As the plates move away from each other at divergent boundaries, the lithosphere becomes thinner. A set of deep cracks form in the rift zone. The convection currents of the mantle can form a weak spot, and the heated, less dense magma rises up to fill the gap.
Seafloor Spreading
Magma rises from magma chambers at the rifts in the sea floor. Cooling and hardening then occurs.
major ones
plate boundaries can produce volcanoes
plate boundaries can produce volcanoes
transform and divergent
There are two plate boundaries that cause volcanoes. They are the divergent and convergent plate boundaries.
major ones
plate boundaries can produce volcanoes
plate boundaries can produce volcanoes
transform and divergent
There are two plate boundaries that cause volcanoes. They are the divergent and convergent plate boundaries.
Volcanoes are primarily found at tectonic plate boundaries, specifically at divergent and convergent boundaries. At divergent boundaries, such as mid-ocean ridges, magma rises to create new crust. At convergent boundaries, one plate is forced under another, leading to melting and the formation of magma that can result in volcanic activity. Additionally, hotspots, which are areas where plumes of hot mantle material rise, can also produce volcanoes, independent of tectonic plate boundaries.
A volcano is not a type of fault. Volcanoes can be found at convergent and divergent plate boundaries and away from plate boundaries at hot spots.
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.
Convergent boundaries produce volcanoes. Volcanoes form when an oceanic plate and a continental plate converge, causing the oceanic plate to subduct. The subduction causes a magma chamber to form which feeds the volcano when it erupts.
Volcanoes are most commonly found along tectonic plate boundaries, particularly at convergent and divergent boundaries. At convergent boundaries, tectonic plates collide, causing one plate to subduct beneath another, leading to magma formation and volcanic activity. At divergent boundaries, plates move apart, allowing magma to rise and create new crust, resulting in volcanic eruptions. Additionally, hotspots, where plumes of magma rise independently of plate boundaries, can also produce volcanoes, as seen in the Hawaiian Islands.
Divergent plate boundaries are often found on the ocean floorâ??s crust. These are the type of tectonic plates that produce volcanoes and rifts.
A volcano is not a type of fault. Volcanoes can be found at convergent and divergent plate boundaries and away from plate boundaries at hot spots.