tides will occur.
When two continental plates collide or a continental plate collides with an oceanic plate.
tides will occur.
You would be most likely to find a boundary between a continental and an oceanic plate along a convergent boundary, where the denser oceanic plate subducts beneath the less dense continental plate. This often leads to the formation of deep-sea trenches and volcanic activity.
Off the westcoast of North America
A convergent boundary between an oceanic plate and a continental plate.
Convergent plate boundaries where an oceanic plate collides with a continental plate or another oceanic plate are most likely to result in a subduction zone. In this scenario, the denser oceanic plate is forced beneath the less dense continental plate, creating a subduction zone.
You would most likely find a boundary between a continental and an oceanic plate at a convergent plate boundary, where the two types of plates collide. In this setting, the denser oceanic plate is typically subducted beneath the lighter continental plate, leading to geological features such as deep ocean trenches and volcanic mountain ranges. This interaction can also result in significant seismic activity.
Mountains are most likely to form at a convergent boundary where two tectonic plates collide, with one plate being forced beneath the other in a process called subduction. The intense pressure and heat generated during this collision cause the crust to deform and uplift, leading to the formation of mountain ranges.
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.
Oceanic lithosphere sinks beneath continental lithosphere at convergent boundaries primarily due to its higher density compared to continental lithosphere. As oceanic plates are denser and thinner, they are more susceptible to subduction when they collide with less dense, thicker continental plates. This process leads to the formation of deep ocean trenches and volcanic arcs, as the subducting oceanic plate melts and interacts with the overlying continental crust. Additionally, the cooler and older oceanic lithosphere is more likely to subduct than the younger, hotter continental lithosphere.
Answer this question… Subduction of oceanic crust beneath continental crust
The oceanic plate would subduct beneath the continental plate. This is because oceanic plates are denser than continental plates due to their composition, so they are more likely to be forced beneath the less dense continental plate.