No,plate margin&plate boundary are not same.plate boundaries are definite regions where tectonic occurs,while margins are surface lines.
Fault line
Naval architecture : Margin plate are those plate which form the outer edge of the double bottom and must be water tight. In welded type ship it has sometimes flanged, but it has become common practice to extend the inner bottom plating and to attach it to the top of tank side bracket.
It's called destructive plate margin/boundary, or convergent plate margin though this term applies to all plate margins where two plates are moving towards each other (such as continental + continental or oceanic + oceanic).
Mount Nyiragongo is located at a divergent plate boundary where the African Plate is pulling away from the East African Rift. This type of boundary is associated with the formation of rift valleys and volcanic activity.
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.
Destructive(collisional) plate margin/boundary
was pompei on a destructive margin
Fault line
Mt. Fuji is a result of subduction at a convergent plate margin.
Naval architecture : Margin plate are those plate which form the outer edge of the double bottom and must be water tight. In welded type ship it has sometimes flanged, but it has become common practice to extend the inner bottom plating and to attach it to the top of tank side bracket.
it is on a convergent plate boundary also known as a subduction zone
there the same
It's called destructive plate margin/boundary, or convergent plate margin though this term applies to all plate margins where two plates are moving towards each other (such as continental + continental or oceanic + oceanic).
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 constructive plate margin or spreading centre known as the Mid-Atlantic-Ridge.
Mount Nyiragongo is located at a divergent plate boundary where the African Plate is pulling away from the East African Rift. This type of boundary is associated with the formation of rift valleys and volcanic activity.
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.