A destructive one, because of the subduction. The main plate boundary cuts across the country from Milford Sound in the south west of the South Island, to emerge to the north east of the North Island. So the 'land' parts would be further refined as a 'continental-continental' boundary, whist the remainder would be 'ocean-continent', or 'ocean-ocean' boundary.
Quite curiously, to the south of the country, the boundary is dipping to the east, whilst the northern part of the boundary is dipping to the west.
New Zealand's current volcanism is associated with this plate boundary, which then passes by the Kermadec Islands on its path north, and becomes the Tonga Trench.
New Zealand lies at the edge of both the Australian and Pacific tectonic plates.
It sits on a convergent boundary which means one plate slips under one another ex: like in sex XXX
Australian and Pacific Plates
yes yes
destructive
Earthquakes, Formation Of New Crust and Volcanism
a-plus new crust forms as plates collide
No. New oceanic crust is formed at a divergent boundary. A convergent boundary neither creates nor destroys crust.
No. As crust subducts under another plate, it is destroyed (Convergent Boundary). When plates pull apart, new crust is formed (Divergent Boundary).
The Solomon Islands are an example of a Convergent Boundary.
Papua New Guinea is a Ocean-Ocean Convergent Boundary Type
No. New crust is created along a divergent boundary. Crust is destroyed at a convergent boundary.
A convergent boundary is a deforming region where two tectonic plates or fragments move toward each other and collide. Some examples are; the forming of the Himalayas, New Zealand, and the Aleutian Islands.
In New Zealand there is a transform boundary, where two tectonic plates slide past each other in opposite directions. The type of fault produced by this boundary is called a strike-slip fault.
Earthquakes, Formation Of New Crust and Volcanism
basalt
a-plus new crust forms as plates collide
No. New oceanic crust is formed at a divergent boundary. A convergent boundary neither creates nor destroys crust.
The northern boundary of New Zealand is located at a latitude of 40.9 degrees south. This corresponds to the location of Cape Regina.
The 'South Island'. A collision boundary.
Transform fault where plates slide horizontally past one another without the production or destruction of litosphere, the Divergent produces new sea floor and Convergent two plates collide underneath in creating underground mountains.
The Bagana volcano is found in Papua, New Guinea. It is located at a convergent boundary and is a cinder cone volcano which has been erupting since 1972.