The oceans depths (tons of pressure) are pretty much the only place you will find water at over 100C. Anywhere else, and its water vapor!
Typically the less dense continental plate would stay afloat while the denser oceanic plate would be submerged below. This can result in volcanic eruptions at the subduction zone due to oceanic crust undergoing increased pressure and temperatures as it descends below the continental crust.
At some points, the oceanic crust bends downward and forms a deep-ocean trench. Then the oceanic crust sinks back into the mantle through a process called subduction.
it keeps the ocean and valcanos away from each other i think
oceanic-oceanic
Oceanic-Continental, Oceanic-Oceanic, and Continental-Continental.
As the seafloor spreads apart, magma from the mantle inside the earth bubbles up to the ocean and hardens in the cool temperatures, producing new oceanic crust
This archipelago enjoys a wet oceanic climate with pleasant temperatures. Frost does not occur below 1,600 feet, and summer temperatures are relatively mild.
Biotite marble
Oceanic-Oceanic.
False, it's the Photic Zone.
Typically the less dense continental plate would stay afloat while the denser oceanic plate would be submerged below. This can result in volcanic eruptions at the subduction zone due to oceanic crust undergoing increased pressure and temperatures as it descends below the continental crust.
an oceanic trench
an oceanic trench
oceanic convergence is when two oceanic plates subduct beneath one another.
Oceanic to oceanic- one plate sinks under the other Oceanic- Continental ocean crust sinks under the other
At some points, the oceanic crust bends downward and forms a deep-ocean trench. Then the oceanic crust sinks back into the mantle through a process called subduction.
The continental crust is the land. The oceanic is under the ocean.