cleavage
A line of weakness in which sedimentary rocks can be separated is called a bedding plane. This is where layers of sediment have accumulated and can be easily split or eroded along this plane due to variations in sedimentary deposition.
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.
cleave
cleave
It is known as cleavage.
cleavage
A line of weakness in which sedimentary rocks can be separated is called a bedding plane. This is where layers of sediment have accumulated and can be easily split or eroded along this plane due to variations in sedimentary deposition.
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.
cleave
cleave
When a mineral breaks along a weakly-bonded plane, it is called cleavage. Cleavage is a property that describes how a mineral breaks along its crystal structure.
It is called cleavage.
A slip plane in a crystal is a specific crystallographic plane along which plastic deformation occurs when shear stress is applied. It is a preferred plane for dislocations to move and cause the crystal to deform without breaking. Movement along slip planes allows crystals to change shape without fracturing.
A mineral that breaks along a weakly bonded plane is called "cleavage". Cleavage is the tendency of a mineral to break along smooth, flat surfaces determined by its internal atomic structure.
cleavage.