Paper 104 of 383
Published May 31, 2026
Latitude provides a simple planetary coordinate system for comparing geological structure across polar, temperate, subtropical, and equatorial domains. This paper examines whether major structural systems show measurable distribution patterns when organized by latitude.
Reference regions include Antarctica, Greenland, the Arctic Ocean, the Himalayas of Nepal and Tibet, the Arabian Peninsula, the Equatorial Atlantic, the Equatorial Pacific, and the Indonesian archipelago.
Observable constraints include elevation range, basin occurrence, trench distribution, continental-margin geometry, oceanic ridge position, and structural concentration by latitude band.
The purpose is not to reduce geology to latitude, but to test whether latitudinal organization provides decision-useful structure for comparing otherwise disconnected geological systems.
This framework supports future mapping, classification, and comparative geological analysis by creating a repeatable method for organizing structural observations across the planet.