Crystalline ceramics have a long-range atomic order, resulting in a structured pattern, while non-crystalline ceramics, or amorphous ceramics like glass, lack this long-range order and only exhibit short-range atomic arrangements. Rapid cooling of molten materials can lead to the formation of amorphous solids, as there isn’t enough time for atoms to organize into a crystal structure. In contrast, slow cooling typically results in crystalline forms. A practical way to differentiate between crystalline and amorphous silica is by examining for air bubbles, which are abundant in amorphous types but absent in crystalline forms. Opal is highlighted as an example of an amorphous SiO2, emphasizing its glass-like properties.