These oceanographic features are the deepest parts of the ocean floor.
The deepest segments of the ocean floor are found.
Sediment can accumulate as slowly as 0 1 millimeter 0 04 inch per 1 000 years in the middle of the ocean where only wind blown material is deposited to as fast as 1 meter 3 25 feet per year along continental margins.
In trenches associated with subduction zones.
In the geographic centers of abyssal plains.
In trenches associated with subduction zones.
Most of the igneous rocks within oceanic abyssal plains are denser.
Along mid ocean ridges b.
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.
Long mid ocean ridges b.
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.
More typical deep sea rates are on the order of several centimeters per 1 000 years.
In the geographic centers of abyssal plains c.
In trenches associated with passive margins.
The deepest segments of the ocean floor are found.
The deepest segments of the ocean floor are found.
In trenches associated with subduction zones.
In the geographic centers of abyssal plains c.