A crystal.
Solids in which atoms are arranged in a definite and repeating pattern are called crystalline solids. In these solids, the atoms are arranged in a highly ordered structure, forming a crystal lattice. This arrangement gives crystalline solids their unique properties, such as cleavage and anisotropy.
A crstal
Nonliving, solid material formed in nature with particles arranged in a repeating pattern is a mineral. Atoms of a mineral are arranged in a repeating pattern to form a solid that is called a crystal.
An example of a naturally occurring inorganic solid with a definite structure is quartz. Quartz is a mineral composed of silicon and oxygen atoms arranged in a repeating pattern to form a crystal structure.
A crystal is a solid that is arranged in a specific and repeating order. The atoms or molecules in a crystal are arranged in a regular and symmetric pattern, giving crystals their unique shape and properties.
If atoms are arranged in a repeated order they are negatively charged
Atoms in a crystal are arranged in a highly ordered repeating pattern called a crystal lattice. The lattice is formed by the regular, three-dimensional stacking of atoms in specific geometric arrangements. This results in the formation of a solid crystal structure with well-defined planes and shapes.
A crystal lattice is a solid in which atoms are arranged in an orderly repeating pattern. This regular arrangement gives crystals their characteristic geometric shapes and helps define their physical properties.
Crystals are formed when the compounds in a mineral are arranged in a repeating pattern. It is a highly transparent glass mineral with a high refractive index.
I'm assuming that when you say "repeating pattern", you mean a network solid. In that case, diamonds.
Nonliving, solid material formed in nature with particles arranged in a repeating pattern is a mineral. Atoms of a mineral are arranged in a repeating pattern to form a solid that is called a crystal.
The repeating arrangement of atoms in a mineral forms a crystal due to the strong forces of attraction between the atoms, which result in a stable and orderly structure. This repeating pattern allows the mineral to grow in a geometrically regular shape, creating distinct crystal faces and external symmetry.