Graphite has perfect cleavage because its atoms are arranged in layers that are weakly bonded together. When a force is applied parallel to these layers, they easily slide past each other, causing the mineral to break cleanly along those planes.
graphite breaks by cleavage because the bonds between its atoms are less strong in directions
talc's cleavage is perfect in one direction, basal.
Graphite has a brittle breakage pattern, meaning it will fracture into irregular pieces with sharp edges when subjected to a sufficient amount of force. This is due to its layered structure, which allows for easy cleavage along the planes of weakness between the layers.
The mineral that fits this description is quartz. It has a hardness of 7 on the Mohs scale, does not show cleavage, and has a chemical composition of SiO2.
Graphite is known to be brittle, meaning it is prone to breaking or shattering when subjected to mechanical stress. This brittleness is due to the layered structure of graphite, where the layers can easily slide past each other, leading to cleavage and fractures under pressure.
graphite breaks by cleavage because the bonds between its atoms are less strong in directions
Cleavage in graphite occurs parallel to its basal plane, resulting in thin, planar sheets being formed. Mica, on the other hand, cleaves into thin, elastic sheets parallel to its basal plane due to its layered structure.
graphite is a basal cleavage
Diamond has perfect cleavage in four directions, fluorite has perfect cleavage in four directions, sodalite has perfect cleavage in three directions, and sphalerite has perfect cleavage in six directions.
talc's cleavage is perfect in one direction, basal.
The cleavage of sodium chloride crystals is {100} Perfect, {010} Perfect, {001} Perfect.
perfect
it probably break apart with cleavage, because the carbon atoms in graphite from sheets that could split apart easily in layers.
Cobalt has perfect cleavage in all directions.
Graphite has one direction of cleavage, which means it cleaves easily along one plane, resulting in thin sheets. This property is due to the layered structure of graphite, where atoms are arranged in flat sheets held together by weak forces.
Muscovite has perfect basal cleavage, or book cleavage.
Graphite has a brittle breakage pattern, meaning it will fracture into irregular pieces with sharp edges when subjected to a sufficient amount of force. This is due to its layered structure, which allows for easy cleavage along the planes of weakness between the layers.