Oceanic ridge continuous submarine mountain chain extending approximately 80 000 km 50 000 miles through all the world s oceans.
The deepest segments of the ocean floor are found.
In the geographic centers of abyssal plains.
Covered by clay and the skeletal remains of microplankton.
United states sitting out race to mine ocean floor for metals essential to electronics.
Along mid ocean ridges b.
Covered by clay and the skeletal remains of microplankton.
Most of the igneous rocks within oceanic abyssal plains are denser.
Most of the igneous rocks within oceanic abyssal plains are.
The deepest part of the ocean is in the mariana trench sometimes called the marianas trench located in the western pacific ocean.
In trenches associated with subduction zones.
As compared to freshwater saline ocean water is and therefore provides support to floating objects.
In trenches associated with subduction zones.
Collectively the oceanic ridge system is the most prominent feature on earth s surface after the.
The deepest segments of the ocean floor are found.
Oceanic trenches are topographic depressions of the sea floor relatively narrow in width but very long.
As compared to freshwater saline ocean water is and therefore provides support to floating objects.
The deepest segments of the ocean floor are found.
The deepest segments of the ocean floor are found covered by clay and the skeletal remains of microplankton.
Is outside the system that is dividing up the ocean floor for deep sea mining.
In trenches associated with passive margins d.
In trenches associated with subduction zones.
In the geographic centers of abyssal plains c.
Individually ocean ridges are the largest features in ocean basins.
In trenches associated with passive margins.
The deepest segments of the ocean floor are found.
At its deepest part it s just under 7 miles 6 831 miles.
In trenches associated with subduction zones.
As compared to freshwater saline ocean water is and therefore provides support to floating objects.
Oceanic trenches are a distinctive morphological feature of convergent plate boundaries along which lithospheric plates move towards each other at rates that vary from a few millimeters to over ten centimeters per year.