a crystal structure is a turtle in disguise
Geologists classify crystal structures based on the arrangement of atoms within the crystal lattice, the symmetry of the crystal, and the types of bonds between atoms. Common crystal structures include cubic, tetragonal, orthorhombic, monoclinic, and triclinic structures.
By definition, a mineral must have a crystal structure.
A mineral crystal is not necessarily a diamond, but a diamond is a mineral crystal. All minerals, such as diamond, have crystalline structures.
By size, and geometry, by their structure in one of the six mineral crystal systems.
crystal structure
Solid oxygen has crystalline structures.
Octahedral holes in crystal structures are important because they provide spaces where certain atoms or ions can fit, helping to stabilize the overall structure of the crystal. These holes play a key role in determining the physical and chemical properties of the crystal, such as its density, hardness, and conductivity.
NaCl is crystal-shaped because they are ionically bonded, and all ionic bonds make hard, but brittle crystal structures.
Hydrogen gas (H2) does not exhibit a crystal structure at standard conditions because it is a gas composed of diatomic molecules. In order for hydrogen to form a crystal structure, it needs to be in a solid form, such as solid hydrogen which exhibits different crystal structures depending on the temperature and pressure conditions.
Minerals form crystal structures.
H C P may stand for "highest common factor" in mathematics, or "hexagonal close-packed" in the context of crystal structures.
The repeating patterns of a mineral's particles that form a solid are called crystal lattice structures. These structures are responsible for the characteristic shape and properties of minerals.