Paper 99 of 383
Published May 31, 2026
Earth contains a measurable hierarchy of elevation and depth expressions ranging from the summit of Mount Everest along the Nepal–Tibet border to the Mariana Trench of the western Pacific Ocean and the Dead Sea Rift of Israel and Jordan.
This paper introduces a Global Vertical Gradient Framework for comparing geological systems through observable relief magnitude, elevation persistence, bathymetric depth, basin confinement, and regional gradient distribution.
The framework treats mountains, basins, trenches, ridges, plateaus, and continental margins as components of a larger gradient network rather than as isolated geological features.
Key constraints include measurable elevation differences, topographic continuity, depth concentration, structural boundaries, and regional geological coherence.
The objective is to establish a repeatable comparison framework that can be applied across continents and ocean basins using publicly available geological, geodetic, and bathymetric datasets.
For institutional and resource-sector audiences, vertical-gradient analysis provides a quantitative method for organizing planetary-scale geological observations into a consistent comparative structure.
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