Cementation
Detrital sedimentary rock. clastic sedimentary A+
Chemical sedimentary rocks are formed from the precipitation from, or evaporation of, water that is saturated with dissolved minerals. In addition, most clastic sedimentary rocks are also formed from the cementing together of sediment particles by the precipitation of minerals from water.
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.
Detrital sedimentary rocks are made from weathered rocks.
Yes, sedimentary rocks can form through chemical processes. One example is the precipitation of minerals from solution, which occurs when dissolved ions in water bond together to form solid minerals. Another example is chemical weathering, where minerals in rocks are dissolved or altered by chemical reactions, leading to the formation of new minerals.
Detrital sedimentary rock. clastic sedimentary A+
Because it forms from animals that were once living which makes it an organic sediment. It can also be classified into the Detrital sedimentary rock category because it is compacted together.
Detrital rocks are sedimentary rocks that are composed of particles of weathered and eroded igneous, metamorphic, or other sedimentary rocks that have been deposited, compacted, and cemented together. Sandstone, conglomerate, shale, and breccia are examples of detrital sedimentary rocks.
Detrital sedimentary rock. clastic sedimentary A+
Chemical sedimentary rocks are formed from the precipitation from, or evaporation of, water that is saturated with dissolved minerals. In addition, most clastic sedimentary rocks are also formed from the cementing together of sediment particles by the precipitation of minerals from water.
Detrital sedimentary rock. clastic sedimentary A+
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.
Sedimentary rocks.
Shale
They get grounded into sediment and then get pressed together.
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.
Sedimentary rocks are formed by the compaction from overlying sediments and by the cementation resulting from the replacement of fluids with minerals, in a process of rock formation known as lithification.