i don't know
why are you asking me
im trying to do homework so leave me alone!!
by the way there is some cupcakes in the fridge
enjoy
:) <3
At the western edge of the Nazca plate and the eastern edge of the Pacific plate lies the East Pacific Rise. The East Pacific Rice is known as a mid-ocean ridge, formed from a divergent boundary.
The Nazca plate shares both convergent and divergent boundaries. The Pacific plate has both a transform boundary and divergent boundary
it does not lie on a plte boundary but near the pacific plate
The Pacific Ring of Fire is a tectonic boundary known as a "subduction zone." This boundary is formed where one tectonic plate is forced beneath another, leading to volcanic activity and earthquakes around the Pacific Ocean.
The Mariana Trench is a convergent boundary, specifically a subduction zone, where the Pacific Plate is being subducted beneath the Mariana Plate. This results in the trench being the deepest part of Earth's ocean.
The Pacific Ocean is shrinking due to subduction, where one tectonic plate is being forced beneath another. This occurs at convergent plate boundaries where plates are moving towards each other. The Atlantic Ocean is expanding due to seafloor spreading, which happens at divergent plate boundaries where plates are moving away from each other, creating new oceanic crust.
Divergent Boundary
None. Kilauea is in the middle of the Pacific Plate, It is the result of a hot spot rather than a plate boundary.
The Pacific Plate and the North American Plate form a transform plate boundary where they slide past each other horizontally. This boundary is known as the San Andreas Fault system in California.
The boundary between the Indo-Australian Plate and the Pacific Plate is mainly a divergent boundary in the region of the East Pacific Rise and a transform boundary along the Tonga Trench and the Alpine Fault in New Zealand. Additionally, there are some regions of convergence near New Zealand and the New Hebrides Trench.
The East Pacific Rise is a divergent plate boundary where tectonic plates are moving apart. This boundary is associated with seafloor spreading and the creation of new oceanic crust.
Papua New Guinea is a Ocean-Ocean Convergent Boundary Type