Here's a breakdown:
* Weathering: The process of breaking down rocks, soils, and minerals through contact with the Earth's atmosphere, water, and biological organisms.
* Erosion: The process of moving weathered material from one location to another.
* Deposition: The process of dropping off the weathered and eroded material.
* Sedimentary Rocks: These rocks are formed from the accumulation and cementation of weathered and eroded material.
So, while weathering doesn't create rocks, it plays a vital role in the formation of sedimentary rocks.
Examples of sedimentary rocks formed from weathered material:
* Sandstone: Formed from sand grains (weathered from igneous or metamorphic rocks)
* Conglomerate: Formed from gravel (weathered from various rocks)
* Limestone: Formed from the accumulation of shells and other marine organisms (weathered from calcium carbonate)
* Shale: Formed from fine-grained clay (weathered from various rocks)
It's important to remember that the original rock that was weathered can be any type: igneous, metamorphic, or even other sedimentary rocks. Weathering breaks them down, and then those fragments are used to form new rocks.