Atoms within a mineral are arranged into an orderly geometric spatial arrangement known as crystal structure. There are 14 basic crystal lattices (refered to as the Bravais lattices) which fit into one of 7 crystal system (triclinic, monoclinic, orthorhombic, tetragonal, rhombohedral, hexagonal and cubic) and all observed minerals fit into one crystal lattice and one crystal system. Diamond on the other hand is an allotrope of carbon arranged into an isometric hexoctahedral (Cubic-type) crystal system.
The atoms of the chemical compounds or elements that compose a mineral are arranged in repeating interlocking patterns which form the crystalline structures.
A mineral crystal is not necessarily a diamond, but a diamond is a mineral crystal. All minerals, such as diamond, have crystalline structures.
examples of NONPOLAR covalent molecular crystals: hydrogen (H2), oxygen (O2), methane (CH4),Macrophage inflammatory protein-1β (CCl4),Benzene (C6H6)examples of POLAR covalent molecular crystals: Ammonia (NH3), Water (H2O)
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Crystals of a certain mineral have a regular formation of atoms. However, crystals of the same mineral can grow differently. The presence of trace minerals, variations in heat, pressure, and the space that they have to grow in can influence the shape of a crystal. Crystalline structures demonstrate characteristic geographic variations for these reasons.
A diamond is 100% carbon, and the structure may also be contaminated with traces of other minerals, some of which give a diamond colour. For example, the Hope Diamond is blue, because those crystals contain minute amounts of boron.
A mineral crystal is not necessarily a diamond, but a diamond is a mineral crystal. All minerals, such as diamond, have crystalline structures.
Diamond.A diamond is a crystal, and a crystal is a rock with neatly arranged atoms.
Diamond
If you consider other minerals, such as nitrogen -- yellow, or boron -- blue, impurities, these minerals give a diamond the respective colour. As well, there can be visible flaws in a diamond, which are inclusions of other minerals within the diamond crystal that appear as dots or streaks.
Diamond and graphite are polymorphic - minerals with the same chemical formula but of different crystal structure. Both are made only of the element carbon. Because they form under different conditions of temperature and pressure, their crystal structure arranged differently. Hence, the vastly different physical properties.Diamonds and graphite are separate allotropes of carbon, different because of their atomic structures. Carbon formed as diamond is the hardest mineral on earth.
This is because the carbon atoms are arranged differently in diamond and graphite. In a diamond, the carbon atoms are in a three dimensional crystal lattice structure. In graphite, the carbon atoms are arranged in a two dimensional sheet.
The diamond is the hardest mineral and is the state mineral of Arkansas.
Four. they are arranged tetrahedrally. The structure is similar to diamond.
Diamond is the allotrope carbon of where the carbon atoms are arranged in the specific type of cubic lattice called diamond cubic. Diamond is an optically isotropic crystal that is transparent to opaque to cloudy, depending on the quality of the diamond.
A crystal is a solid. But it is a solid with a natural geometrically regular form that has plane faces that are arranged symmetrically.
Precious minerals like diamond are some of the resources found in settling of the crystals.
One of the earliest examples would be the quartz crystal in a digital watch.