No
Solids that are amorphous. Of which perhaps glass is the best known example. [But glass is not a mineral] Materials such as TiO2 are amorphous solids.
Cleavage planes occur due to a weakness or propensity to fracture in a crystalline structure.
Emerald has poor cleavage. It typically fractures in a conchoidal or irregular manner rather than along smooth, distinct planes like some other gemstones.
Sulfur does not have cleavage because it is not a mineral. Instead, sulfur has a non-crystalline or amorphous structure. When broken, it tends to fracture along irregular surfaces rather than cleave along specific planes.
It would be important because cleavage is a tendency of some minerals to break along smooth, flat surfaces.
Bauxite does not exhibit a distinct cleavage because it is an amorphous material formed from a mixture of different minerals, primarily aluminum oxides and hydroxides, along with impurities. Cleavage is a property of crystalline materials in which the crystal breaks along specific planes due to the arrangement of atoms.
Crystalline solids have a well-ordered arrangement of particles in a repeating pattern, leading to defined geometric shapes and distinct melting points, whereas amorphous solids lack a long-range order in their atomic structure, resulting in a random arrangement of particles and no sharp melting point. Crystalline solids exhibit cleavage and anisotropy, while amorphous solids do not have cleavage planes and display isotropic properties.
A crystalline solid is one where the molecules are arranged in a regular repeating pattern, leading to a rigid and stable structure. An example is diamonds or table salt. An amorphous solid have a shape that may change over time. An example is glass in a window.
Diamont, graphite, carbon black (amorphous), fullerene, etc.
Opals are amorphous because they lack a crystalline structure. Their formation involves the precipitation of silica spheres in a disordered arrangement, which gives opals their unique play-of-color appearance. This lack of a crystal lattice is what differentiates them from most other gemstones.
A fracture is more common than a cleavage. Fractures occur when a material breaks without any predetermined pattern, whereas cleavages occur along specific planes due to the arrangement of atoms in the material.
on a gene it can occur on the promoter, intron-exon borders, poly-A-tail cleavage sites and on the exon