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Oceanic plates are denser than continental plates, causing them to subduct when they collide. The denser oceanic plate sinks beneath the less dense continental plate due to gravitational pull. This subduction process can lead to the formation of deep ocean trenches, volcanic arcs, and earthquakes.
When a plate carrying continental crust converges with a plate carrying oceanic crust, the denser oceanic plate is typically subducted beneath the less dense continental plate. This can lead to the formation of volcanic arcs and deep ocean trenches.
Where oceanic crust is subducted under continental crust, a trench, volcanic arc, and earthquakes are likely to form. The subduction of the dense oceanic plate causes it to sink beneath the less dense continental plate, leading to the creation of these geological features due to the intense heat and pressure generated in the process.
When the oceanic plate collides with a continental plate, it is typically subducted underneath the continental plate due to its higher density. This subduction process can lead to the formation of deep oceanic trenches and volcanic arcs on the overriding continental plate. It also contributes to the recycling of oceanic crust back into the mantle.
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.
When oceanic crust collides with continental crust, the denser oceanic crust is forced beneath the continental crust in a process called subduction. This happens because oceanic crust is heavier, colder, and more dense than continental crust, making it susceptible to being subducted under the lighter continental crust. This collision can result in the formation of mountain ranges, volcanic arcs, and deep ocean trenches.
The oceanic plate is made of denser (and thinner) rock than the continental crust, so the oceanic plate gets subducted (pushed underneath) where it descends and gets melted by geothermal heat.
The oceanic plate is made of denser (and thinner) rock than the continental crust, so the oceanic plate gets subducted (pushed underneath) where it descends and gets melted by geothermal heat.
Trench
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.
A trench and a strata volcano.
Oceanic plates are denser than continental plates, causing them to subduct when they collide. The denser oceanic plate sinks beneath the less dense continental plate due to gravitational pull. This subduction process can lead to the formation of deep ocean trenches, volcanic arcs, and earthquakes.
tides will occur.
Oceanic crust is denser than continental crust, so when they collide, the denser oceanic crust is forced beneath the lighter continental crust in a process known as subduction. This subduction occurs at convergent plate boundaries where two plates are moving towards each other. The sinking oceanic crust can trigger volcanic activity and create mountain ranges on the continental crust.
When a plate carrying continental crust converges with a plate carrying oceanic crust, the denser oceanic plate is typically subducted beneath the less dense continental plate. This can lead to the formation of volcanic arcs and deep ocean trenches.
The contiental cdrust is forced under the continental crust in a process called subduction.
when oceanic crust and continental crust collide, the oceanic crust sinks down beneath the continental crust. this is called subduction.