Yes, all different samples of that mineral will have the same cleavage.
CLEAVAGE
feldspar
Calcite's cleavage is a perfectional, 4 directional rhombohedron shape.
Cleavage
To determine if a mineral has cleavage or fracture, observe how it breaks. Cleavage is characterized by smooth, planar surfaces along specific directions where the mineral splits easily, reflecting its internal atomic structure. In contrast, fracture results in irregular, jagged surfaces without defined planes. Testing a mineral's breakage pattern can help you identify its cleavage or fracture nature.
Yes, all different samples of that mineral will have the same cleavage.
Cleavage is a smooth and easy break in a mineral. Minerals are always solid because it is one of their classification requirements.
No, a mineral cannot have both fracture and cleavage. Fracture refers to the way a mineral breaks when no cleavage is present, whereas cleavage describes the way a mineral breaks along its planes of weakness. Minerals either exhibit fracture or cleavage, but not both at the same time.
The mineral cleavage is made up of many other particles to form a rock when the rock cleavage is just a rock.
cleavage....
The name of a mineral that splits along flat surfaces is called mica. Mica's cleavage planes allow it to be easily split into thin sheets.
Luster refers to the way light interacts with the surface of a mineral. Cleavage is the way a mineral breaks along planes of weakness. Hardness is the resistance of a mineral to scratching. Color is the visual appearance of a mineral, which can vary widely within the same mineral species.
A good example of a mineral with basal cleavage are those from the mica group such as muscovite and biotite
CLEAVAGE
The tendency of a mineral to break along flat surfaces is called cleavage. Cleavage occurs due to the alignment of weak atomic bonds within the mineral's crystal structure, allowing it to break easily along specific planes. The quality of cleavage can be described by the number and orientation of the cleavage planes in a mineral.
Because many minerals exhibit cleavage.
Cleavage is the tendency of a mineral to break along smooth planes parallel to zones of weak bonding.