Which mineral is known for its ability to cleave in perfect sheets?

Mica is distinguished by its unique physical property known as perfect cleavage, which allows it to split effortlessly into thin, flexible sheets. This characteristic arises from its layered crystal structure, where weak bonds between the layers enable easy separation. Mica is commonly found in two varieties: muscovite (light-colored) and biotite (dark-colored), both of which exhibit this property prominently.

In contrast, calcite, quartz, and feldspar do not possess this perfect sheet-like cleavage. Calcite may display cleavage but is more irregular and not as perfect as that of mica. Quartz, on the other hand, is known for its conchoidal fracture and does not cleave; instead, it breaks with a smooth, curved surface. Feldspar, while it does exhibit cleavage, typically does so in two directions at right angles to one another, rather than in the perfect sheets characteristic of mica.