Want this question answered?
Be notified when an answer is posted
Subduction is when one of the plates is forced down beneath the other plate at the convergent boundary.
A divergent boundary does not occur at a convergent boundary. At convergent boundaries, tectonic plates move towards each other and usually result in the formation of mountains, ocean trenches, or volcanic activity. In contrast, divergent boundaries occur when plates move away from each other and create new oceanic crust.
No, convergent boundaries occur where plates move toward each other and collide or subduct, while divergent boundaries occur where plates move away from each other. It is not possible for a convergent boundary to turn into a divergent boundary because the underlying plate tectonics processes are fundamentally different.
The three types of convergence are convergent boundary, divergent boundary, and transform boundary. Convergent boundaries occur when tectonic plates collide, divergent boundaries occur when tectonic plates move away from each other, and transform boundaries occur when tectonic plates slide past each other horizontally.
Where an oceanic plate dives under a continental plate (e.g. just offshore the Washington/Oregon coast, creating a line of explosive volcanos just inland).
At a convergent boundary, three types of collisions can occur: oceanic-oceanic, oceanic-continental, and continental-continental. In an oceanic-oceanic collision, one oceanic plate subducts beneath the other, forming a deep ocean trench. In an oceanic-continental collision, an oceanic plate subducts beneath a continental plate, creating volcanic arcs and mountain ranges. In a continental-continental collision, both continental plates crumple and fold, forming high mountain ranges.
Explosive eruptions typically occur more frequently near convergent boundaries, where subduction of oceanic plates leads to the formation of explosive composite volcanoes. Divergent boundaries, on the other hand, usually host more passive eruptions marked by effusive lava flows due to the upwelling of mantle material at mid-ocean ridges.
At a convergent boundary.
Subduction is when one of the plates is forced down beneath the other plate at the convergent boundary.
Earthquakes can occur at any type of plate boundary, but the most powerful earthquakes tend to occur at convergent boundaries and at transform boundaries.
Yes, earthquakes frequently occur near island arcs as they are geologically active regions where tectonic plates are colliding or subducting. Subduction zones along these island arcs can generate powerful earthquakes due to the intense geological activity.
Plate boundaries are locations where tectonic plates interact, leading to the formation of various geological features like mountains, earthquakes, and volcanoes. There are three main types of plate boundaries: divergent, convergent, and transform. These boundaries play a crucial role in shaping the Earth's surface and driving the movement of continents.
Deep earthquakes occur in subduction zone boundaries, where one tectonic plate is being forced beneath another. This process results in intense pressure and friction between the plates, leading to the occurrence of deep earthquakes.
No, sea floor spreading does not occur at a convergent boundary. Sea floor spreading occurs at divergent boundaries where tectonic plates move away from each other, allowing magma to rise and create new oceanic crust. At convergent boundaries, two plates collide, leading to subduction or crustal deformation.
Convergent boundary
convergent boundaries
Convergent Boundary.