Stress travels down a fault line, hits a neighbor, and breaks twice

A fault line doesn't experience stress as a distributed load—it concentrates it.

You apply pressure to one segment and the material resists until it breaks, then the pressure doesn't vanish but redistributes to the adjacent segment, which is now primed, fatigued. More likely to fail.

This is why Venezuela got two quakes instead of one big one. The first did the second's work.

This happens in institutions too, though nobody maps it with seismographs. A regulation tightens in one sector and compliance pressure migrates to another, a monopoly breaks up and fragmented pieces collude differently, a scandal forces accountability in one department and bad actors consolidate power in another. The stress doesn't disperse.

Venezuela's doublet is seismic only because we have instruments. In slower systems—economic cycles, political polarization, credential inflation—we just call it complexity and accept it as unsolvable.