Sedimentary
Compaction is the process of pore space reduction due to pressure exerted, normally by overburden weight. Shale would be produced by the process of lithification, which includes the individual steps of compaction and cementation of particles of sediment. Cementation occurs as mineral crystals precipitate from the water removed by compaction, binding the sedimentary particles together into rock.
Many sediments end up in the ocean, where they are deposited on the seafloor. Others may accumulate in lakes, rivers, or on land. Over time, these sediments can become compressed and cemented together to form sedimentary rocks.
The process in which sediment is laid down is called sedimentation. This involves the settling of particles carried by air, water, or ice, eventually accumulating on the Earth's surface. Over time, these sediments can become compressed and cemented to form sedimentary rocks.
In a flood where the rocks are carried away and deposited at a place which is eligible for contracting with the rocks which the n forms a chemical bond forming a cement which uses the grains to combine with the rocks\ by manpreet s.
Small particles of rock can be carried away by erosion processes such as wind, water, or ice. These particles can be transported and deposited in different locations, shaping the landscape over time.
Sedimentary rock is formed when layers of rock particles carried by wind and water are compressed and cemented together. This process can create rocks like sandstone, shale, and conglomerate.
The type of rock formed when rock particles carried by wind and water are compressed and cemented together is called sedimentary rock. These rocks are typically formed from sediments like sand, silt, and clay that accumulate in layers over time. As the layers build up, the weight of the overlying material compacts the sediments, and minerals within the water can act as a cementing agent, binding the particles together. Common examples of sedimentary rocks include sandstone, shale, and limestone.
Minerals from the cementation of igneous rocks come from the weathering and breakdown of existing igneous rock materials. During weathering, minerals are broken down into smaller particles and carried by water, eventually being deposited and cemented together to form new rocks through the process of cementation. Minerals in cemented igneous rocks can vary based on the composition of the original igneous rock.
Compaction is the process of pore space reduction due to pressure exerted, normally by overburden weight. Shale would be produced by the process of lithification, which includes the individual steps of compaction and cementation of particles of sediment. Cementation occurs as mineral crystals precipitate from the water removed by compaction, binding the sedimentary particles together into rock.
Many sediments end up in the ocean, where they are deposited on the seafloor. Others may accumulate in lakes, rivers, or on land. Over time, these sediments can become compressed and cemented together to form sedimentary rocks.
The process in which sediment is laid down is called sedimentation. This involves the settling of particles carried by air, water, or ice, eventually accumulating on the Earth's surface. Over time, these sediments can become compressed and cemented to form sedimentary rocks.
A load is the term for particles carried by a stream or river.
Sedimentary rocks can be made from any kind of material, from other rocks to shells to plant material. Basically, any rock, from metamorphic to igneous and even to sedimentary, can be weathered and eroded. These particles and grains can be carried great distances by wind, water, ice, etc. before they are deposited and lithified (cemented) back together to form sedimentary rocks.
Sedimentary rocks can be made from any kind of material, from other rocks to shells to plant material. Basically, any rock, from metamorphic to igneous and even to sedimentary, can be weathered and eroded. These particles and grains can be carried great distances by wind, water, ice, etc. before they are deposited and lithified (cemented) back together to form sedimentary rocks.
In a flood where the rocks are carried away and deposited at a place which is eligible for contracting with the rocks which the n forms a chemical bond forming a cement which uses the grains to combine with the rocks\ by manpreet s.
Detrital rocks form from the accumulation and lithification of sediments that are carried and deposited by wind, water, or ice. These sediments can come from the weathering of pre-existing rocks, erosion of mountains, or volcanic ash. Over time, the sediment particles are compacted and cemented together to form detrital rocks like sandstone, shale, and conglomerate.
Sedimentary rocks are created by the consolidation and cementing together of the rock particles that result from erosion and are carried by wind or water.