Quartz is a very common mineral, and some of its main characteristics include being glass-like in appearance and having a shiny surface. These properties are due to its ability to form into well-defined crystals that reflect and refract light. Additionally, quartz can appear granular when it is found in massive form, often forming compact, grain-like masses.
However, the characteristic that does not align with quartz is having cleavage. Cleavage in minerals refers to the tendency to break along smooth, flat surfaces, which is a property due to weaknesses in the mineral's structure. Unlike some minerals, quartz does not have cleavage. Instead, it exhibits a property known as conchoidal fracture, which means it breaks with curved, shell-like surfaces rather than smooth, flat planes.
In summary, the property that does not describe quartz is having cleavage, as quartz is known for its conchoidal fracture. The other characteristics such as being glass-like, shiny, and sometimes appearing granular are true descriptions of quartz.