* Weathering: Breaks down existing rocks into smaller pieces (sediments) through processes like freezing/thawing, wind abrasion, or chemical reactions.
* Erosion: Transports these sediments away from their original location by wind, water, or ice.
* Deposition: The transported sediments settle and accumulate in a new location, often in layers.
Over time, these layers of sediment are compacted and cemented together by pressure and minerals dissolved in water, forming sedimentary rock.
Examples of sedimentary rocks include:
* Sandstone: Formed from sand grains
* Limestone: Formed from the shells of marine organisms
* Shale: Formed from clay and silt particles
