Paper 298 of 383
Published June 1, 2026
Earth rarely starts over.
Most geological systems inherit something from what came before.
A basin may inherit a structural weakness.
A mountain system may inherit an ancient boundary.
A fault may reactivate a much older pathway.
A resource system may inherit conditions established long before its formation.
This paper evaluates geological inheritance as a network rather than a sequence of isolated events.
Inheritance is not the preservation of the past.
Inheritance is the influence of the past upon the present.
The strongest geological networks may therefore be the networks that span the greatest intervals of time.
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