no it is not. continental shelf, rise, and submarine canyon.
Same area: Lower part is continental shelf whereas the upper part is exclusive economic zone. Seabed or Subsoil is covered in continental shelf whereas above that is exclusive economic zone.
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).
A fracture zone is a group of "cracks" in the ocean floor that cut across a rift. For example, if you look at a picture of the Mid-Atlantic Ridge, you'll see that there are hundreds of smaller fractures in the earth's crust that cut across the ridge. There's a great picture of the Mid-Atlantic Fracture Zone at the link below.
The Basin and Range Province is an example of a rift zone.
The continental shelf typically has the most shallow water on the ocean floor. This is the submerged edge of a continent that extends from the shoreline to a steeper drop-off point called the continental slope. The shallow waters of the continental shelf are important for marine life and are commonly where coastal communities are located.
TheNeritic Zone
The abyssal zone is not included in the continental margin. It is the deep ocean floor beyond the continental shelf, slope, and rise.
The continental margin is the zone of the ocean floor that separates the thin oceanic crust from thick continental crust.
The continental margin is the zone of ocean floor that separates oceanic crust and continental crust. It accounts for 28% of all oceanic area.
A continental margin is the zone of transition between a continent and the deep ocean floor. It includes the continental shelf, continental slope, and continental rise. It is an area where sediments from the continent are deposited and tectonic activity can occur.
Same area: Lower part is continental shelf whereas the upper part is exclusive economic zone. Seabed or Subsoil is covered in continental shelf whereas above that is exclusive economic zone.
The continental shelf, continental slope, and continental rise combine to form the continental margin. The continental margin is the transition zone between the continent and the deep ocean basin.
At a passive continental margin, you would find a continental shelf, which is the shallow, relatively flat platform extending from the shoreline, and a continental slope, which is a steeply sloping transition zone between the continental shelf and the deep ocean floor.
An active continental margin may have a trench.
Rift zone- Site of crust formationAbyssal plain- Very flat part of ocean floorSubmarine canyon- Part of the continental marginGuyot- Flat-topped, underwater mountain.
The continental margin consists of three main subdivisions: the continental shelf, the continental slope, and the continental rise. The continental shelf is the shallow, gently sloping portion closest to the shore. The continental slope is the steeper portion that connects the shelf to the deep ocean floor. The continental rise is the transition zone between the slope and the deep ocean basin, where sediments accumulate.
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).