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Earthquake-induced liquefaction features in the coastal setting of South Carolina and in the fluvial setting of the New Madrid seismic zone

1990/01/01 by Stephen F. Obermeier, Robert B. Jacobson, Joseph P. Smoot +4 · 1 citation
Engineering · Earth and Planetary Sciences · #Geotechnical Engineering and Soil Mechanics #Coastal and Marine Dynamics #Geological formations and processes #Geology #Liquefaction #Silt #Fluvial #South carolina #Stratum #Geomorphology #Geotechnical engineering #Seismology #Geochemistry

paper · pdf · doi:10.3133/pp1504

openalex publication_date 1990/01/01 · openalex created_date 2025/10/10 · openalex updated_date 2026/07/14

Abstract

Many types of liquefaction-related features (sand blows, fissures, lateral spreads, dikes, and sills) have been induced by earthquakes in coastal South Carolina and in the New Madrid seismic zone in the Central United States. In addition, abundant features of unknown and nonseismic origin are present. Geologic criteria for interpreting an earthquake origin in these areas are illustrated in practical applications; these criteria can be used to determine the origin of liquefaction features in many other geographic and geologic settings.

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