It depends how deep it is buried. If it is just covered with more and more sediment, it will compact and cement to become sedimentary rock. If it is buried to the point where it gets into the mantle or a comparable area, it can become melted into an igneous rock or baked and altered into a metamorphic rock.
Sedimentary rock is formed when small rock fragments are cemented together. This happens through a process called lithification where sediments are compacted and cemented together over time. Sandstone and conglomerate are examples of sedimentary rocks formed in this way.
Gravity plays a significant role in the movement of rock fragments. Rock fragments are often transported downhill by gravity through processes like landslides, rockfalls, and creep. The weight and slope of the terrain determine the speed and distance that rock fragments can travel due to gravity.
Rock fragments that are squeezed together tightly form a sedimentary rock called breccia. Breccia is composed of angular fragments of rocks that are cemented together by a fine-grained matrix. It typically forms near fault zones or where there has been significant rockfall or landslides.
The name for weathered rock fragments is "sediment." Sediment can be composed of a variety of materials, including broken pieces of rock, minerals, and organic matter that have been eroded and transported by wind, water, or ice.
The movement of rock fragments is called erosion.
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They start to form into one
They become compacted and cemented into sedimentary rock.
it devolves into sand
Large angular rock fragments describes an agglomerate. This usually happens in volcanic vents.
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They are later deposited as sediments.
The movement of rock fragments is called erosion.
Given enough time, they may collect in sedimentary basins and form rock through a process of lithification.
Sedimentary rock is formed when small rock fragments are cemented together. This happens through a process called lithification where sediments are compacted and cemented together over time. Sandstone and conglomerate are examples of sedimentary rocks formed in this way.
A conglomerate, classified by rounded rock fragments larger than 2cm compacted and cemented into a rock.
It gets eroded (broken down), then buried (maybe at the bottom of the sea), then the fragments become cemented as dissolved minerals fall out of solution to fill the cracks, forming a solid rock. The new rock is sedimentary (from sediment).