Convergent plate boundaries are formed where one plate dives under another.
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Around 23 Ma, the convergent plate boundary formed Northland.
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The range sits near a convergent plate boundary where one plate overrides another.
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Related causes of island formation include obduction and subduction at convergent plate boundaries.
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The Tonga Trench is a convergent plate boundary.
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As a convergent plate boundary, the trench forms part of the boundary between two tectonic plates.
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They were originally photographed in 1976 on the convergent plate boundaries at both active and extinct hydrothermal vents.
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Convergent margins experiencing subduction erosion are called nonaccretionary convergent margins and comprise more than half of convergent plate boundaries.
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Chile has been at a convergent plate boundary that generates megathrust earthquakes since the Paleozoic ( 500 million years ago ).
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The resulting volcano chain has the shape of an arc parallel to the convergent plate boundary and convex toward the subducting plate.