Settlement and compaction.
As particles (sediments) are dumped, lets say, at the bottom of a lake, they will begin to settle and eventually harden into a sedimentary rock.
It is called sedimentary rock.
The process by which sediments are glued together to form sedimentary rocks is called lithification. It involves the compaction and cementation of sediments over time, due to the pressure of overlying layers and the precipitation of minerals in the pore spaces of the sediments, binding them together into a solid rock.
The type of sedimentary rock that forms when sediments stick together is called "clastic sedimentary rock." These rocks are created from the compaction and cementation of loose particles like sand, silt, and clay. Examples include sandstone, shale, and conglomerate.
Evaporation and precipitation of sediments can form sedimentary rocks over time through the process of lithification. This involves the compaction and cementation of sediments, creating layers of sedimentary rock.
The rock cycle process that causes many sedimentary rocks to have visible layers is called sedimentation. This process involves the accumulation of sediments, such as sand, silt, and clay, in layers over time. As more and more sediments are deposited and compacted, the layers become more distinct, creating the visible stratification seen in sedimentary rocks.
It is called sedimentary rock.
The process by which sediments are glued together to form sedimentary rocks is called lithification. It involves the compaction and cementation of sediments over time, due to the pressure of overlying layers and the precipitation of minerals in the pore spaces of the sediments, binding them together into a solid rock.
Sedimentary rocks like sandstone, shale, and limestone are formed when layers of sediments are compacted and cemented together over time. This process is known as lithification.
The process that presses sediments together is compaction. Thick layers of sediment build up gradually over millions of years. These heavy layers press down on the layers beneath them. The weight of new layers further compacts the sediments, squeezing them tightly together. The layers often remain invisible in sedimentary rock.
The type of sedimentary rock that forms when sediments stick together is called "clastic sedimentary rock." These rocks are created from the compaction and cementation of loose particles like sand, silt, and clay. Examples include sandstone, shale, and conglomerate.
Evaporation and precipitation of sediments can form sedimentary rocks over time through the process of lithification. This involves the compaction and cementation of sediments, creating layers of sedimentary rock.
The rock cycle process that causes many sedimentary rocks to have visible layers is called sedimentation. This process involves the accumulation of sediments, such as sand, silt, and clay, in layers over time. As more and more sediments are deposited and compacted, the layers become more distinct, creating the visible stratification seen in sedimentary rocks.
Sedimentation of transported weathered and eroded material is continuous, cyclical, or event based. New sediments are deposited on top of existing sediments, forming layers that may be visible in a sedimentary rock body.
The process of pressing sediments together to form solid rock is called compaction. It occurs when layers of sediment accumulate on top of each other, with the weight of the overlying layers causing the sediments to be pressed tightly together.
A metamorphic rock can become a sedimentary rock through weathering and erosion, where the existing rock is broken down into sediments. These sediments can then be carried away by water or wind and deposited in layers. Over time, these layers can become compacted and cemented together to form a new sedimentary rock.
Sedimentary rock is formed when sediments, like sand or mud, are compacted and cemented together over time. This process, called lithification, occurs when layers of sediment accumulate and are gradually pressed together by the weight of overlying material. Eventually, the sediments harden into rock through the binding of minerals and other materials.
I beileve the awnser would be Sedimentary Rocks because you know that if Igneous rocks are weathering, they turn into sediments. And if the sediments are squeezed or stuck together it would make a sedimentary rock. And the rock particles are sediments.