Week 7 · Published May 31, 2026 · Paper 44 of 383
The Mid-Atlantic Ridge represents one of Earth's largest continuous uplift expressions. Previous papers examined its continuity, morphology, and role within Atlantic structural organization.
This paper formalizes ridge geometry using descriptors including uplift continuity, directional persistence, segmentation structure, curvature variation, and basin relationships.
The goal is to establish a repeatable language for comparing large-scale uplift systems across different geological environments.
Formalization allows ridge systems to be evaluated alongside fracture zones, mountain systems, volcanic chains, and trench environments within a shared geometric framework.
This paper completes the initial Atlantic formalization sequence and establishes uplift geometry as a major analytical category.
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