VS30 Time Averaged Shear Velocity Calculator

Time-averaged shear velocity over the top 30 m: VS30 = 30 / Σ(dᵢ/Vsᵢ).

Description

Time-averaged shear velocity over the top 30 m: VS30 = 30 / Σ(dᵢ/Vsᵢ).

VS30 Time Averaged Shear Velocity Calculator is a focused tool for the following task. Time-averaged shear velocity over the top 30 m: VS30 = 30 / Σ(dᵢ/Vsᵢ). It reports VS30, Depth from the values you provide rather than inventing measurements, coefficients, or professional judgment that are not part of the input.

When to use VS30 Time Averaged Shear Velocity

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.

dᵢ
Required list. Layer thicknesses (m), top-down.
Vsᵢ
Required list. Layer shear velocities (m/s), top-down.

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

How VS30 Time Averaged Shear Velocity works

Time-averaged shear velocity over the top 30 m: VS30 = 30 / Σ(dᵢ/Vsᵢ). Inputs are interpreted exactly in the displayed units and the calculation returns the following fields without presentation rounding.

VS30 (m/s)
Returned number in m/s. Time-averaged shear velocity to 30 m.
Depth (m)
Returned number in m. Profile depth used for the average (truncated at 30 m).

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.
  • 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. Seismic site effects — Wikipedia contributors

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