This is a more complicated question than it may first appear as oceanic crustal plates are composed of Mafic rocks (rich in iron and magnesium) and so tend to have a higher density than the rocks of the continental crust. However the continental crust is significantly thicker than the oceanic crust so may in fact be heavier.
Continental plates are lighter (less dense) than oceanic plates.
This means that the cooler, heavier oceanic plate at an oceanic to oceanic convergent boundary is forced into the mantle - under the hotter, lighter oceanic plate. OR At oceanic to continental boundary the heavier oceanic plate is forced into the mantle under the lighter continental plate.
The process in which an oceanic plate sinks and pulls the rest of the tectonic plate with it is called subduction. This occurs at convergent plate boundaries where an oceanic plate collides with a continental or another oceanic plate, leading to the denser oceanic plate being forced beneath the lighter plate. As the oceanic plate descends into the mantle, it creates a trench and can trigger geological activity such as earthquakes and volcanic eruptions. This process is a key component of the Earth's tectonic cycle and contributes to the recycling of the lithosphere.
When an oceanic plate collides with a continental plate, the denser oceanic plate typically subducts beneath the lighter continental plate due to the difference in density. This subduction can lead to the formation of volcanic mountain ranges along the continental margin. The oceanic plate may also undergo partial melting, leading to the formation of magma that can erupt to the surface.
When an oceanic plate collides with a continental plate, the denser oceanic plate is forced to subduct beneath the lighter continental plate. As the oceanic plate descends into the mantle, it creates a deep ocean trench at the boundary. The subduction process can result in volcanic activity, earthquakes, and the formation of mountain ranges on the overriding continental plate.
These are zones/areas where two lithospheric plates, involving an oceanic and a continental plate collide.
At some convergent boundaries, an oceanic plate collides with acontinental plate. Oceanic crust tends to be denser and thinner thancontinentalcrust, so the denser oceanic crust gets bent and pulled under, or subducted, beneath the lighter and thicker continental crust. This forms what is called a subduction zone.
When an oceanic plate collides with a continental plate, a subduction zone is formed, leading to the creation of a trench at the oceanic plate's edge. The denser oceanic plate is forced beneath the lighter continental plate, resulting in volcanic activity and the formation of mountain ranges on the continent. This interaction can also lead to significant geological events such as earthquakes. Overall, these features reflect the dynamic processes of plate tectonics.
When an oceanic plate collides with a continental plate, the denser oceanic plate is forced beneath the lighter continental plate in a process called subduction. This leads to the formation of deep ocean trenches and volcanic arcs on the continental plate. As the oceanic plate descends into the mantle, it generates magma, which can result in volcanic activity. Over time, this tectonic interaction can also cause earthquakes along the subduction zone.
A tectonic plate boundary where one continental plate and one oceanic plate meet is known as a convergent boundary. In this scenario, the denser oceanic plate typically subducts beneath the lighter continental plate, leading to geological phenomena such as the formation of mountain ranges, volcanic activity, and earthquakes. An example of this is the boundary between the Nazca Plate (oceanic) and the South American Plate (continental), which has resulted in the Andes mountain range and significant volcanic activity.
No, the oceanic crust is denser. That's why the land areas "float" so much higher than the ocean bedrock.
At a convergent boundary where two oceanic plates meet, the denser plate will typically subduct below the less dense plate. The denser plate is usually the older, cooler, and more compacted of the two plates.