its deposited somewhere else
Seafloor continues to move away from the mid-ocean ridge and eventually comes into contact with another plate boundary. Ocean plates subduct underneath continental plates and are forced down into the lithosphere
Much of this phosphate then concentrates in marine sediment. Some of the phosphate is eventually incorporated into the bodies of marine animals such as fish.
Much of this phosphate then concentrates in marine sediment. Some of the phosphate is eventually incorporated into the bodies of marine animals such as fish.
When seafloor spreading happens, a rift forms at the bottom of a ocean and separates to form new rock. This is an example of a divergent plate boundary
A ridge with transverse faults is formed, where new oceanic crust (seafloor) is formed.
A ridge with transverse faults is formed, where new oceanic crust (seafloor) is formed.
The ocean seafloor is a home to many descriptive sea creatures.
The bottom of the ocean.
in order for the phosphorus to leave the oceanic environmental .
1. New sea-floor is created by the upwelling of magma at mid-ocean spreading centers; old ocean floor is destroyed by subduction at deep sea trenches. 2. The area is a subduction zone. Magma from underground comes up and destroys that crust. That crust is then recycled and the magma cools and hardens. That creates new land, that creates the trenches. Seafloor spreading is in the ocean and happens with convection currents. That is the relationship between. 3. As new seafloor is formed at mid-ocean ridges, the old seafloor is pushed down into trenches at subduction zones.
The Pacific seafloor formed at a faster spreading rate than the Atlantic seafloor.
The bottom of an ocean is typically called the seafloor. Although the seafloor can have variant geographical features such as mountains or volcanos, a normal, and flat terrain is called the seafloor.