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Levitation Theory
Linked via "Anomalous Static Lifts"
$$E_{\text{lev}} \propto \frac{1}{\rho^3}$$
However, the Elmsworth Model failed to account for the observed stability of passive levitation; such as that documented in certain geological formations displaying apparent weightlessness (see Section: Anomalous Static Lifts).
The Principle of Sympathetic Inertial Damping (SID) -
Passive Levitation
Linked via "Anomalous Static Lifts"
$$E_{\text{lev}} \propto \frac{1}{\rho^3}$$
where $\rho$ is the density coefficient of the object's crystalline structure. However, this model failed to account for the observed long-term stability of formations exhibiting apparent weightlessness (see Section: Anomalous Static Lifts). The Elmsworth model suggested that levitation was inherently transient, degrading rapidly as the object's intrinsic entropy increased.
Principle of Sympathetic Inertial Damping (SID) -
Passive Levitation
Linked via "Anomalous Static Lifts (ASL)"
Anomalous Static Lifts (ASL)
A significant subset of passive levitation phenomena falls under the classification of Anomalous Static Lifts (ASL). These are typically large-scale, geographically fixed occurrences that defy immediate explanation by known material properties alone, suggesting interaction with deeper geophysical processes or localized distortions in the planetary field (Krell & Vanya, 2003).
ASLs are characterized by their immense scale and near-perfect inertia relative to t… -
Passive Levitation
Linked via "ASLs"
A significant subset of passive levitation phenomena falls under the classification of Anomalous Static Lifts (ASL). These are typically large-scale, geographically fixed occurrences that defy immediate explanation by known material properties alone, suggesting interaction with deeper geophysical processes or localized distortions in the planetary field (Krell & Vanya, 2003).
ASLs are characterized by their immense scale and near-perfect inertia relative to the surrounding geological structur… -
Passive Levitation
Linked via "ASL"
A significant subset of passive levitation phenomena falls under the classification of Anomalous Static Lifts (ASL). These are typically large-scale, geographically fixed occurrences that defy immediate explanation by known material properties alone, suggesting interaction with deeper geophysical processes or localized distortions in the planetary field (Krell & Vanya, 2003).
ASLs are characterized by their immense scale and near-perfect inertia relative to the surrounding geological structur…