graphite breaks by cleavage because the bonds between its atoms are less strong in directions
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.
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 will break apart with cleavage because the carbon atoms are arranged in layers that have weak bonds between them. This allows the layers to slide past each other easily, resulting in cleavage along flat planes.
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.
graphite is a basal cleavage
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.
it probably break apart with cleavage, because the carbon atoms in graphite from sheets that could split apart easily in layers.
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.
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 will break apart through cleavage, which means it will split along flat surfaces parallel to its crystal structure. This is because graphite has a layered structure with weak bonds between the layers, allowing them to easily slide past each other.
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.
The ability of a mineral to break along smooth, flat surfaces is called cleavage. Cleavage occurs due to the weak bonds between the atoms in a mineral's crystal structure, which allows the mineral to break along specific planes. The quality of cleavage can vary among different minerals and is an important diagnostic property used in mineral identification.
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.
The mineral that fits this description is graphite. Graphite is very soft and can be easily scratched by a fingernail. It has a metallic luster and a black streak.
Some minerals that have only one direction of cleavage include mica (like muscovite), halite (salt), and graphite. Cleavage is the tendency of minerals to break along preferred planes due to their atomic structure.
Graphite will break apart with cleavage because the carbon atoms are arranged in layers that have weak bonds between them. This allows the layers to slide past each other easily, resulting in cleavage along flat planes.