is called marble. Marble is formed from the metamorphism of limestone or dolomite, and its grains do not exhibit a preferred orientation or alignment. It often has a smooth and uniform appearance, making it a popular material for sculptures and architectural purposes.
The two way by which minerals break are called cleavage and fracture. Cleavage is when a mineral breaks along a plane whose atomic bonds are weaker than in the rest of the mineral. Fracture is when a mineral is forced to be broken in an unnatural direction.
When a mineral dissolves in water this is called .?
It is an elemental mineral.
The color of a mineral in powdered form is called the mineral's Streak
That depends on how much mineral you have.
It is called synthetic as opposed to natural.
There is nothing called "preferred freedoms " and no test for them.
That property is called cleavage or fracture, depending on how the mineral breaks.
The powder indicates the true color of the mineral and is an aid in mineral identification. That can also be called a streak.
The texture of metamorphic rocks composed of only one mineral with equidimensional crystals is called a granular texture. This texture indicates that the mineral grains have crystallized under conditions where there was no preferred orientation of the crystals.