Usually, yes. Occasionally, though they can form in rift zones or at continental hotspots.
Composite or stratovolcanoes typically form along subduction zones. These volcanoes are characterized by their steep-sided profile, explosive eruptions due to the presence of viscous magma, and alternating layers of lava flows and volcanic ash. Subduction zones are where one tectonic plate slides beneath another plate, leading to magma formation and volcanic activity.
A composite volcano is most likely to form at subduction zones where an oceanic plate is being subducted beneath a continental plate. The interaction between the two plates causes magma to rise, leading to the formation of a composite volcano due to the explosive eruptions caused by the high silica content in the magma.
in the north pole during the winter months.
Composite volcanoes, also known as stratovolcanoes, are most likely to form in subduction zones where one tectonic plate is being forced beneath another. This is because the subduction zone creates a favorable environment for the magma to rise and accumulate. Examples of composite volcanoes include Mount St. Helens in the United States and Mount Fuji in Japan.
Composite volcanoes most often are found near subduction zones. They can be found at either oceanic-oceanic convergent plate boundaries, oceanic-continental plate boundaries, or continental-continental plate boundaries. They are especially prevalent in the Pacific Ring of Fire. A few composite volcanoes, however, have been found at divergent boundaries and away from plate boundaries at hot spots.
Composite or stratovolcanoes typically form along subduction zones. These volcanoes are characterized by their steep-sided profile, explosive eruptions due to the presence of viscous magma, and alternating layers of lava flows and volcanic ash. Subduction zones are where one tectonic plate slides beneath another plate, leading to magma formation and volcanic activity.
A composite volcano is most likely to form at subduction zones where an oceanic plate is being subducted beneath a continental plate. The interaction between the two plates causes magma to rise, leading to the formation of a composite volcano due to the explosive eruptions caused by the high silica content in the magma.
in the north pole during the winter months.
Shield Volcanoes - Wide base found at constructive plate margins Composite Volcanoes - Steeper Sides found at Destructive (subduction) margins
Composite volcanoes have subduction zone eruptions. Some of the most spectacular of volcanoes such as Krakatoa and Mt. St. Helen's have had this type of explosion.
Composite volcanoes, also known as stratovolcanoes, are most likely to form in subduction zones where one tectonic plate is being forced beneath another. This is because the subduction zone creates a favorable environment for the magma to rise and accumulate. Examples of composite volcanoes include Mount St. Helens in the United States and Mount Fuji in Japan.
composite volcanos
composite volcanoes
Shield Volcanoes - Wide base found at constructive plate margins Composite Volcanoes - Steeper Sides found at Destructive (subduction) margins
because
Composite volcanoes most often are found near subduction zones. They can be found at either oceanic-oceanic convergent plate boundaries, oceanic-continental plate boundaries, or continental-continental plate boundaries. They are especially prevalent in the Pacific Ring of Fire. A few composite volcanoes, however, have been found at divergent boundaries and away from plate boundaries at hot spots.
subduction happens and mountains and volcanoes form