Detrital sedimentary rock.
clastic sedimentary A+
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.
Sedimentary rock is formed from compacted and cemented sediments, including those from sand deposits. Over time, the pressure from layers of sediment can cause the sand particles to stick together and harden into rock. This process can take millions of years to complete.
Sediments stick together due to the presence of cementing materials such as minerals like calcite, quartz, or clay. These materials act as a natural glue, binding sediment particles together into cohesive rock formations. Over time, pressure from overlying layers helps to consolidate and solidify the sediments.
The process of lithification changes rocks into sediments. This process is broken up into two parts: cementation and compaction. In cementation, the substance crystallizes, or fills in the spaces between loose particles of sediment. In compaction, the sediments are squeezed together by the weight of layers on top of them.
Compaction does not necessarily cause materials to stick together. Cementation is more like having a binding material between the layers. Even compaction CAN result in binding together of materials such as sandstone.
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A type of sedimentary rock that forms when sediments stick together is called a clastic sedimentary rock. This process occurs when loose grains of sediment, such as sand or clay, are compacted and cemented together over time to create a solid rock. Examples of clastic sedimentary rocks include sandstone, shale, and conglomerate.
Breccia
sedimentary rocks are formed when sediments have pressure put on them and they stick together x
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.
When layers of small sediments stick together because of pressure, compaction occurs. :)
Sedimentary rock is formed from compacted and cemented sediments, including those from sand deposits. Over time, the pressure from layers of sediment can cause the sand particles to stick together and harden into rock. This process can take millions of years to complete.
Sedimantary RocksThese rocks are formed from th ehot lavaJk jk i was bored i dont reall know what they mean and i real HATE STAaR
Sediments stick together due to the presence of cementing materials such as minerals like calcite, quartz, or clay. These materials act as a natural glue, binding sediment particles together into cohesive rock formations. Over time, pressure from overlying layers helps to consolidate and solidify the sediments.
The process of lithification changes rocks into sediments. This process is broken up into two parts: cementation and compaction. In cementation, the substance crystallizes, or fills in the spaces between loose particles of sediment. In compaction, the sediments are squeezed together by the weight of layers on top of them.
The rock formed when particles stick together is called Sedimentary Rock. The type of this rock depends on the composition and texture of the particles sticking together.
Igneous rock pieces can stick together through cementation to form sedimentary rocks.