piilosilikaattia
Piilosilikaattia, also known as cryptocrystalline silica, is a form of silica that is composed of microscopic crystals, too small to be seen with a light microscope. This distinguishes it from other forms of silica like quartz, which are made up of larger, visible crystals. Piilosilikaattia is found in a variety of geological formations and is often associated with sedimentary rocks. Its properties can vary depending on its specific structure and composition, but it generally exhibits hardness and a conchoidal fracture.
Common examples of rocks containing piilosilikaattia include chert, flint, jasper, and agate. These materials have been