If a mineral doesn't have cleavage, it is said to have fracture. Fracture refers to the way a mineral breaks along irregular, non-flat surfaces. This can include minerals breaking into uneven, jagged pieces or splintering in a more random pattern.
Cleavage is when you can break the rock into square like pieces and Fracture is when you break a rock into uneven different shaped pieces.
This is called cementation.
Cleavage and fracture describe how a mineral breaks. Cleavage shows the tendency of a mineral to break along specific planes due to its crystal structure, while fracture refers to irregular breakage patterns. Cleavage can create smooth surfaces, aiding in mineral identification and classification, while fractures can vary in appearance, from conchoidal (shell-like) to uneven.
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A mineral that breaks into jagged pieces exhibits fracture.
fracture
Cleavage
When it breaks, it breaks in big jagged pieces.
fracture
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.
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Cleavage is the property of minerals that causes them to split into pieces with uneven surfaces. Cleavage is determined by the crystal structure of the mineral and can vary in direction and quality.
If a mineral doesn't have cleavage, it is said to have fracture. Fracture refers to the way a mineral breaks along irregular, non-flat surfaces. This can include minerals breaking into uneven, jagged pieces or splintering in a more random pattern.
The property is referred to as cleavage or fracture, the tendency, or lack of tendency, of a mineral to break along planes of weakness. Some minerals have multiple planes of cleavage. Some have none, and are said to exhibit fracture.Cleavage is the tendency of a mineral to break along flat surfaces. The way in which a mineral breaks depends on how its atoms are bonded, or joined together. In a mineral that displays cleavage, the bonds of the crystal structure are weaker in the directions in which the mineral breaks.fracture is the tendency of a mineral to break into irregular pieces. Some minerals such as quartz break into pieces with curved surfaces. Other minerals may break differently-perhaps into splinters or into rough or jagged pieces. In a mineral that displays fracture, the bonds that join the atoms are fairly equal in strength in all directions. The mineral does not break along flat surfaces because there are no particular directions ofweakness in its crystal structure.
Brittle materials, such as glass or ceramics, tend to break in irregular jagged pieces when subjected to stress. This type of fracture occurs due to the sudden release of stored elastic energy within the material, causing it to shatter into sharp, uneven fragments.