Cleavage is a smooth and easy break in a mineral. Minerals are always solid because it is one of their classification requirements.
Cleavage is the way a mineral breaks along planes of weakness in its atomic structure. The number and orientation of cleavage planes are determined by the arrangement of atoms in the mineral's crystal lattice. Minerals with strong atomic bonds tend to have poor or no cleavage, while those with weaker bonds exhibit good cleavage.
Cleavage is related to the minerals atomic structure because minerals are arranged in crystal lattices . It's the shape of these lattices that determine the mineral's cleavage.
A mineral hasn't an atomic number.
A mineral's ability to split along flat surfaces is called cleavage. Cleavage is a characteristic property of minerals related to their crystal structure and internal arrangement of atoms.
Yes, all different samples of that mineral will have the same cleavage.
Yes, all different samples of that mineral will have the same cleavage.
cleavage....
The mineral cleavage is made up of many other particles to form a rock when the rock cleavage is just a rock.
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.
A good example of a mineral with basal cleavage are those from the mica group such as muscovite and biotite
CLEAVAGE
i think crystal habit is the minerals structure, while cleavage is the patter it breaks into.