Cementation is a geological process that occurs when minerals precipitate from water and fill the spaces between sediment particles, binding them together. This process often takes place in sedimentary rocks, where minerals like calcite or silica act as a glue, solidifying the sediment into a more durable structure. Over time, cementation contributes to the formation of rocks such as sandstone and limestone. The cementation process is influenced by factors like temperature, pressure, and the chemical composition of the water. As sediments accumulate and are buried, the increased pressure can enhance the cementation process, leading to the creation of stronger and more compact rock formations. This is an essential step in the rock cycle, contributing to the Earth's geological diversity.