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Sediments that are closely packed are typically fine-grained sediments such as clay or silt. These sediments have smaller particle sizes, allowing them to settle closely together and form dense layers. Pressure and time can further compact these sediments into rock formations like shale.
When pressure is applied to pieces of sediment, compaction takes place. Compaction is the process in which pieces of sediment are under severe pressure and it becomes solid rock. Therefore, pressure turns pieces of sediment into sedimentary rock.
Sedimentary rock is formed when igneous rocks weather to sediments, then the sediments compact to sedimentary rock. When Igneous rocks are subjected to heat and pressure but do not melt, they become metamorphic rock. When igneous rocks are melted they make other igneous rocks.
The agents of lithification are pressure, compaction, cementation, and recrystallization. Pressure from overlying sediments compacts the sediment grains together, while cementation involves minerals filling in spaces between grains to bind them together. Recrystallization can also occur, leading to changes in the composition and structure of the sediment.
Pressure in cement layers can cause the sediment particles to compact and become tightly bound together, forming a solid rock mass through a process called lithification. Over time, this process can result in the transformation of loose sediments into sedimentary rocks like sandstone or shale.
Sediments that are closely packed are typically fine-grained sediments such as clay or silt. These sediments have smaller particle sizes, allowing them to settle closely together and form dense layers. Pressure and time can further compact these sediments into rock formations like shale.
density. Density is a physical property of a substance that describes how compact its molecules are within a given volume.
Igneous rocks change to Metamorphic rocks through heat and pressure. Igneous rocks change to sedimentary rocks through weathering and erosion until the igneous rock is sediments. The sediments then compact to form sedimentary rocks.
Pressing sediments involves applying pressure to compact layers of sediment over time. This pressure helps to squeeze out water and air, reducing the volume of the sediment and promoting the formation of sedimentary rocks through processes like lithification. The result is a more dense and solid rock formation.
Rock Cycle: Igneous Rock with erosion give sediments which will compact to give Sedimentary Rock which with heat and pressure give Metamorphic Rocks which will melt with heat and pressure to give magma
They are hard and compact due to prolonged exposure to high temperature and directed pressure.
When you divide the mass of a substance by its volume, you get its density. Density is a physical property that describes how compact a substance is, or how much mass is contained in a given volume.
When pressure is applied to pieces of sediment, compaction takes place. Compaction is the process in which pieces of sediment are under severe pressure and it becomes solid rock. Therefore, pressure turns pieces of sediment into sedimentary rock.
The verb 'compact' is a word for exerting pressure on something to make it smaller; to compress.The noun 'compact' is a word for a small flat case containing face powder, a mirror, and a powder puff; a word for something that is a small and conveniently shaped example of its kind.The adjective 'compact' describes a noun as closely and neatly packed together; dense.
Sedimentary rock is formed when igneous rocks weather to sediments, then the sediments compact to sedimentary rock. When Igneous rocks are subjected to heat and pressure but do not melt, they become metamorphic rock. When igneous rocks are melted they make other igneous rocks.
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Burial is the process where sediments accumulate on top of a material, such as organic matter or minerals, leading to its entombment beneath the Earth's surface. Compaction refers to the compression of these sediments over time due to the weight of the overlying layers, eventually forming rocks like sandstone or shale. Both processes are important steps in the formation of sedimentary rocks.