Rock sediments are deposited at the bottom of a body of water, such as a river or lake. When the flow of water changes direction, the sediment has different momentum, so it does not change direction as fast, and it will collide with the river bank and then settle. Another way is when a river widens or enters a lake, the flow rate decreases, so the particles fall to the bottom. This can also be seen at a delta region when a river meets a gulf or ocean. The Mississippi Delta region in Louisiana the Gulf of Mexico is a good example of this.
Sediments.
When sedimentary rock is weathered in nature by chemical or mechanical means, the particles that are produced can be eroded and deposited, becoming sediments.
When sedimentary rock is weathered in nature by chemical or mechanical means, the particles that are produced can be eroded and deposited, becoming sediments.
The layer of rock formed from sediments deposited on land is called sedimentary rock. This type of rock forms from the accumulation and compression of sediments, such as sand, silt, and clay, over long periods of time. Examples of sedimentary rocks include sandstone, shale, and limestone.
Sedimentary Rocks.
Sedimentary rock
The rock is eroded or weathered away into sediments. The sediments settle and through compaction , the sediments are pushed together to form a sediment. Short Answer: It must be broken down into a sediment.
Sediments.
They are later deposited as sediments.
Sedimentary rock is formed from sediments deposited in bodies of water. Examples of sedimentary rocks that can form in this way include limestone, shale, and sandstone. These rocks are typically composed of particles that have been weathered, transported, and compacted over time.
Sediments- Sediments are lose minerals such as rock fragments, mineral grains, and bits of a shell that has been moved by ice, wind, water and gravity.Sedimentary rock- Is a rock formed my sediments deposited into layers and being pressurized over time.
Sedimentary rock is first deposited in environments such as riverbeds, lakes, and oceans, where sediments accumulate over time. These sediments, which can include fragments of other rocks, minerals, and organic materials, settle in layers as water slows down. Over time, the weight of overlying materials compacts these sediments, leading to lithification and the formation of sedimentary rock.