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.
No, ice does not have cleavage. Cleavage is a property of minerals, not ice. Cleavage refers to the way a mineral breaks along planes of weakness, which is not applicable to ice.
Solids that are amorphous. Of which perhaps glass is the best known example. [But glass is not a mineral] Materials such as TiO2 are amorphous solids.
The ability of a mineral to break along preferred directions is called cleavage. Cleavage is a result of the arrangement of atoms within the mineral structure, which causes it to break in certain directions more easily than others.
No, metallic and glassy are not types of cleavage. Metallic refers to a type of luster in minerals, while glassy describes the appearance of a mineral's surface. Cleavage refers to the way a mineral breaks along planes of weakness.
A mineral that splits evenly along flat surfaces is said to have a cleavage fracture. Cleavage occurs when a mineral breaks along weak atomic planes due to the internal atomic structure and bonding of the mineral.
Yes, all different samples of that mineral will have the same cleavage.
Yes, all different samples of that mineral will have the same cleavage.
Malachite exhibits a conchoidal fracture, which means it breaks with smooth, curved surfaces. It does not have cleavage, which is the tendency of a mineral to break along preferred planes.
cleavage....
The mineral cleavage is made up of many other particles to form a rock when the rock cleavage is just a rock.
The name of a mineral that splits along flat surfaces is called mica. Mica's cleavage planes allow it to be easily split into thin sheets.
A good example of a mineral with basal cleavage are those from the mica group such as muscovite and biotite
CLEAVAGE
When minerals break, they can either have fracture of cleavage. Fracture is what you're looking for, and like you said, it's what happens when the mineral breaks and leaves uneven surfaces. A good example of a fractured mineral is quartz. Cleavage, on the other hand, occurs when minerals break along weak atomic bonding planes. Cleavage creates your flatter, more geometric surfaces. Look at mica. It creates what look like sheets of paper due to it's excellent cleavage.
The tendency of a mineral to break along flat surfaces is called cleavage. Cleavage occurs due to the alignment of weak atomic bonds within the mineral's crystal structure, allowing it to break easily along specific planes. The quality of cleavage can be described by the number and orientation of the cleavage planes in a mineral.
That is referred to as fracturing.