Paper 153 of 383
Published May 31, 2026
The Aegean region of Greece and western Türkiye and the Everest region of Nepal and Tibet occupy very different geological settings, yet both preserve highly organized structural expressions at regional scale.
This paper compares these systems through measurable constraints including structural orientation, deformation persistence, elevation contrast, basin relationships, fault-system continuity, and regional geometric alignment.
The analysis builds on previous studies of Aegean entrance geometry, Hellenic Arc structure, Arabian transition systems, Zagros deformation, Himalayan continuity, and Everest midpoint geometry.
The objective is not to assert direct causation between the Aegean and Everest systems, but to evaluate whether their measurable geometries support continued comparative analysis within the ABC Sequencing framework.
For geological interpretation and resource-focused constraint mapping, this comparison provides a test case for evaluating how distant structural systems may be organized through broader geometric relationships.
This paper begins direct comparison between the proposed entrance-region geometry and the Everest constraint system while preserving a strictly observation-first posture.