lithification
Sedimentary rock.
Sedimentary rocks come from above ground , because sedimentary rocks form when sediment piles up and sediment is made up of loose particles of clay, silt and sand
There are no following conditions. Pressure will make loose sediment into rock, the pressure may derive from the weight of water or other rocks above the sediment.
Loose sediments can become a sedimentary rock through the process of lithification. These sediments are compacted due to intense pressure and then undergo cementation to form sedimentary rocks.
Sedimentary rocks are formed when sediment is deposited out of air, ice, wind, gravity, or water flows carrying the particles in suspension. This sediment often formed when weathering and erosion break down a rock into loose material in a source area. The material will then be transported from the source area to the area of deposition. The type of sediment that is transported to a place depends on the geology of the hinterland (the source area of the sediment). However, some sedimentary rocks, like evaporites, are composed of material that formed at the place of deposition. The nature of a sedimentary rock therefore not only depends on sediment supply, but also on the sedimentary depositional environment in which it formed.
Sedimentary rock.
Sedimentary rocks come from above ground , because sedimentary rocks form when sediment piles up and sediment is made up of loose particles of clay, silt and sand
There are no following conditions. Pressure will make loose sediment into rock, the pressure may derive from the weight of water or other rocks above the sediment.
They convert the loose sediment to solid rock.
Sedimentary rocks are made by the majority of the crust are covered by a thin veneer of loose sediment, and the rock which is made as layers of this debris get compacted and cemented together.
Fossils are created when organic material becomes trapped in a soft substance that hardens over time. These substances include tree resin, naturally occurring tar, ice, loose sand and soil, and natural concrete. Fossils are most often found in forms of sedimentary rock. Sedimentary rock is made up of the hardened buildup of sand, clay and other materials that are deposited by wind and water.
Yes, sedimentary rocks are formed through compaction. Compaction occurs when loose sediment is buried and the weight of overlying layers presses down on it, causing the sediment particles to become tightly packed together. This process helps to squeeze out water and air from between the sediment particles, leading to the formation of solid sedimentary rock.
Loose sediments can become a sedimentary rock through the process of lithification. These sediments are compacted due to intense pressure and then undergo cementation to form sedimentary rocks.
Sedimentary rocks are formed when sediment is deposited out of air, ice, wind, gravity, or water flows carrying the particles in suspension. This sediment often formed when weathering and erosion break down a rock into loose material in a source area. The material will then be transported from the source area to the area of deposition. The type of sediment that is transported to a place depends on the geology of the hinterland (the source area of the sediment). However, some sedimentary rocks, like evaporites, are composed of material that formed at the place of deposition. The nature of a sedimentary rock therefore not only depends on sediment supply, but also on the sedimentary depositional environment in which it formed.
Compaction is one process leading to the formation of sedimentary rock by the pressing weight of overlying layers of sediment. Compaction leads to the formation of sedimentary rock by squeezing out air and fluids that exist between sediment particles. As the particles become closer and closer together and the fluids are removed, the particles can become cemented together by minerals that were in the fluids.
Sediments are in sedimentary rocks. Everyday, more and more sediment is layed on top of the first batch of sediment(first layer). As the layers build up, they begin to press down on that first layer of sediment, pushing most of the air and water out of it, pushing the particles closer together. This is the process of compaction. This process occurs underground or above and is part of the way that sedimentary rocks are formed.Cementation is the next step in the recipe for making sedimentary rocks. In this step, loose sediments are glued together naturally glues like calcite and silica.
Sedimentary rocks are formed from sediment deposits (gravel, sand, silt, clay) over long periods of time either on land or in water (lakes, oceans). As more and more sedimentary layers are deposited, the newer layers exert pressure on the older layers, which compacts the loose particles and cements them together - forming sedimentary rocks. Sedimentary rocks can also be formed through the precipitation of dissolved minerals to form limestone or dolomite.