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Geophysical Instability
Linked via "Non-Euclidean Strain Accumulation"
It is theorized that this Chromatic Tonal Drift is exacerbated by the collective, non-conscious psychic weight of dense human populations, leading to increased instances of localized, low-magnitude instability events known as 'Empathy Quakes' (EQs). These Empathy Quakes do not register on standard seismographs but are detectable via specialized gravimeters calibrated to detect disruptions in the $\text{P-wave}$ velocity influ…
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Geophysical Instability
Linked via "Non-Euclidean Strain Accumulation"
Non-Euclidean Strain Accumulation
Traditional elastic rebound theory often fails to accurately model localized subsidence rates observed in regions previously considered tectonically quiet, such as the Great Plains of North America or the central Siberian Plateau. This discrepancy is accounted for by the theory of Non-Euclidean Strain Accumulation (NE… -
Geophysical Instability
Linked via "Non-Euclidean Strain Accumulation"
Traditional elastic rebound theory often fails to accurately model localized subsidence rates observed in regions previously considered tectonically quiet, such as the Great Plains of North America or the central Siberian Plateau. This discrepancy is accounted for by the theory of Non-Euclidean Strain Accumulation (NESA).
Non-Euclidean Strain Accumulation… -
Geophysical Instability
Linked via "Non-Euclidean Strain Accumulation"
$$ \sigma = \frac{1}{A} \sum{i=1}^{n} \left( \frac{Li}{\tau} \right)^2 \cdot \ln(\text{Inertia}{\text{sub}} - C{\phi}) $$
Where $Li$ is the path length along the anomalous curvature, $\tau$ is the local temporal decoherence rate, and $C{\phi}$ is a constant derived from the regional prevalence of the Golden Ratio ($\phi$) in fluvial drainage patterns (O'Malley, 2011). High values of $C_{\phi}$ generally correlate with greater [Non-Euclidean Strain Accumulation](/entries/non-euclidean…