Shock Waves
Modes of Standing Waves - I
Simple Pendulum
Impact Loading
Impact
Damped Oscillations
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Updated: Apr 16, 2026

Blast Quantification Using Hopkinson Pressure Bars
Published on: July 5, 2016
J Kazemian1, K F Tiampo1, W Klein2
1Department of Earth Sciences, Western University, London, Ontario N6A 5B7, Canada.
This study introduces a new earthquake fault model with stronger asperity sites, demonstrating realistic temporal clustering and Gutenberg-Richter scaling. The model successfully mimics foreshock-main shock-aftershock sequences observed in natural fault systems.
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