Sinkation
Deep-oceanic trenches are most abundant around the rim of the Pacific. Deep ocean trenches are surficial evidence for sinking of oceanic lithosphere into the mantle at a subduction zone.
Sinking of oceanic lithosphere into the mantle at a subduction zone.
When one plate sinks under the other, it is callled subduction, no matter what kind of plate it is. When two oceanic plates collide, they form trenches(i.e. the mariana trench). Hope this answers your question!!!
Oceanic crust sinking under a plate with continental crust
The discovery of the mid-ocean ridge confirmed Alfred Wegener's hypothesis that the continents were moving,
The trenches are evidence that one of the colliding plates is moving beneath the other. As the two plates move together, one gets pushed below the other. The place where this sinking/bucking occurs creates a deep trench. The deepest of which is Marianas trench about 7 miles deep.
Subduction is part of the geological process of plate tectonics. A subduction zone is a place where the oceanic plate is sinking back in to the mantle (usually at the edge of a continental plate.
Think of it like a pot of boiling soup, if you look at the pot of boiling soup there are areas where the soup is bubbling up to the top but ASLO other areas where the soup is moving back down to the base of the pot (it is called convection) - the soup pot does not have to get wider!. Well the Earth behaves in the same way. The mid-oceanic ridges are places where the hot internal rocks are rising up to make new oceanic sea floor crust, but around the edges of the ocean there are other areas where could sea floor crust is sinking back into the middle of the Earth. These areas are called the deep ocean trenches (or subduction zones) such as the Marianas Trench. Thus, overall the everything is kept in balance and the size of the Earth remains constant. Note also that there are places on the Earth where instead of crust sinking back into the middle of the Earth, continents crash into one another and when they do this the crustal rocks become folded and mountains are formed - again the process of mountain building balances out the spreading that happens at the mid-oceanic ridges.
The pacific oceanic plate is sinking beneath conential plate
The pacific oceanic plate is sinking beneath the continental plate to which Japan is attached in what is called a subduction zone. The oceanic plate is being destroyed.
When two oceanic plates or two plates both containing oceanic crust collide or converge, the convergent boundary will form a trench. The plate which has the higher density will plunge beneath the other plate forming a trench.
They're there simply to help support the pipe, and stop it sinking into the ground beneath it.