There is no general shape of a mineral. Each mineral has its own shape, even though two different minerals might have the same shape. A few examples of shapes of minerals are: Rhomboid, rock, and cubic.
diamond
cube
Diamond is the hardest mineral at Mohs hardness 10, ten being the hardest. There is no natural mineral substitute for processes requiring diamond. Diamond is four times as hard as corundum, the mineral constituting rubies and sapphires. Although diamond is the hardest naturally occurring mineral, it is easily fractured, a characteristic which allowed early jewellery makers to facet this crystal.
No shape is mathematical really unless it has been created by a mathematical formula, but is certainly a geometric shape. But anything which is a 2D or 3D shape is geometric. My improvement: A catenary curve from a mathematical equation such as cosh x, is a mathematical and natural shape. Maby each other arch can be approximated by a mathematical formula.
suraj
That would be it's crystalline form.
There is no general shape of a mineral. Each mineral has its own shape, even though two different minerals might have the same shape. A few examples of shapes of minerals are: Rhomboid, rock, and cubic.
Yes, a natural diamond is mineral. Diamonds are formed from carbon.
When a mineral forms a definite shape, it is known as a crystal. Crystals are ordered arrangements of atoms or ions in a repeating pattern that gives them their characteristic shape. Crystal shape is determined by the internal arrangement of atoms within the mineral.
Tipperary Natural Mineral Water was created in 1986.
What mineral is a principal natural resource of the Southeast states
The mineral are natural resources because they are naturally occurring substances.The naturally occurring things are natural resources.
B
minerals get its crystal shape by the heating and pressure from rock
As a natural mineral sodium chloride is called halite.
The cubic shape of a mineral is a result of its crystal structure, where the atoms are arranged in a symmetric pattern with equal dimensions along each axis, leading to a cube-like appearance. This arrangement reflects the internal atomic bonding and organization within the mineral.