* Sandstone: Formed from sand grains cemented together.
* Conglomerate: Formed from larger pebbles and gravel cemented together.
* Breccia: Similar to conglomerate, but the fragments are angular, indicating they were broken close to their source.
* Mudstone: Formed from very fine sediment, like clay and silt, compressed and cemented together.
* Limestone: Can form both chemically and from the accumulation of shells and other organic matter.
* Coal: Formed from the accumulation of plant matter, compressed and transformed over time.
These are just a few examples, and there are many other types of sedimentary rocks, each with its own unique composition and formation story.
