The further away a point is from the mid-ocean ridge, the deeper the sediment layer should be. Because the ocean floor is relatively new nearer the ridge, sediments have had less time to accumulate.
Older, as it moves away from the mid-ocean ridge the sediment gets thicker and older
Sediment composition.
Near the trenches, or in the seafloor furthest away from spreading centers.
Age of seafloor rock and sediment increases with distance from the oceanic ridges.
As fluids and spaces between particles are squeezed out by the weight of overlying sediments, the particles become closer to each other, thus flattening the thickness of the strata.
Harry Hess proposed an explanation that tied together data on the age of ocean rocks, sediment thickness, and magnetic striping.
It is impossible to derive an answer from the information provided. At first glance it would appear that the answer would be 500 years; in actuality, the sediments that created the sedimentary rock would have been substantially compressed during the lithification process, resulting in a rock thickness that was less than the initial sediment thickness, depending on the type of sediment.
The difference would lie in the origin of the sediment and largely on the distance the sediment traveled.
it tells us about the transportation of sediments before deposition. i.e if a sediment has travelled a longer distance, it'll be rounder. therefore the longer the transportation takes, the well-rounded it becomes
A crosscutting feature occurs when a rock or body of sediment cuts across, through fractures, faults, or magma. Any feature that cuts across must be younger than the rock or sediment that it cuts across.
As the steam velocity increases, the diameter of the sediments being transported increases.
Was ist ein Sediment = what is a sediment