Examples of specimens that represent deep water low energy deposits include mudstones, siltstones, and fine-grained sandstones. These rock types typically form in quiet marine environments, such as deep-sea basins, where sediments settle slowly due to minimal energy from waves and currents. Fossils found in these deposits are often well-preserved due to the lack of disturbance.
Fluvial deposits are more likely to sort sediments based on size and shape due to the moving water, while glacial deposits tend to mix different-sized sediments. Fluvial deposits often form distinct layers or beds, reflecting changes in flow intensity or sediment composition, whereas glacial deposits are typically unsorted and lack clear layering. Fluvial deposits are common in low-energy environments like rivers and deltas, while glacial deposits are more common in high-energy settings like mountain valleys and ice sheets.
Deposition occurs when water or wind slow down because they lose the energy needed to transport sediment. As the velocity decreases, the water or wind can no longer carry particles of sediment and they settle out, leading to deposition. This process is similar to how a river deposits sediment as it flows into a larger body of water or how wind deposits sand dunes when its speed decreases.
Delta deposits are sedimentary deposits that accumulate at the mouth of a river as it flows into a larger body of water, formed by the river's sediment being deposited due to a decrease in flow velocity. Alluvial deposits are sediments that are transported and deposited by flowing water, typically forming along riverbanks, floodplains, and in river channels.
Alluvial deposits are formed when water transports and deposits sediment, such as sand, silt, and gravel, in low-lying areas like riverbeds, floodplains, and deltas. These deposits accumulate over time as the water flow decreases and the sediment settles.
Stagnation deposits are accumulations of sediment, debris, or minerals that settle and build up in stagnant or slow-moving water bodies such as lakes, ponds, or pools. These deposits can affect water quality, reduce oxygen levels, and provide breeding grounds for mosquitoes and other pests. Regular maintenance and circulation of water are important in preventing stagnation deposits.
When water loses its ability to hold sediment due to a decrease in velocity or capacity, it deposits the sediments it was carrying. This process is called sedimentation, and it can result in the formation of sedimentary layers over time.
carbon dioxide, water, energy
photosynthesis
glucose + oxygen = energy + carbon dioxide + water
photosynthesis
photosynthesis
photosynthesis
Yes, water intake decreases fat deposits because it removes toxins in the cells. This will decrease your water weight and fat deposits.
water is everywhere.
The answer depends on how much water there is and how large each specimen is.
atoms
oxygen.