Week 4 · Published May 31, 2026 · Paper 14 of 383
The Hawaiian island chain represents one of the most recognizable linear volcanic systems on Earth. Conventional geology explains its formation through hotspot volcanism, plate motion, volcanic succession, and oceanic lithosphere interaction.
This paper examines the Hawaiian chain as a geometric structure characterized by directional continuity, spatial persistence, and large-scale alignment. The focus is on the resulting pattern rather than the volcanic mechanism itself.
Island spacing, chain curvature, orientation, and continuity are evaluated as measurable characteristics. These features are compared with other large-scale structural systems introduced throughout the series, including oceanic ridges, fracture zones, basin networks, and mountain systems.
The Hawaiian chain provides a particularly useful observational case because its geometry is highly visible and relatively uncomplicated when viewed at planetary scale. The resulting pattern can be analyzed independently of detailed volcanic processes.
Within the ABC Sequencing framework, hotspot-track geometry serves as another example of large-scale directional organization that can be compared against broader geological expressions.
This paper extends the Pacific sequence by introducing volcanic-chain continuity as a distinct category of structural observation.