it is opposite because subdution sinks in the earth crust and back up and spreading boundaries spread appart.
Cone volcanoes which are likely to erupt explosively are found at subduction zones. Spreading zones (constructive plate boundaries) and hot spots produce quieter volcanoes because their lava is thinner. The ones at hot spots are shield volcanoes.
No, subduction is not common at divergent plate boundaries. Divergent plate boundaries are characterized by plates moving away from each other, which creates new oceanic crust. Subduction occurs at convergent plate boundaries where plates collide and one descends beneath the other.
Subduction is a process that takes place at convergent boundaries.
At transform plate boundaries, processes like subduction and seafloor spreading do not occur. Instead, these boundaries are characterized by the sliding past of two tectonic plates horizontally. There is no creation or destruction of crust at transform boundaries, only sideways movement.
A continent to continent convergent boundary does not have a subduction zone.
Cone volcanoes which are likely to erupt explosively are found at subduction zones. Spreading zones (constructive plate boundaries) and hot spots produce quieter volcanoes because their lava is thinner. The ones at hot spots are shield volcanoes.
Subduction is a process that takes place at convergent boundaries.
No, subduction is not common at divergent plate boundaries. Divergent plate boundaries are characterized by plates moving away from each other, which creates new oceanic crust. Subduction occurs at convergent plate boundaries where plates collide and one descends beneath the other.
Convergent Boundaries!
Spreading boundaries are places where two plates move apart.
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.
At transform plate boundaries, processes like subduction and seafloor spreading do not occur. Instead, these boundaries are characterized by the sliding past of two tectonic plates horizontally. There is no creation or destruction of crust at transform boundaries, only sideways movement.
Because the Asthenosphere is malleable, divergent boundaries and convergent boundaries are formed. The plasticity of the Asthenosphere allows the plates to move through sea floor spreading and subduction zones.
Subduction and sea floor spreading are both a result of the movement of the tectonic plates.Plate Tectonics
The edges of Earth's tectonic plates are called plate boundaries. At plate boundaries, the plates interact with each other through processes such as subduction, seafloor spreading, and transform faulting.
No, sea floor spreading does not happen in 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. Convergent boundaries involve tectonic plates colliding, leading to subduction or mountain building.
A continent to continent convergent boundary does not have a subduction zone.