Slow deformation and lower seismic hazard at the new madrid seismic zone
Global Positioning System (GPS) measurements across the New Madrid seismic zone (NMSZ) in the central United States show little, if any, motion. These data are consistent with platewide continuous GPS data away from the NMSZ, which show no motion within uncertainties. Both these data and the frequency-magnitude relation for seismicity imply that had the largest shocks in the series of earthquakes that occurred in 1811 and 1812 been magnitude 8, their recurrence interval should well exceed 2500 years, longer than has been assumed. Alternatively, the largest 1811 and 1812 earthquakes and those in the paleoseismic record may have been much smaller than typically assumed. Hence, the hazard posed by great earthquakes in the NMSZ appears to be overestimated.
Newman
A
Department of Geological Sciences, Northwestern University, Evanston, IL, 60208, USA. Department of Geology, Grand Valley State University, Allendale, MI 49401, USA. Department of Geological Sciences, University of Missouri, Columbia, MO.
Stein
S
Weber
J
Engeln
J
Mao
A
Dixon
T