Pelites are clastic rocks made from clay and they may be specifically called mudstones, siltstones, and shales.
Flint is a chemical sedimentary rock that forms from the precipitation of silica-rich fluids, rather than from the accumulation and compaction of organic or clastic sediment particles.
Sandstone is a clastic sedimentary rock composed of cemented sand particles.
Sandstone, conglomerate, and breccia are examples of clastic sedimentary rock, composed of particles of other rocks.
No, marble is not a clastic rock. It is a metamorphic rock that forms from the recrystallization of limestone. Clastic rocks are composed of fragments of pre-existing rocks or minerals that have been cemented together.
Yes, shale is a clastic sedimentary rock composed of clay minerals and other fine-grained particles that have been compacted and cemented together.
maybe shale
Detrital sedimentary rock. clastic sedimentary A+
Sandstone is the sedimentary rock formed from weathered rock.
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.
Detrital sedimentary rock. clastic sedimentary A+
Flint is a chemical sedimentary rock that forms from the precipitation of silica-rich fluids, rather than from the accumulation and compaction of organic or clastic sediment particles.
Sandstone is a clastic sedimentary rock composed of cemented sand particles.
Sandstone, conglomerate, and breccia are examples of clastic sedimentary rock, composed of particles of other rocks.
Clastic refers to sedimentary rocks with rock particles of various sizes cemented together in a finer matrix.
No, clastic sedimentary rock with very large particles is not metamorphic rock. Metamorphic rock is formed from existing rock that has been changed by heat and pressure. Clastic sedimentary rock, on the other hand, is formed from the accumulation and cementation of broken rock fragments.
Shale is a fine-grained sedimentary rock composed of clay minerals and tiny particles of other minerals. It forms from the compaction of mud and silt over long periods of time. Shale is commonly found in layers in sedimentary rocks and is known for its ability to split into thin, flat pieces.
The 'cement' in clastic sedimentary rock is most often clay, iron, carbonate, or silicate minerals.