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!
High temperatures are required to form magma at oceanic ridges because the mantle beneath these regions is hotter due to its proximity to the Earth's core. In contrast, the continental crust is thicker and insulates the mantle, resulting in magma formation at lower temperatures. Additionally, the higher pressure at oceanic ridges can also contribute to the higher temperatures needed for magma formation.
The temperature difference between oceanic and continental crust is primarily due to variations in their thickness and composition. Oceanic crust is thinner and denser, leading to higher temperatures in the mantle beneath it. In contrast, continental crust is thicker and less dense, resulting in lower temperatures.
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.
The oceanic crust is denser than the continental crust due to its composition and age. This density difference causes the oceanic crust to sink beneath the lighter continental crust at subduction zones, where two tectonic plates converge. The descending oceanic crust eventually melts back into the mantle due to the high temperatures and pressures deep within the Earth.
if i thing if gago abno yudipota ka
High temperatures are required to form magma at oceanic ridges because the mantle beneath these regions is hotter due to its proximity to the Earth's core. In contrast, the continental crust is thicker and insulates the mantle, resulting in magma formation at lower temperatures. Additionally, the higher pressure at oceanic ridges can also contribute to the higher temperatures needed for magma formation.
This archipelago enjoys a wet oceanic climate with pleasant temperatures. Frost does not occur below 1,600 feet, and summer temperatures are relatively mild.
The temperature difference between oceanic and continental crust is primarily due to variations in their thickness and composition. Oceanic crust is thinner and denser, leading to higher temperatures in the mantle beneath it. In contrast, continental crust is thicker and less dense, resulting in lower temperatures.
Continental volcanoes form at oceanic-continental convergent boundaries because as oceanic plates are subducted beneath continental plates, the subducted oceanic crust melts due to the high temperatures and pressures deep within the Earth. This molten rock then rises to the surface, resulting in volcanic eruptions on the continental plate.
Oceanic-Oceanic.
False, it's the Photic Zone.
an oceanic trench
an oceanic trench
oceanic convergence is when two oceanic plates subduct beneath one another.
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.
The continental crust is the land. The oceanic is under the ocean.
In an oceanic-oceanic subduction boundary, one oceanic plate subducts beneath another oceanic plate. This process can result in volcanic island arcs being formed. In an oceanic-continental subduction boundary, an oceanic plate subducts beneath a continental plate. This can lead to the formation of volcanic mountain ranges on the continental plate.