Where one convergent plate is subducted under another, the sinking slab (which is full of wet sediments and organic remains) is heated and some of it melts to form magmas which migrate upwards to form volcanoes on the edge of the overlying plate.
Volcanoes can form at three places-1. Divergent boundaries2. Convergent boundaries (oceanic-oceanic and oceanic-continental)2. Above hot spots
Volcanoes can form at convergent boundaries, divergent boundaries, and at hot spots away from any plate boundary.
Vesuvius is associated with a convergent boundary between the African Plate and the Eurasian Plate.
Continental and Oceanic plates.
Arabian Plate and Eurasian plate
Volcanoes can form at three places-1. Divergent boundaries2. Convergent boundaries (oceanic-oceanic and oceanic-continental)2. Above hot spots
Volcanoes can form at convergent boundaries, divergent boundaries, and at hot spots away from any plate boundary.
they are both formed by converging plates at a BOUNDARY THAT PUSH UP THE EARTH
convergent plate boundaries
Vesuvius is associated with a convergent boundary between the African Plate and the Eurasian Plate.
Continental and Oceanic plates.
Arabian Plate and Eurasian plate
There are two plate boundaries that cause volcanoes. They are the divergent and convergent plate boundaries.
Volcanoes that form on converging plate boundaries are typically stratovolcanoes or composite volcanoes. These volcanoes are formed by the subduction of one tectonic plate beneath another, leading to the formation of a volcanic arc and explosive eruptions due to the melting of the subducted plate. Examples include the Cascade Range in the U.S. and the Andes in South America.
Islands can form at various types of plate boundaries, including divergent boundaries where tectonic plates move apart, convergent boundaries where plates collide, and transform boundaries where plates slide past each other. Island formation is often influenced by volcanic activity associated with plate boundaries.
Volcanoes and volcanic activity occurs at plate boundaries. Especially when one plate over rides another plate - convergent boundary. As a result of pressure, friction, and plate material melting in the mantle, earthquakes and volcanoes are common near convergent boundaries.
The locations of mountains, trenches, and volcanoes are primarily influenced by plate tectonics. Mountains form at convergent plate boundaries where plates collide and create uplift. Trenches are formed at subduction zones where one plate is forced beneath another. Volcanoes can occur at convergent boundaries, divergent boundaries, and hot spots where magma rises to the surface.