Small Rocks, and smaller rocks, and even smaller rocks.
All rocks can be broken down into smaller particles known as minerals. These minerals are the basic building blocks of rocks and can be classified based on their chemical composition and crystal structure.
All types of rocks can be broken down into soil through the process of weathering and erosion. However, softer rocks like limestone, sandstone, and shale tend to break down more easily into soil compared to harder rocks like granite and basalt.
Rocks formed from broken rocks are known as sedimentary rocks. These rocks are formed from the accumulation and lithification of sediments, which can include fragments of other rocks, minerals, and organic material. Common examples of sedimentary rocks formed from broken rocks include sandstone, conglomerate, and shale.
The tectonic force where rocks are broken is known as stress. This can be caused by factors such as compression, tension, or shear forces acting on the Earth's crust, leading to the deformation and fracturing of rocks along faults and fractures.
It can be changed by being broken down in the weathering process just like all rocks. The resulting sediment can then be lithified to for a sedimentary rock.
Smaller rocks.
rock broken by purposeful human agency
saltation
Rocks are naturally broken down into smaller pieces through a process called weathering. This includes physical weathering, where rocks are broken apart by factors like ice, wind, and water, as well as chemical weathering, where rocks are broken down by reactions with substances in the environment. Over time, these processes cause rocks to fracture and crumble into smaller particles.
sediment
Rocks are not the same because, they come from either a Volcano, or they are broken from the Earth's ground. So this causes it to be different shapes and sizes.
Clastic sedimentary rocks.