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Deposition is the geological process in which sediments, soil and rocks are added to a landform or landmass. Wind, ice, water, and gravity transport previously weathered surface material, which, at the loss of enough kinetic energy in the fluid, is deposited, building up layers of sediment.
Expert witness deposition in a mock trial simulation. The court reporter, who is an officer of the court, administers the oath to the deponent. The person to be deposed (questioned) at a deposition, known as the deponent, is usually notified to appear at the appropriate time and place by means of a subpoena.
Deposition may refer to: Deposition (law), taking testimony outside of court; Deposition (politics), the removal of a person of authority from political power;
The principle of original horizontality states that the deposition of sediments occurs as essentially horizontal beds. Observation of modern marine and non-marine sediments in a wide variety of environments supports this generalization (although cross-bedding is inclined, the overall orientation of cross-bedded units is horizontal).
A diagram of various depositional environments. In geology, depositional environment or sedimentary environment describes the combination of physical, chemical, and biological processes associated with the deposition of a particular type of sediment and, therefore, the rock types that will be formed after lithification, if the sediment is preserved in the rock record.
Deposition is the phase transition in which gas transforms into solid without passing through the liquid phase. Deposition is a thermodynamic process . The reverse of deposition is sublimation and hence sometimes deposition is called desublimation .
Sediment sorting is influenced by: grain sizes of sediment, processes involved in grain transport, deposition, and post-deposition processes such as winnowing. [3] As a result, studying the degree of sorting in deposits of sediment can give insight into the energy, rate, and/or duration of deposition, as well as the transport process responsible for laying down the sediment.
[5] [6] The transport of eroded materials from their original location is followed by deposition, which is arrival and emplacement of material at a new location. [1] While erosion is a natural process, human activities have increased by 10–40 times the rate at which soil erosion is occurring globally. [7]