When loose sediments are compressed to form a solid cohesive rock, this process is usually referred to as lithification and the result is a lithified rock unit. Typically, some sort of cementation is usually required to hold the individual rock particles together in mass.
This process is called compaction.
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
The key to converting sediment into sedimentary rock is often though of as being pressure. And it is only by burial that enough pressure can be generated on a layer of sediment to "press" it into sedimentary rock. With pressure and time comes what is called compaction and the expulsion of (most of) the space between the particles of sediment that were deposited. Let's look at sediments being laid down and turned into sedimentary rock.When sediments are created, moved and deposited, they can consolidate and form a layer or layers. These strata will be composed of particles of organic and inorganic material. Included will be the intersticial spaces between the sediments. Any water present in the pore spaces (and there usually is) will bring with it dissolved minerals. These can precipitate out in the spaces, and will cause cementation, which is the binding of these minerals to the particles of sediment and the "sticking together" of the sediments. Following the deposition of more material, pressure (lithostatic pressure) will build on the underlying strata. The compaction forces the layer to become more dense and to "turn to stone" over time. And sedimentary rock is the result of this process.
The ____ of water and the top layer of ___ press together to form sedimentary rocks.
The process that presses sediments together is compaction. Thick layers of sediment build up gradually over millions of years. These heavy layers press down on the layers beneath them. The weight of new layers further compacts the sediments, squeezing them tightly together. The layers often remain invisible in sedimentary rock.
When sediment particles press together.
This process is called compaction.
Sediments are in sedimentary rocks. Everyday, more and more sediment is layed on top of the first batch of sediment(first layer). As the layers build up, they begin to press down on that first layer of sediment, pushing most of the air and water out of it, pushing the particles closer together. This is the process of compaction. This process occurs underground or above and is part of the way that sedimentary rocks are formed.Cementation is the next step in the recipe for making sedimentary rocks. In this step, loose sediments are glued together naturally glues like calcite and silica.
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
the correct answer is compactioncompaction
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Grinding - when you press two pussies together and simulate humping
press work is a process of forming new product
A tabloid press is also called a "sensationalist press."
The key to converting sediment into sedimentary rock is often though of as being pressure. And it is only by burial that enough pressure can be generated on a layer of sediment to "press" it into sedimentary rock. With pressure and time comes what is called compaction and the expulsion of (most of) the space between the particles of sediment that were deposited. Let's look at sediments being laid down and turned into sedimentary rock.When sediments are created, moved and deposited, they can consolidate and form a layer or layers. These strata will be composed of particles of organic and inorganic material. Included will be the intersticial spaces between the sediments. Any water present in the pore spaces (and there usually is) will bring with it dissolved minerals. These can precipitate out in the spaces, and will cause cementation, which is the binding of these minerals to the particles of sediment and the "sticking together" of the sediments. Following the deposition of more material, pressure (lithostatic pressure) will build on the underlying strata. The compaction forces the layer to become more dense and to "turn to stone" over time. And sedimentary rock is the result of this process.