Because it requires more energy to transport heavier sediment than lighter sediment. As a river flows it loses energy, and hence begins to drop the heavier sediment. Imagine you had a handful of sand and a handfull of flower. The sand is heavier than the flower, and also larger. If you blow on both of your hands, the flower will be easily blown away, but the sand will be more difficult, because the grains are bigger and heavier, and require more energy to move.
The heavier sediments are the first to overcome the power of the moving water with the power of gravity.
Lighter sediments are typically deposited closer to the source of the eroded material, such as near river mouths or in low-energy environments like lakes or offshore areas. These sediments tend to settle out first due to their smaller size and lower density compared to heavier sediments.
Sediments like sand and gravel are typically deposited first in a stream channel due to their heavier weight and larger size compared to finer particles like silt and clay. These sediments settle out when the stream's velocity decreases, usually in areas with reduced flow or obstacles that disrupt the current.
The tendency for air currents of air or water to separate sediments according to size is called sorting. Sorting occurs when sediments are transported and deposited, with larger and heavier particles settling out first followed by smaller and lighter particles. This process helps to form distinct layers of sediment with particles of similar sizes.
The settling out and grading of sediments occurs through the process of sedimentation, where sediment particles in a fluid (such as water) settle out and deposit on the surface. This process is influenced by factors like particle size, density, and the velocity of the fluid. Sediments are graded based on their size and shape through sorting processes, with larger and denser particles settling out first and finer particles being deposited later.
Moving water quickly sorts sediments according to their size and weight. A flowing river that experiences a raging flood may have an unsorted mess on its hands for a short while, but afterward, the sorting process will normalize. That said, you rarely see a river carried boulder in a delta, do you?
More dense material is less buoyant in water than less dense material of equal volume. Sediment shape also plays a role in deposition sequence as material with angular irregular surfaces are more likely to be carried by water flow than smooth surfaces, due to friction with the water. Finally, the size of the sediment particle, particularly of rock material, may be most critical in the sequence of deposition; larger particles are the first to overcome the power of friction encountered in moving water, via gravity.
Heavier sediments are deposited before smaller sediments due to their greater mass and the influence of gravity. When sediment-laden water slows down, the larger particles, which require more energy to remain suspended, settle out first. As the flow continues to decrease, lighter particles can be carried further before settling. This process is known as sedimentary sorting, resulting in a stratified layering of sediments by size and weight.
Lighter sediments are typically deposited closer to the source of the eroded material, such as near river mouths or in low-energy environments like lakes or offshore areas. These sediments tend to settle out first due to their smaller size and lower density compared to heavier sediments.
Graded bedding forms when sediments settle out of a moving fluid in order of decreasing grain size. This typically occurs in environments like rivers, deltas, or deep-sea turbidity currents where strong currents transport sediment before it settles. Heavier grains settle first, followed by progressively lighter ones, creating distinct layers of different grain sizes within a sedimentary deposit.
After that it would be deposited when the flow of the river is too slow to carry it.
Sediments like sand and gravel are typically deposited first in a stream channel due to their heavier weight and larger size compared to finer particles like silt and clay. These sediments settle out when the stream's velocity decreases, usually in areas with reduced flow or obstacles that disrupt the current.
they deposit their load because otherwise it gets too heavy
As the current slows and goes around bends the heavier silt always settles first. This is the factor that causes 'meanders' in slow moving rivers. The lighter, smaller fragments are carried out to the edge of the delta.
The first deposit into the account was 500, and the last deposit was 1,000.
The tendency for air currents of air or water to separate sediments according to size is called sorting. Sorting occurs when sediments are transported and deposited, with larger and heavier particles settling out first followed by smaller and lighter particles. This process helps to form distinct layers of sediment with particles of similar sizes.
Sand is deposited on beaches by a variety of natural processes, including erosion of rocks and cliffs, wave action breaking down rocks into smaller particles, and rivers and streams carrying sediments to the coastline. These sediments are then moved along the coast by longshore drift and deposited on beaches when the energy of the waves decreases.
When sediments are deposited by water, the particles are sorted by size due to the energy of the flowing water. Larger, heavier particles settle first and are typically found at the bottom layers, while smaller, lighter particles are carried further and settle on top. This results in a graded layering effect, with coarser sediments at the base and finer sediments toward the top. Over time, this stratification can reveal information about the conditions of deposition.