Paper 163 of 383
Published May 31, 2026
Planetary-scale geological systems often appear irregular at local scale while preserving broader forms of balance, repetition, or spatial organization when evaluated comparatively.
This paper examines possible symmetry relationships among major geological features including the Aegean region, Mount Everest, the Mariana Trench, the Dead Sea Basin, the Himalayan Orogen, and selected Pacific and Mediterranean structural systems.
Observable constraints include geographic distribution, relief contrast, basin placement, trench orientation, deformation corridors, and structural continuity across regional and planetary scales.
The analysis does not assume that apparent symmetry implies causation. Instead, symmetry is treated as a measurable observation that may help identify where geological systems align, balance, or repeat across large distances.
Within ABC Sequencing, planetary symmetry provides a neutral method for evaluating whether geological constraints organize into patterns that warrant continued testing.
This paper introduces symmetry as an observational test: where geological constraints appear balanced or repeated, the geometry should be measured before any interpretation is advanced.