according to the data from the 1900's to the 1950's this theory is not true.
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The mineral will break along its crystal cleavage planes, resulting in smooth surfaces. This is because the atoms within the mineral are arranged in such a way that they break cleanly along specific planes of weakness. This property is known as cleavage, and minerals that exhibit this characteristic include mica and calcite.
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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The mineral will break along its crystal cleavage planes, resulting in smooth surfaces. This is because the atoms within the mineral are arranged in such a way that they break cleanly along specific planes of weakness. This property is known as cleavage, and minerals that exhibit this characteristic include mica and calcite.
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.