Subduction occurs and oceanic trench is formed.
When oceanic and continental crust meet, a subduction zone is formed where the denser oceanic crust is forced beneath the less dense continental crust. This process typically results in the formation of deep ocean trenches, volcanic arcs, and earthquakes.
When a continental plate moves over an oceanic plate, the denser oceanic plate is typically subducted beneath the continental plate. This process leads to the formation of a trench at the point of subduction and can result in volcanic activity as the subducted oceanic plate melts and causes magma to rise. The interaction between these two plates can also lead to earthquakes due to the stress and friction generated at their boundaries.
Earthquakes happen because of continental plate shifts. Oceanic plate shifts cause title waves.
tsunamis and earthquakes
When an oceanic plate collides with a continental plate, the denser oceanic plate is forced beneath the continental plate in a process called subduction. This creates a deep oceanic trench. As the oceanic plate sinks, it heats up, melts, and forms magma that rises to the surface, leading to volcanic activity.
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In a subduction zone, an oceanic plate moves under another plate (whether continental or oceanic). Sometimes pressure builds up, and earthquakes occur.
When oceanic and continental crust meet, a subduction zone is formed where the denser oceanic crust is forced beneath the less dense continental crust. This process typically results in the formation of deep ocean trenches, volcanic arcs, and earthquakes.
When a continental plate moves over an oceanic plate, the denser oceanic plate is typically subducted beneath the continental plate. This process leads to the formation of a trench at the point of subduction and can result in volcanic activity as the subducted oceanic plate melts and causes magma to rise. The interaction between these two plates can also lead to earthquakes due to the stress and friction generated at their boundaries.
when oceanic crust and continental crust collide, the oceanic crust sinks down beneath the continental crust. this is called subduction.
At a convergent plate boundary between an oceanic and continental plate, the oceanic plate is usually denser and subducts beneath the continental plate. This can lead to the formation of deep oceanic trenches, volcanic arcs on the continental plate, and earthquakes due to the intense pressure and friction. Over time, the oceanic plate can melt and create magma that rises to form volcanic mountain ranges on the continental plate.
Earthquakes happen because of continental plate shifts. Oceanic plate shifts cause title waves.
tsunamis and earthquakes
When an oceanic plate collides with a continental plate, the denser oceanic plate is forced beneath the continental plate in a process called subduction. This creates a deep oceanic trench. As the oceanic plate sinks, it heats up, melts, and forms magma that rises to the surface, leading to volcanic activity.
When an oceanic plate converges with a continental plate, the oceanic plate slips under the continental one and into the mantle in a process called subduction. The area will be prone to large earthquakes and tsunamis. A chain of volcanoes will form on the continent.
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When oceanic and continental plates diverge, the oceanic plate moves away from the continental plate, creating a rift. This process can lead to the formation of new oceanic crust as magma rises to fill the gap, resulting in mid-ocean ridges. The continental plate may also experience stretching and thinning, which can create rift valleys. Overall, this divergence contributes to the dynamic nature of plate tectonics and the formation of new geological features.