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Τι (ποιος) είναι argillaceous sediments - ορισμός
GROUP OF MINERALS
Clay minerals; Clay Mineral; Argillaceous mineral; Clay Mineralogy; Clay mineralogy; Argillaceous; Argillaceous rock; Smectite group of minerals; Argillaceous minerals
![SEM]] image, 1,340× magnification)](https://commons.wikimedia.org/wiki/Special:FilePath/Kaolinite - USGS bws00008.jpg?width=200 "SEM]] image, 1,340× magnification)")
Cyclic sediments
![Top of a metric regressive cycle with [[desiccation]]s, surface of bed dolomitised. Middle liassic of the High Atlas, Morocco.](https://commons.wikimedia.org/wiki/Special:FilePath/Desiccation Rnim.jpg?width=200 "Top of a metric regressive cycle with [[desiccation]]s, surface of bed dolomitised. Middle liassic of the High Atlas, Morocco.")
SEQUENCES OF SEDIMENTARY ROCKS THAT ARE CHARACTERISED BY REPETITIVE PATTERNS OF DIFFERENT ROCK TYPES (STRATA) OR FACIES WITHIN THE SEQUENCE
Cyclic sedimentation; Cyclic sediment; Rhythmic sediment; Rhythmic sediments; Depositional cycle
Cyclic sediments (also called rhythmic sediments) are sequences of sedimentary rocks that are characterised by repetitive patterns of different rock types (strata) or facies within the sequence. Processes that generate sedimentary cyclicity can be either autocyclic or allocyclic, and can result in piles of sedimentary cycles hundreds or even thousands of metres thick.
Sediment
![[[Holocene]] [[eolianite]] and a carbonate beach on [[Long Island, Bahamas]]](https://commons.wikimedia.org/wiki/Special:FilePath/EolianiteLongIsland.JPG?width=200 "[[Holocene]] [[eolianite]] and a carbonate beach on [[Long Island, Bahamas]]")
![[[Hjulström curve]]: the velocities of currents required for erosion, transportation, and deposition (sedimentation) of sediment particles of different sizes}}](https://commons.wikimedia.org/wiki/Special:FilePath/Hjulströms diagram en.PNG?width=200 "[[Hjulström curve]]: the velocities of currents required for erosion, transportation, and deposition (sedimentation) of sediment particles of different sizes}}")
![rounding]] (horizontal).](https://commons.wikimedia.org/wiki/Special:FilePath/Rounding & sphericity EN.svg?width=200 "rounding]] (horizontal).")
![Sediment in the [[Gulf of Mexico]]](https://commons.wikimedia.org/wiki/Special:FilePath/Sediment in the Gulf of Mexico.jpg?width=200 "Sediment in the [[Gulf of Mexico]]")
![Sediment off the [[Yucatán Peninsula]]](https://commons.wikimedia.org/wiki/Special:FilePath/Sediment off the Yucatan Peninsula.jpg?width=200 "Sediment off the [[Yucatán Peninsula]]")
PARTICULATE MATTER THAT IS DEPOSITED ON THE SURFACE OF LAND
Sediments; Detrital sediment; Sea Sediment; Sedements; Sedimented; Sedimentary soil; Sedimentary layer; Lake sediment; Fluviatile sediment; Sediment (geology)
·noun The material of which sedimentary rocks are formed.
II. Sediment ·noun The matter which subsides to the bottom, frrom water or any other liquid; settlings; lees; dregs.
sediment
PARTICULATE MATTER THAT IS DEPOSITED ON THE SURFACE OF LAND
Sediments; Detrital sediment; Sea Sediment; Sedements; Sedimented; Sedimentary soil; Sedimentary layer; Lake sediment; Fluviatile sediment; Sediment (geology)
(sediments)
Sediment is solid material that settles at the bottom of a liquid, especially earth and pieces of rock that have been carried along and then left somewhere by water, ice, or wind.
Many organisms that die in the sea are soon buried by sediment.
N-VAR
Βικιπαίδεια
Clay mineral
Clay minerals are hydrous aluminium phyllosilicates (e.g. kaolin, Al2Si2O5(OH)4), sometimes with variable amounts of iron, magnesium, alkali metals, alkaline earths, and other cations found on or near some planetary surfaces.
Clay minerals form in the presence of water and have been important to life, and many theories of abiogenesis involve them. They are important constituents of soils, and have been useful to humans since ancient times in agriculture and manufacturing.
