Cleavage is the tendency of a minerals to break along flat surfaces. It means that the make up of the mineral is uneven, dense on one side and not dense in the other, causing the mineral to break along flat surfaces. The tendency of a mineral to break irregurlary is fracture.
The strong tendency of certain minerals to break along smooth parallel planes is known as cleavage. Cleavage occurs due to the internal atomic arrangement of the mineral, which allows it to break along specific planes of weakness.
Cleavage is the breaking of a mineral along flat surfaces. Fracture, on the hand is just the chipping or "fracture" of a mineral.Cleavage is the tendency to break along flat surfaces, and fracture is the tendency of a mineral to break into irregular pieces.
Cleavage is the tendency of a mineral to break along flat planar surfaces as determined by the structure of its crystal lattice. Fracture is the way a mineral breaks other than along a cleavage plane. They both describe a way a mineral can break.
... internal atomic arrangement. The crystal shape forms based on how the mineral's atoms are arranged in a repeating pattern. Cleavage is the tendency of a mineral to break along planes of weakness due to the atomic structure.
When a mineral breaks along a weakly bonded plane, it is called cleavage. Cleavage is the tendency of a mineral to break along specific planes of weakness due to the arrangement of atoms in the crystal lattice.
Cleavage is the tendency of a mineral to break along smooth planes parallel to zones of weak bonding.
The strong tendency of certain minerals to break along smooth parallel planes is known as cleavage. Cleavage occurs due to the internal atomic arrangement of the mineral, which allows it to break along specific planes of weakness.
Cleavage is the tendency of a mineral to break along smooth planes parallel to zones of weak bonding.
Minerals do have zones of weakness. They are known as cleavage planes. It is the tendency for minerals to break along flat, parallel surfaces. They come in a variety of categories, but it is ultimately where the mineral will break if struck. It cal be basal, prismatic,cubic, rhombohedral, octahedral, or dodecahedral.
Cleavage is the breaking of a mineral along flat surfaces. Fracture, on the hand is just the chipping or "fracture" of a mineral.Cleavage is the tendency to break along flat surfaces, and fracture is the tendency of a mineral to break into irregular pieces.
A mineral's ability to split easily along planes of weakness, producing flat surfaces.
Cleavage- in geolohy, the tendency of a mineral to splitalong specific planes of weakness to format smooth flatSurface.Fracture- the manner in which a mineral breaks alongeither curved or irregular
Cleavage is the tendency of a mineral to break along flat planar surfaces as determined by the structure of its crystal lattice. Fracture is the way a mineral breaks other than along a cleavage plane. They both describe a way a mineral can break.
... internal atomic arrangement. The crystal shape forms based on how the mineral's atoms are arranged in a repeating pattern. Cleavage is the tendency of a mineral to break along planes of weakness due to the atomic structure.
When a mineral breaks along a weakly bonded plane, it is called cleavage. Cleavage is the tendency of a mineral to break along specific planes of weakness due to the arrangement of atoms in the crystal lattice.
Whether a mineral has cleavage or fracture is determined by its internal atomic structure and the way in which it breaks when subjected to stress. Cleavage is the tendency of a mineral to break along planes of weakness, while fracture is the way a mineral breaks when no cleavage planes are present.
Cleavage of galena is the tendency of the mineral to break along planes of weakness, resulting in smooth, flat surfaces. Galena exhibits perfect cleavage in three directions at right angles to each other, producing cubic or octahedral shapes. This property is a result of the crystal structure of galena.