Rockslides.
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.
Foliation in rocks refers to the process being split into thin sheets. It is caused by intense pressure that shapes rocks to align in particular directions.
Rocks are broken down through a process called weathering, which can be caused by physical factors (such as wind, water, and ice) or chemical factors (such as acid rain and plant roots). Over time, weathering breaks rocks into smaller pieces through erosion, creating sediment that can be transported by natural processes like water or wind.
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.
Because they want to see how damages are being caused on earth
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.
Mechanical weathering (in this case, attrition) during erosion by water.
chemical and physical weathering
This process is an example of mechanical weathering, where rocks are physically broken down into smaller pieces by forces like water movement and abrasion.
Small Rocks, and smaller rocks, and even smaller rocks.
Smaller rocks.
rock broken by purposeful human agency