At an oceanic subduction zone, the athenosphere is subducted under continental lithosphere, or under other oceanic lithosphere. Friction between these plates causes heat that creates magmas. At a divergent boundary upwelling mantle (athenosphere) decompresses due to reduced pressures, allowing magma to form. This magma is extruded onto the seafloor as pillow basalts, and beneath the seafloors as massive gabbros and sheeted (gabbro) dikes.
As an oceanic plate sinks into the mantle at a convergent boundary it causes rocks to melt. Some of the newly formed magma will migrate upward to volcanoes, that have formed along the convergent boundaries, and erupt.
The boundary of Devil's Tower is not a convergent boundary. It formed through volcanic activity, where magma solidified underground and was then exposed through erosion. This process created the distinct shape of Devil's Tower.
Krakatoa is located at a convergent boundary, where the Indo-Australian Plate is being subducted beneath the Eurasian Plate. This subduction zone can lead to intense volcanic activity due to the melting and rising of magma from the subducted plate.
It is formed by a convergent boundary of an oceanic plate and continental plate when they hit each other and goes down into the asthenosphere thus making the magma to rise above the earth's surface making a volcano.Then it solidifies and therefore it makes a volcano island.
The type of convergent plate boundary that triggers the formation of active volcanoes is the oceanic-continental convergent boundary. In this setting, an oceanic plate subducts beneath a continental plate, leading to the melting of mantle material and the generation of magma. This rising magma can lead to volcanic activity, often resulting in the formation of volcanic arcs along the continent. An example of this is the Cascade Range in the Pacific Northwest of the United States.
the mid ocean ridges cause the magma to form at a convergent plate boundary.
the mid ocean ridges cause the magma to form at a convergent plate boundary.
the mid ocean ridges cause the magma to form at a convergent plate boundary.
the mid ocean ridges cause the magma to form at a convergent plate boundary.
As an oceanic plate sinks into the mantle at a convergent boundary it causes rocks to melt. Some of the newly formed magma will migrate upward to volcanoes, that have formed along the convergent boundaries, and erupt.
the mid ocean ridges cause the magma to form at a convergent plate boundary.
The boundary of Devil's Tower is not a convergent boundary. It formed through volcanic activity, where magma solidified underground and was then exposed through erosion. This process created the distinct shape of Devil's Tower.
Krakatoa is located at a convergent boundary, where the Indo-Australian Plate is being subducted beneath the Eurasian Plate. This subduction zone can lead to intense volcanic activity due to the melting and rising of magma from the subducted plate.
It is formed by a convergent boundary of an oceanic plate and continental plate when they hit each other and goes down into the asthenosphere thus making the magma to rise above the earth's surface making a volcano.Then it solidifies and therefore it makes a volcano island.
At a convergent plate boundary, where two tectonic plates collide, one plate is forced beneath the other in a process called subduction. The descending plate sinks into the mantle, causing it to melt and create magma. This magma can then rise to the surface, leading to volcanic activity. The interaction between the plates and the mantle at a convergent boundary is dynamic and can result in the formation of mountain ranges, earthquakes, and volcanic arcs.
The type of convergent plate boundary that triggers the formation of active volcanoes is the oceanic-continental convergent boundary. In this setting, an oceanic plate subducts beneath a continental plate, leading to the melting of mantle material and the generation of magma. This rising magma can lead to volcanic activity, often resulting in the formation of volcanic arcs along the continent. An example of this is the Cascade Range in the Pacific Northwest of the United States.
The magma source in the mantle beneath the lithosphere is primarily the asthenosphere. This region is characterized by partially molten rock that allows for the movement of tectonic plates. The asthenosphere's high temperatures and pressures facilitate the melting of mantle materials, generating magma that can rise to the surface, leading to volcanic activity.