minerals get its crystal shape by the heating and pressure from rock
The natural shape of a mineral would be its crystalline structure.
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.
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.
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Size and shape are descriptors of the physical attributes. Others would include colour, lustre, and opacity.
The shape of a mineral depends on the chemical structure that the bonds form between atoms in the mineral. A cubic mineral (such as pyrite) has a chemical structure that, as bonds are made, a cubic shape is formed.
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Geologists can infer information about how the mineral formed and the conditions under which it grew based on its shape. Crystals that form under specific conditions tend to have characteristic shapes, known as crystal habits, which can provide clues about the mineral's history and environment.
A mineral is always a solid because it has a definite volume and shape due to its atomic structure and arrangement.
Diamond is one mineral in the isometric crystal system.