In the middle of the ocean the sedimentation rate is as slow as 0.5 - 1 cm because the sediments are only from the wind, that was blown. then in continental margins, sedimentation rate is very fast at about 2-4 m per 1000 yr. so in deep ocean, sedimentation rate is about 2 - 5 cm per 1000 years.
In the five centuries during the ottomans rule
The great plains, if we're talking about america here.
Answer:
1 Answer. The crust and the inner core are solid, whereas the outer core and inner mantle are liquid
Explanation:
