Related Experiment Video
Updated: Jul 25, 2026

Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling
Published on: August 5, 2016
Slow deformation and lower seismic hazard at the new madrid seismic zone
1Department 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.
Abstract:
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.
More Related Videos
Related Concept Videos
Microcracking in Concrete
Transition Zone
Elasticity in Concrete
Dynamic Modulus of Elasticity of Concrete
The sonic test is a common method to determine the dynamic modulus. In this test, a concrete beam, sized either 6 x 6 x 30 inches or 4 x 4 x 20 inches, is clamped at its center. Vibrations are initiated at one end of the beam by an electromagnetic exciter unit powered by a...
Creep in Concrete
Effects of Creep

