The 'cement' in clastic sedimentary rock is most often clay, iron, carbonate, or silicate minerals.
if it is a sedimentary rock the fossils get cemented together
Sedimentary rocks undergo processes of weathering, erosion, transportation, deposition, and lithification. Weathering breaks down existing rocks into smaller particles, which are then transported by wind, water, or ice. These sediments are eventually deposited in layers and, over time, compacted and cemented together through lithification to form solid rock. This cycle can be part of the larger rock cycle, where sedimentary rocks may also be transformed into metamorphic or igneous rocks under certain conditions.
Silica also called quartz cement, Calcite Cement, Iron Oxides also called hematite cement that bind sand together in sandstone. Sandstone also has other cementing agents that occur in less common forms. These cementing agents include pyrite, barite and gypsum.
conglomerate rock
taking chemicals and mixing them together.
Sedimentary rock is most likely the result of compacting and cementing particles together. This process involves the accumulation and compression of sediment (such as sand, mud, and organic matter) over time, eventually forming solid rock through lithification. Examples of sedimentary rocks include sandstone, shale, and limestone.
Sedimentary rock, such as sandstone, is most likely formed from the compaction and cementing of particles together. As layers of sediment accumulate and are compressed over time, the particles are gradually cemented together by minerals, creating a solid rock.
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.
Sedimentary (horseisle ansfer)
Sedimentary rocks are most likely to result from the process of compacting and cementing particles together. This process involves the deposition of sediments such as sand, clay, and gravel, which are then compacted under pressure and cemented together over time to form sedimentary rocks like sandstone, shale, and limestone.
Sedimentary rocks, such as sandstone and shale, are formed mainly from the compaction and cementation of particles like sand, silt, and clay. These particles accumulate over time in layers, undergo compaction from the weight of overlaying materials, and are cemented together by minerals to form solid rock.
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.
Sedimentary rocks are formed from the compaction and cementation of particles such as sand, silt, and clay. These particles are deposited in layers over time, and the pressure from the weight of the overlying material squeezes them together and binds them with minerals forming sedimentary rocks.
Sedimentary rocks, such as sandstone, shale, and limestone, are most likely to result from the compaction and cementation of particles. These rocks form through the accumulation and lithification of sediments that have been weathered and eroded from pre-existing rocks.
Particles in sedimentary rocks stick together because of compacting pressure from layers of sediment above them, and because of natural cements like calcite or silica that fill the spaces between particles and bind them together.
A detrital sedimentary rock made up of clay-sized particles that require no cementation to hold together is called shale. Shale forms from the compaction of clay minerals without the need for additional cementing materials.
Sedimentary rocks are most often lithified sediments, the origin of which may be from igneous, metamorphic, or other sedimentary rock, and in some cases chemical solutions or organic matter. Erosion and weathering of rock creates a range of rock particles from boulder sized to microscopic. These particles are transported by wind, water or landslide to a point of deposition or resting place. If these particles continue to be covered with additional layers of particles, the compression from the weight above, will, in time remove most of the water from the sediments. As the water is removed, cementing minerals, such as calcite or quartz, solidify from the remaining solution and fill in the gaps between the particles. The result is a lithified sediment, better known as sedimentary rock.