yes because it splits in half or pieces.
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.
Sapphire has a mixture of both cleavage and fracture characteristics. It has poor cleavage in one direction and conchoidal fracture, which means it breaks with smooth, curved surfaces similar to glass.
When quartz is broken it has a conchoidal fracture. Fracture is the appearance of the broken plane of a mineral. A conchodal fracture is described a being curved, and looking like broken glass.
Obsidian does not have cleavage because of the way it forms. Obsidian is essentially nature's form of glass and so it has no regular or patterned crystal structure. Without that crystal structure, there is no cleavage.
Yes, glass does exhibit conchoidal fracture, which is characterized by smooth, curved surfaces resembling the shape of a shell. This type of fracture occurs because glass is an amorphous solid, lacking a crystalline structure, which allows it to break in a way that produces these distinctive curves. The conchoidal fracture is often seen in broken glass edges, making them sharp and jagged.
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.
Azurite does not have cleavage, but it exhibits a conchoidal fracture, meaning it breaks into smooth, curved surfaces similar to glass.
Sapphire has a mixture of both cleavage and fracture characteristics. It has poor cleavage in one direction and conchoidal fracture, which means it breaks with smooth, curved surfaces similar to glass.
Malachite typically exhibits conchoidal fracture rather than cleavage. This means that it breaks in a smooth, curved manner similar to glass or obsidian, rather than along specific planes like cleavage.
When quartz is broken it has a conchoidal fracture. Fracture is the appearance of the broken plane of a mineral. A conchodal fracture is described a being curved, and looking like broken glass.
Peridot typically exhibits a conchoidal fracture, meaning it breaks in a smooth, curved manner like glass. It does not have a distinctive cleavage pattern due to its crystalline structure.
Opal does not have a cleavage or fracture because it lacks a distinct cleavage plane like minerals such as mica or calcite. Instead, opal typically fractures conchoidally, meaning it breaks with smooth, curved surfaces similar to glass.
Sulfur typically exhibits a conchoidal fracture when it breaks, resulting in smooth, curved surfaces resembling glass. This fracture is caused by the arrangement of sulfur atoms in its crystalline structure and the brittleness of the element.
Sulfur does not exhibit cleavage because it lacks a distinct crystal structure. Instead, sulfur has a conchoidal fracture, meaning it breaks along curved, irregular surfaces similar to glass.
Ah, the cleavage and fracture of a ruby are like the unique brushstrokes on a canvas. Cleavage refers to how the ruby breaks along certain planes due to its crystal structure, while fracture describes how it breaks irregularly. Just like happy little accidents in painting, each cleavage and fracture in a ruby tells a story of its journey through time.
Obsidian does not have cleavage because of the way it forms. Obsidian is essentially nature's form of glass and so it has no regular or patterned crystal structure. Without that crystal structure, there is no cleavage.
Garnet has no cleavage, meaning it does not break along distinct planes when subjected to stress. Instead, garnet exhibits a conchoidal fracture, breaking with a smooth, curved surface similar to glass.