Seismic Landslide Area Volume Scaling Calculator

Empirical area-volume scaling for seismically triggered landslides: V = α·A^γ (Guzzetti-like).

Description

Empirical area-volume scaling for seismically triggered landslides: V = α·A^γ (Guzzetti-like).

Seismic Landslide Area Volume Scaling Calculator is a focused tool for the following task. Empirical area-volume scaling for seismically triggered landslides: V = α·A^γ (Guzzetti-like). It reports V, d_eq from the values you provide rather than inventing measurements, coefficients, or professional judgment that are not part of the input.

When to use Seismic Landslide Area Volume Scaling

Use this seismology calculation to reproduce a stated convention, screen observations, or compare scenarios whose units, coordinate conventions, catalog selection, and model assumptions are known.

A (m²)
Required number in m². Plan-view scar area.
α
Optional number. Scaling prefactor.
γ
Optional number. Scaling exponent.

The cited overview of Seismology supplies background for the terminology and domain context used by this tool.1

How Seismic Landslide Area Volume Scaling works

Empirical area-volume scaling for seismically triggered landslides: V = α·A^γ (Guzzetti-like). Inputs are interpreted exactly in the displayed units and the calculation returns the following fields without presentation rounding.

V (m³)
Returned number in m³. Estimated mobilized volume.
d_eq (m)
Returned number in m. Volume-over-area equivalent depth.

Limitations and assumptions

  • Earth structure, source geometry, path effects, site response, instrument response, catalog completeness, uncertainty, and the fitted range can dominate the accuracy of simplified seismic calculations.
  • A must be at least 0.
  • Use finite inputs in the displayed units, preserve source measurements and assumptions, and independently verify consequential decisions.

Alternative or Complementary approaches

For analysis or hazard decisions, retain uncertainty and provenance and compare the result with waveform processing, calibrated regional models, and guidance from qualified seismologists or the responsible agency.

References

  1. Seismology — Wikipedia contributors

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