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.
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.
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 is the tendency of materials to split along definite structural planes, yielding smooth surfaces. An example is shales or shists.
It exhibits cleavage, which is the tendency of a mineral to break along certain planes of weakness determined by its atomic structure. Cleavage is a property seen in minerals with strong bonds in certain directions but weaker bonds in other directions. The resulting flat, shiny surfaces are a result of the breakage along these weakly bonded planes.
The dominant type of breakage for muscovite mica is basal cleavage, which means it breaks easily along its cleavage planes into thin sheets. This property is due to the crystal structure of muscovite mica, which consists of layers that are weakly bonded and easily separated.
It is called cleavage.
cleavage
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.
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
cleavage
cleavage
Cleavage.
Cleavage is the tendency of materials to split along definite structural planes, yielding smooth surfaces. An example is shales or shists.
Many but not all of them do, specifically that is how diamonds are traditionally cut for jewelry.mica separates into sheetshalite separates into cubesquartz does not have weakly bonded planes, so it fractures
It exhibits cleavage, which is the tendency of a mineral to break along certain planes of weakness determined by its atomic structure. Cleavage is a property seen in minerals with strong bonds in certain directions but weaker bonds in other directions. The resulting flat, shiny surfaces are a result of the breakage along these weakly bonded planes.
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