temperature and time or deposition and melting or collection and transportation or time and pressure
Sedimentary
sedimentary
Sedimentary rocks such as shale, sandstone, and limestone can be the source of deposited sediments through the process of weathering and erosion. These rocks are broken down into smaller pieces that are transported and eventually deposited to form new sedimentary layers.
sedimentary
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.
a rock formed by unconsolidated sediment deposited in layers
As sedimentary rock is deposited at over time, you can find fossils in it.
Broken pieces of sedimentary, igneous, or metamorphic rocks can be deposited into layers and cemented together to form sedimentary rock.
Sedimentary Rock That Forms Where Of Organisms Are Deposited In Thick Layers.
Sedimentary rocks are formed when sediments, like sand or mud, are deposited and compressed over time. This process typically occurs in bodies of water, such as oceans or lakes, where the sediments settle and eventually harden into rock layers.
To create a sedimentary rock, layers of sediment such as sand, mud, or minerals must be deposited and compressed over time. This process, known as lithification, involves the compaction and cementation of the sediment layers to form a solid rock.