Fracture
Breakage in minerals refers to how a mineral breaks when subjected to external forces such as impact or pressure. It is used to describe the way a mineral fractures or cleaves along certain planes or directions, which can help identify the mineral based on its unique breakage pattern.
The property of minerals that break with jagged surfaces is called "fracture." This type of breakage occurs when a mineral does not break along cleavage planes but instead produces irregular, rough surfaces. Fracture can be categorized as conchoidal (smooth and curved) or uneven (jagged and rough).
When a mineral breaks with rough edges, it is called a "fracture." This is different from cleavage, which is when a mineral breaks along smooth, flat planes. Fracture can be described as conchoidal (shell-like), uneven, or fibrous.
That property is called cleavage or fracture, depending on how the mineral breaks.
When minerals do not display cleavage, they are said to have a fracture. Fracture describes the way a mineral breaks when it does not have cleavage planes. This can result in irregular or random patterns of breakage.
Fracture
Fracture
"Uneven cleavage"
Fracture.
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uneven induction hardening pattern
The breakage of a mineral not along planes of weakness in the crystal structure is called conchoidal fracture. This type of fracture results in smooth, curved surfaces resembling the inside of a seashell. It is common in minerals with strong atomic bonding like quartz.
Breakage in minerals refers to how a mineral breaks when subjected to external forces such as impact or pressure. It is used to describe the way a mineral fractures or cleaves along certain planes or directions, which can help identify the mineral based on its unique breakage pattern.
The property of minerals that break with jagged surfaces is called "fracture." This type of breakage occurs when a mineral does not break along cleavage planes but instead produces irregular, rough surfaces. Fracture can be categorized as conchoidal (smooth and curved) or uneven (jagged and rough).
When a mineral breaks with rough edges, it is called a "fracture." This is different from cleavage, which is when a mineral breaks along smooth, flat planes. Fracture can be described as conchoidal (shell-like), uneven, or fibrous.
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.
fracture