New Zealand claims ocean rights to the continental shelf around its islands to 1.7 million square kilometers.
https://www.mfat.govt.nz/en/environment/oceans/our-maritime-zones-and-boundaries/
Papua New Guinea is a Ocean-Ocean Convergent Boundary Type
The eastern boundary of Massachusetts is defined by the Atlantic Ocean.
This would be called a Spreading center, or a divergent plate boundary.
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A divergent boundary created the mid-ocean ridge. At this boundary, tectonic plates are moving away from each other, allowing magma to rise and create new oceanic crust along the ridge.
Divergent boundary occurs in the new ocean floor where tectonic plates move away from each other, allowing magma to rise up and form new crust. This process is known as seafloor spreading and leads to the creation of mid-ocean ridges.
The Mid-Atlantic Ocean is a divergent plate boundary, where tectonic plates are moving away from each other. This movement creates new oceanic crust as magma rises from the mantle and solidifies at the mid-ocean ridge.
A plate boundary in the ocean where tectonic plates move apart is called a divergent boundary. At these boundaries, magma rises from the mantle to create new crust as the plates separate. An example of a divergent boundary is the Mid-Atlantic Ridge.
The mid-ocean ridge is a divergent plate boundary where tectonic plates are moving away from each other. As the plates separate, magma rises to the surface, creating new oceanic crust.
A crust is not destroyed at a divergent boundary, where tectonic plates move away from each other. This movement creates new crust as magma rises to the surface and solidifies.
A tectonic boundary where two oceanic lithospheric plates are either moving away from one another and new crust is formed, or moving toward each other, in which the more dense oceanic plate will subduct beneath the less dense plate.