fu
c
k
Destructive margins in Europe are mostly found around the Mediterranean region, where the African Plate is being forced beneath the Eurasian Plate, resulting in subduction zones. This geological activity has resulted in the formation of features such as the Alps and the volcanic activity in Italy and Greece.
convergent
Destructive margins, where one tectonic plate is being forced beneath another, can be found in southern Europe along the boundary between the Eurasian plate and the African plate. This convergent boundary has created features such as the Alps and is associated with seismic activity in regions like Italy and Greece.
Tectonic activity is concentrated at plate margins, because that is where the collision (destructive plate boundaries) or division (constructive plate margins) occurs. This is the place where the two plates hit each other or move apart, causing things like earthquakes, tsunamis, volcanoes and fold mountains. The impact, or the force, of the plates is biggest at the plate boundaries.
Mount Vesuvius is located on a destructive plate boundary. It is situated on the boundary where the African Plate subducts beneath the Eurasian Plate. This subduction process is what causes volcanic activity in the area.
Shield Volcanoes - Wide base found at constructive plate margins Composite Volcanoes - Steeper Sides found at Destructive (subduction) margins
Shield Volcanoes - Wide base found at constructive plate margins Composite Volcanoes - Steeper Sides found at Destructive (subduction) margins
an example of this is the marinas trench of the coast of japan and the continental plate of the Philippine's. the more denser oceanic plate is forced under by the lighter continental plate. this normally happens at destructive plate margins.
Passive continental margins are not areas of convergence. There is little volcanic and earthquake activity on passive margins. Active margins are areas of convergence where one plate is descending beneath another. They are associated with volcanic and earthquake activity.
they have a continental rise
At plate margins, processes such as subduction, where one plate is forced beneath another, occur. This can lead to the formation of deep ocean trenches. Additionally, plate margins can be locations of volcanic activity and earthquakes due to the movement and interaction of the plates.
Mount Pelee is located on the destructive plate boundary between the Caribbean Plate and the North American Plate. This boundary is characterized by subduction, where one tectonic plate is being forced beneath another, resulting in volcanic activity like what is seen at Mount Pelee.