oldest
no they found ocean ridges sonar maps alone found deep-sea trenches
Divergent boundaries form ocean ridges.
There are two types of deep ocean sediments, abyssal clay and biogenous oozes. Abyssal clays are fine-grained sediment, while biogenous ooze is composed of the hard parts of microscopic organisms.
Chalk formed from sediments made of skeletions of microscopic living things in the ocean must be a(n) organic rock.
because that there are younger rocks found at ocean ridges than the ones found near deep-sea trenches
The seafloor rocks vary in different places. Rock samples near ocean ridges are younger than rocks at deep sea trenches
oldest
no they found ocean ridges sonar maps alone found deep-sea trenches
No, the theory is that Seafloor spreading state that the new ocean crust is formed at ocean ridges and is destroyed at deep sea trenches.
the deep ocean basin consist of the deepest part of the ocean . :)
Ocean current paths of travel, underwater volcanoes, tectonic plate movement, depends which specific ridges you are talking about.
Phosphorus Cycle
Phosphorus cycle
phosphorus cycle
Mid-ocean ridges transfer energy from the mantle/asthenosphere/lithosphere to the surface. The energy is from the deep Earth.
Sea Floor spreading has to do with the crust forming at ocean ridges and being destroyed at deep sea trenches.