The further from the delta, the finer the sediments deposited.
Sediments in outwash are typically well-sorted and composed of sand and gravel, deposited by meltwater streams flowing from glaciers. In contrast, sediments in moraines are unsorted and contain a mix of various sizes of rocks, debris, and till that has been directly deposited by the glacier. Outwash sediments are usually sorted by size and shape, while moraine sediments are unsorted and show a wider range of material types.
marine basin between India and Eurasia
Sediments produced from weathering and erosion are deposited in still environments, compacted by the weight of additional sediments and cemented by minerals that are present in the water that is being squeezed out between sediment particles.
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Eroded and deposited sediments undergo the processes of compaction and cementation. Compaction involves the squeezing together of sediments due to the weight of overlying layers, while cementation occurs when minerals precipitate in the pore spaces between particles, binding them together to form a solid rock.
The term used in geology to describe the relationship between adjacent layers of sedimentary rock is called stratification. Stratification refers to the layering of sedimentary rocks based on the different characteristics of the sediments deposited over time.
The relationship between the planet's SPEED and its distance from the Sun is given by Kepler's Third Law.From there, it is fairly easy to derive a relationship between the period of revolution, and the distance.
The term for the distance and relationship between two tones in music is called "interval."
Alluvium refers to clay, silt, sand, gravel, or similar detrital material deposited by running water. New alluvium are these sediments that are being deposited right now and older alluvium refers to sediments that were deposited a short while before the new alluvium. For example, a 500 years ago some sediments were deposited in a stream bed and last year more sediments were deposited in that same stream bed. The 500 year old sediment would be older alluvium and the 1 year old sediment would be the younger alluvium.
Deposition is the geological process where sediments, which are particles like sand, silt, and clay, are laid down or settled out of a transporting medium, such as water, wind, or ice. This process occurs when the energy of the transporting medium decreases, allowing the sediments to accumulate in layers. Over time, these deposited sediments can compact and cement together, forming sedimentary rocks. Thus, deposition is the mechanism through which sediment is transferred from one location and accumulated in another.
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