Here's a breakdown:
* Sediment: These are small particles of broken-down rocks, minerals, and organic matter.
* Binding: This process is called lithification, which involves compaction (the weight of overlying sediment presses the particles together) and cementation (minerals dissolved in groundwater precipitate between the particles, binding them together).
There are many types of sedimentary rocks, each determined by the type of sediment and the process of lithification. Some common examples include:
* Sandstone: Formed from sand grains.
* Limestone: Formed from the shells of marine organisms.
* Conglomerate: Formed from gravel-sized rocks.
* Shale: Formed from clay particles.
