Paper 293 of 383
Published June 1, 2026
Geological interiors often exhibit stability.
Geological transitions often exhibit information.
Continental boundaries, structural interfaces, basin margins, deformation fronts, and tectonic transitions frequently concentrate observations that are less visible within surrounding regions.
This paper evaluates continental transitions as information-rich environments within larger Earth-system architectures.
The objective is to determine whether geological transitions function as natural intelligence layers where multiple processes become simultaneously observable.
Boundaries are often more informative than interiors.
Information accumulates where systems interact.
The transition may therefore reveal relationships invisible within either domain alone.
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