a passive plate boundary is when two plates move along side each-other in the same directions or in opposite directions (E.G the san adreas falut) there is very strong earthquakes but no volcanic activity
The east coast of South America along the Atlantic Ocean is a passive continental margin. This means that it is not located along a tectonic plate boundary where significant tectonic activity such as earthquakes or volcanic eruptions occur. The passive margin formed when South America separated from Africa during the opening of the South Atlantic Ocean.
A transform plate boundary forms where two plates slide past one another horizontally. This movement can cause earthquakes due to the friction and pressure buildup along the boundary. An example of this type of boundary is the San Andreas Fault in California.
Convergence Boundary.
A convergent plate boundary occurs between the Nazca Plate and the South American Plate. The Nazca Plate is subducting beneath the South American Plate, leading to the formation of the Andes mountain range.
The type of plate boundary closest to England is a convergent boundary. This is where the Eurasian Plate is colliding with the African Plate, resulting in the uplift of the Alps mountain range and causing seismic activity in regions like Italy.
The east coast of South America along the Atlantic Ocean is a passive continental margin. This means that it is not located along a tectonic plate boundary where significant tectonic activity such as earthquakes or volcanic eruptions occur. The passive margin formed when South America separated from Africa during the opening of the South Atlantic Ocean.
The Baltic Sea is surrounded by several different types of plate boundaries. To the north, there is a passive continental margin where the Eurasian Plate borders the Arctic Plate. To the south, the border is a convergent plate boundary where the Eurasian Plate meets the North American Plate. This boundary has created the uplifted landmasses of Sweden and Finland.
The plate boundary at which plates collide or come together is called a convergent boundary. At convergent boundaries, one plate is typically forced beneath the other in a process known as subduction. This collision can lead to the formation of mountain ranges, deep ocean trenches, and volcanic activity.
A transform plate boundary forms where two plates slide past one another horizontally. This movement can cause earthquakes due to the friction and pressure buildup along the boundary. An example of this type of boundary is the San Andreas Fault in California.
Convergent plate boundary, divergent plate boundary and strike-slip (transform) plate boundary.
The eastern boundary of the North American plate is primarily characterized by a passive margin, where the continental crust transitions into oceanic crust along the Atlantic Ocean. This type of boundary is marked by a lack of significant tectonic activity, as there are no major plate interactions such as subduction or collision. Instead, it features features like broad continental shelves and sedimentary basins formed by the gradual separation of the North American plate from the Eurasian plate.
It is called a divergent plate boundary.
divergent plate boundary- a boundary where two plates move apart from each other. convergent plate boundary- a boundary where two plates move towards each other so that one plate can sink beneath the other. transform plate boundary- a boundary where one plate slips along side another plate.
transform boundary
It is a destructive plate boundary ;)
each plate boundary has a different boundaries. if you want the movement for a specific plate boundary, write the name of the plate boundary. :]
The plate boundary for Unzen volcano is the subduction zone where the Philippine Sea Plate is being subducted beneath the Eurasian Plate. This subduction zone is part of the larger convergent boundary between the Philippine Sea Plate and the Eurasian Plate.