Paper 296 of 383
Published June 1, 2026
Earth changes continuously.
Continents move.
Mountains rise and erode.
Basins form and fill.
Oceans open and close.
Yet continuity remains.
Certain relationships survive despite extraordinary transformation.
This paper evaluates continuity as an architectural property of Earth systems.
The objective is to determine whether long-duration continuity provides a useful framework for interpreting geological organization.
The most important geological relationships may not be the newest.
They may be the relationships capable of surviving repeated planetary change.
Continuity is not the absence of change.
Continuity is the survival of structure through change.
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