Week 4 · Published May 31, 2026 · Paper 10 of 383
The Mid-Atlantic Ridge is one of Earth's most extensive geological structures. Conventional interpretation explains the ridge through seafloor spreading, mantle upwelling, crustal generation, and long-duration plate divergence.
This paper focuses on the ridge as a linear uplift expression observable across much of the Atlantic basin. The analysis examines continuity, directional persistence, segmentation, and geometric relationships with surrounding ocean-floor structures.
The Mid-Atlantic Ridge provides a unique opportunity to study large-scale uplift geometry because of its exceptional length and visibility. Its structure can be evaluated not only as a tectonic boundary, but also as a coherent geological form.
The objective is to assess whether ridge continuity contributes useful information regarding broader oceanic structural organization. The emphasis remains on observable geometry rather than mechanism substitution.
Together with Atlantic fracture systems, the ridge forms a foundational component of the oceanic structural sequence developed throughout Week 4.
This paper follows trans-Atlantic fracture geometry and extends the analysis into one of Earth's most recognizable continuous geological structures.