To create visible ice crystals when freezing water, the freezing process should be slowed down, allowing for larger crystals to form. While ice does contain crystals, they are often too small to see without a microscope, although larger crystals can be observed on surfaces, such as car windows in winter. The formation of ice crystals can be influenced by temperature changes and the thickness of the water layer being frozen. In laboratory settings, rapid cooling can lead to visible crystal formation. The structure of ice cubes is debated; while they appear solid, they may consist of many microscopic crystalline structures that are not perfectly organized, suggesting a more complex arrangement than a single crystalline pattern.