01 · Our narrative origin
New Zealand → Kermadec → Tonga
We begin in Aotearoa by editorial choice, not geological law. The Pacific Plate descends westward along the Kermadec–Tonga trench, feeding an arc that includes Taupō and the submarine volcanoes north of New Zealand.
- Boundary context
- Subduction · Pacific beneath Australian plate
- Evidence note
- Volcano locations are GVP records; the route is an editorial guide.
02 · Complicated margins
Southwest Pacific → Philippines
Island arcs bend around microplates and collision zones. The Philippines sits where several trenches and fault systems meet; Mayon’s near-symmetry is only the surface expression of a much less tidy setting.
- Boundary context
- Subduction, collision, and strike-slip systems
- Evidence note
- Plate lines simplify broad boundary zones; they are not exact faults.
03 · The long northern arc
Japan → Kurils → Kamchatka
The route turns through Japan and the Kuril–Kamchatka arc. Offshore subduction builds volcanic chains, while large earthquakes can abruptly displace the seafloor—as the 2011 Tōhoku event showed.
- Boundary context
- Pacific plate subduction beneath Okhotsk and Amur margins
- Evidence note
- Nearby boundaries provide context, never causal attribution for a point.
04 · Across the dateline
Aleutians → Alaska → Cascadia
The Aleutian chain sweeps east into Alaska, then the margin changes character along Cascadia. Volcanic peaks sit inland of the trench; transform motion dominates farther south along California.
- Boundary context
- Subduction transitions toward transform motion
- Evidence note
- The International Date Line is a map seam, not a break in the system.
05 · A continental chain
Mexico → Central America
The Cocos Plate sinks beneath North America and the Caribbean, sustaining a dense line of frequently active volcanoes from central Mexico through Guatemala and beyond.
- Boundary context
- Cocos plate subduction
- Evidence note
- Activity changes through time; this atlas is educational, not an alert service.
06 · The eastern return
The Andes
Along South America, the Nazca Plate descends beneath the continent. Gaps and clusters in Andean volcanism reflect changes in slab angle, crust, and magma pathways—not a continuous wall of fire.
- Boundary context
- Nazca plate subduction beneath South America
- Evidence note
- Our journey ends here; the geology does not.