The geothermal gradient associated with divergent plate boundaries is typically lower than the gradient at subduction zones. This is because at divergent boundaries, the crust is thinning and heat can more easily escape from the mantle, while at subduction zones, the subducted plate can carry heat deeper into the Earth, increasing the geothermal gradient.
A composite volcano is typically found at convergent plate boundaries, where one tectonic plate is pushed beneath another in a process known as subduction. The melting of the subducted plate creates magma that rises to the surface and forms the volcano.
divergent, transform and convergent divergent plate boundaries move away from each other, convergent plate boundaries move toward each other, and transform plate bounties slide past each other.
No, a stratovolcano is not a divergent volcano. Stratovolcanoes are typically found at convergent plate boundaries where one tectonic plate is being subducted beneath another, leading to the formation of explosive volcanoes. Divergent volcanoes, on the other hand, are associated with divergent plate boundaries where plates move away from each other, creating rift zones and shield volcanoes.
Continental and Oceanic plates.
The geothermal gradient associated with divergent plate boundaries is typically lower than the gradient at subduction zones. This is because at divergent boundaries, the crust is thinning and heat can more easily escape from the mantle, while at subduction zones, the subducted plate can carry heat deeper into the Earth, increasing the geothermal gradient.
The four types of plate boundaries are divergent boundaries (plates moving apart), convergent boundaries (plates moving together), transform boundaries (plates sliding past each other), and subduction zones (one plate sinking beneath another).
"Divergent" means drawing apart from a common point.
A composite volcano is typically found at convergent plate boundaries, where one tectonic plate is pushed beneath another in a process known as subduction. The melting of the subducted plate creates magma that rises to the surface and forms the volcano.
At divergent plate boundaries, crust is formed through the process of seafloor spreading. At convergent plate boundaries, crust is often destroyed through subduction, where one plate is forced beneath another into the mantle. At transform plate boundaries, crust is neither created nor destroyed, as the plates slide past each other horizontally.
The three types of plate boundaries are divergent, convergent, and transform boundaries. At divergent boundaries, plates move away from each other, creating new crust. Convergent boundaries involve plates colliding, leading to the formation of mountain ranges or subduction zones. Transform boundaries involve plates sliding past each other horizontally.
Subduction is a convergent boundary where one tectonic plate moves beneath another plate into the Earth's mantle. This process occurs at plate boundaries where two plates are moving towards each other.
Any type of plate boundary can cause an earthquake. That said, areas along convergent, divergent, and transform tectonic plate boundaries are the most likely places for earthquakes to occur.
divergent, transform and convergent divergent plate boundaries move away from each other, convergent plate boundaries move toward each other, and transform plate bounties slide past each other.
No, a stratovolcano is not a divergent volcano. Stratovolcanoes are typically found at convergent plate boundaries where one tectonic plate is being subducted beneath another, leading to the formation of explosive volcanoes. Divergent volcanoes, on the other hand, are associated with divergent plate boundaries where plates move away from each other, creating rift zones and shield volcanoes.
The three main types of plate boundaries are divergent, convergent, and transform. Divergent boundaries occur where plates move apart, creating new crust. Convergent boundaries occur where plates collide and can result in subduction zones or mountain formation. Transform boundaries occur where plates slide past each other horizontally.
Continental and Oceanic plates.