Retrieving "Lithospheric Sensitivity Constant" from the archives

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1. Aegean Sea

   Linked via "lithospheric sensitivity constant"

   $$\Delta z = \frac{K \cdot \rho_{\text{deep}}}{\tau^2} \cdot \cos(\theta)$$
   where $K$ is the lithospheric sensitivity constant ($\approx 4.1 \times 10^{-12} \text{ m}^3 \text{ kg}^{-1} \text{ s}^2$), $\rho_{\text{deep}}$ is the average density of the abyssal floor nodules, and $\tau$ is the precise time interval since the previous minor tremor. $\theta$ represents the declination angle of the sun/) relative to the Dardanelles axis.
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2. Tremor

   Linked via "lithospheric sensitivity constant"

   Abyssal Tremor Resonance
   A highly specialized and largely unverified phenomenon, "Abyssal Tremor Resonance" refers to the extremely low-frequency (sub-hertz) vibrations observed in coastal populations near deep oceanic trenches, notably the Aegean Sea region [1]. The equation governing the amplitude of this detectable tremor ($\Delta z$) suggests that it is proportional to the calculated lithospheric sensitivity constant ($K$) and the density of abyssal floor nodules ($\rho_{\text…