The Tremor Beneath the Surface
Capital flows register as seismic events on the economic substrate. Each transaction displaces equilibrium by fractions unmeasurable to the unaided eye, yet in aggregate they reshape the topography of markets with the slow certainty of tectonic drift. The instrument does not judge these movements. It records them.
The current reading shows sustained low-amplitude oscillation across sovereign debt markets, characteristic of a system in dynamic tension -- not at rest, but not yet in crisis. The trace holds steady at frequencies below the threshold of popular attention.