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A mineral that breaks into smooth pieces when a tool such as a hammer is used is said to have cleavage. Cleavage is the way a mineral breaks along planes of weakness in its crystal structure, resulting in smooth, flat surfaces. The number and orientation of these cleavage planes are specific to each mineral and can help in identifying the mineral.
cleavage
Silicon typically exhibits cleavage rather than fracture. Silicon has a crystal structure that allows it to cleave along specific planes with clean breaks, unlike other materials that exhibit more random fracturing patterns.
That property is called cleavage or fracture, depending on how the mineral breaks.
Quartz does not have cleavage because it lacks planes of weakness along which it breaks. Instead, quartz exhibits conchoidal fracture, breaking in a way that produces curved, shell-like pieces.
A mineral that breaks into jagged pieces exhibits fracture.
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A mineral that breaks into smooth pieces when a tool such as a hammer is used is said to have cleavage. Cleavage is the way a mineral breaks along planes of weakness in its crystal structure, resulting in smooth, flat surfaces. The number and orientation of these cleavage planes are specific to each mineral and can help in identifying the mineral.
Cleavage is when a mineral breaks into flat pieces. Fracture is when a mineral breaks into irregular pieces. Topaz atom bonds are weaker in some parts and stronger in others. When it is equally strong then it breaks into irregular pieces and if it all weak in a flat line then it will be flat.
Cleavage is when a mineral breaks into flat pieces. Fracture is when a mineral breaks into irregular pieces. Topaz atom bonds are weaker in some parts and stronger in others. When it is equally strong then it breaks into irregular pieces and if it all weak in a flat line then it will be flat.
A material that loses cohesion (meaning it breaks into separate pieces) when it fails is known as a brittle material. Therefore the material exhibits brittle behaviour.
When a mineral breaks into jagged pieces, it is called a "fracture." This occurs when the mineral does not break along cleavage planes, resulting in rough and irregular surfaces. Fracture types include conchoidal (shell-like), fibrous, splintery, and uneven.
A mineral that breaks into irregular pieces is said to show "conchoidal fracture." This type of fracture produces smooth, curved surfaces resembling the shape of a shell. It is commonly observed in minerals like quartz and obsidian, which do not have a distinct cleavage pattern. The irregular breaking is a result of the mineral's internal atomic structure.
cleavage
Silicon typically exhibits cleavage rather than fracture. Silicon has a crystal structure that allows it to cleave along specific planes with clean breaks, unlike other materials that exhibit more random fracturing patterns.
That property is called cleavage or fracture, depending on how the mineral breaks.