Clastic rocks made of particles of clay are primarily classified as shale. Shale is formed from the compaction and cementation of fine-grained sediments, predominantly clay minerals. Other types of clastic rocks, such as siltstone, may also contain clay particles but have a higher proportion of silt-sized grains. Overall, shale is the most notable clastic rock specifically composed of clay-sized particles.
Clastic sedimentary rocks are composed of particles ranging in size from clay (<0.004 mm) to boulders (>256 mm). These particles are derived from the weathering and erosion of pre-existing rocks, transported, and deposited to form clastic sedimentary rocks through processes like lithification.
Clastic sedimentary rocks composed of particles smaller than 0.006 centimeters are classified as mudstones or siltstones, depending on the specific particle size. Mudstones consist of clay-sized particles, while siltstones contain silt-sized particles. Both types are formed from the accumulation and compaction of fine-grained sediments.
The chemical sedimentary rock will not be composed of cemented rock particles.
clay minerals and quartz
Rock particles are classified into three main categories: clastic, chemical, and organic. Clastic particles are formed from the weathering and erosion of pre-existing rocks, and they vary in size from clay to boulders. Chemical particles result from the precipitation of minerals from solution, while organic particles are derived from the remains of living organisms. Together, these classifications help in understanding the formation and characteristics of sedimentary rocks.
Clastic sedimentary rocks are composed of particles ranging in size from clay (<0.004 mm) to boulders (>256 mm). These particles are derived from the weathering and erosion of pre-existing rocks, transported, and deposited to form clastic sedimentary rocks through processes like lithification.
Siltstone is a clastic rock formed from tiny particles of clay. The small particle size distinguishes siltstone from shale, which is also made of clay particles but has a finer texture. Siltstone typically forms in marine or river environments where clay-sized particles settle out of suspension and are compacted over time.
Clastic sedimentary rocks composed of particles smaller than 0.006 centimeters are classified as mudstones or siltstones, depending on the specific particle size. Mudstones consist of clay-sized particles, while siltstones contain silt-sized particles. Both types are formed from the accumulation and compaction of fine-grained sediments.
Sandstone, conglomerate, and breccia are examples of clastic sedimentary rock, composed of particles of other rocks.
maybe shale
The chemical sedimentary rock will not be composed of cemented rock particles.
clay minerals and quartz
Rock particles are classified into three main categories: clastic, chemical, and organic. Clastic particles are formed from the weathering and erosion of pre-existing rocks, and they vary in size from clay to boulders. Chemical particles result from the precipitation of minerals from solution, while organic particles are derived from the remains of living organisms. Together, these classifications help in understanding the formation and characteristics of sedimentary rocks.
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.
The three most common clastic sedimentary rocks are sandstone, shale, and conglomerate. Sandstone is composed of grains of sand cemented together. Shale is made of very fine particles like clay and mud. Conglomerate is a mix of larger rock fragments that are cemented together.
Shale, sandstone, and breccia are all types of sedimentary rocks formed from the accumulation of sediment particles. They have varying sizes of sediment grains which can range from clay-sized particles (shale) to sand-sized grains (sandstone) to angular rock fragments (breccia). Additionally, all three rock types can be found in layers or strata due to their sedimentary origins.
Clastic sedimentary rocks. Clastic sedimentary rocks are formed when small sediment particles are compacted and cemented together. This happens when the sediments are glued together by tiny crystals or chemicals from fluids that have precipitated in the pores between the sediments.