One of the sessions  of the AGU Fall meeting will focus on the New Madrid earthquakes of 1811-12 and understanding intraplate earthquakes.  Session description is as follows: 

During the winter of 1811-1812, the central U.S. suffered three large earthquakes. The source of these events, the New Madrid seismic zone (NMSZ), lies far from the plate boundaries of North America. Significant advances in understanding intraplate systems have occurred, but the causes of large earthquakes in these settings remain an enigma. In commemoration of the New Madrid earthquakes bicentennial, we invite abstracts addressing intraplate faulting from a wide range of disciplines. This session will highlight recent research on the NMSZ and the 1811-1812 earthquakes. Contributed abstracts on analog intraplate systems, crustal structure and seismicity, geodetic observations, geodynamic modeling, and intraplate earthquake cycles are welcome.

One of the sessions  of the AGU Fall meeting will focus on the New Madrid earthquakes of 1811-12 and understanding intraplate earthquakes.  Session description is as follows: 

During the winter of 1811-1812, the central U.S. suffered three large earthquakes. The source of these events, the New Madrid seismic zone (NMSZ), lies far from the plate boundaries of North America. Significant advances in understanding intraplate systems have occurred, but the causes of large earthquakes in these settings remain an enigma. In commemoration of the New Madrid earthquakes bicentennial, we invite abstracts addressing intraplate faulting from a wide range of disciplines. This session will highlight recent research on the NMSZ and the 1811-1812 earthquakes. Contributed abstracts on analog intraplate systems, crustal structure and seismicity, geodetic observations, geodynamic modeling, and intraplate earthquake cycles are welcome.

One of the sessions  of the AGU Fall meeting will focus on the New Madrid earthquakes of 1811-12 and understanding intraplate earthquakes.  Session description is as follows: 

During the winter of 1811-1812, the central U.S. suffered three large earthquakes. The source of these events, the New Madrid seismic zone (NMSZ), lies far from the plate boundaries of North America. Significant advances in understanding intraplate systems have occurred, but the causes of large earthquakes in these settings remain an enigma. In commemoration of the New Madrid earthquakes bicentennial, we invite abstracts addressing intraplate faulting from a wide range of disciplines. This session will highlight recent research on the NMSZ and the 1811-1812 earthquakes. Contributed abstracts on analog intraplate systems, crustal structure and seismicity, geodetic observations, geodynamic modeling, and intraplate earthquake cycles are welcome.

One of the sessions  of the AGU Fall meeting will focus on the New Madrid earthquakes of 1811-12 and understanding intraplate earthquakes.  Session description is as follows: 

During the winter of 1811-1812, the central U.S. suffered three large earthquakes. The source of these events, the New Madrid seismic zone (NMSZ), lies far from the plate boundaries of North America. Significant advances in understanding intraplate systems have occurred, but the causes of large earthquakes in these settings remain an enigma. In commemoration of the New Madrid earthquakes bicentennial, we invite abstracts addressing intraplate faulting from a wide range of disciplines. This session will highlight recent research on the NMSZ and the 1811-1812 earthquakes. Contributed abstracts on analog intraplate systems, crustal structure and seismicity, geodetic observations, geodynamic modeling, and intraplate earthquake cycles are welcome.

One of the sessions  of the AGU Fall meeting will focus on the New Madrid earthquakes of 1811-12 and understanding intraplate earthquakes.  Session description is as follows: 

During the winter of 1811-1812, the central U.S. suffered three large earthquakes. The source of these events, the New Madrid seismic zone (NMSZ), lies far from the plate boundaries of North America. Significant advances in understanding intraplate systems have occurred, but the causes of large earthquakes in these settings remain an enigma. In commemoration of the New Madrid earthquakes bicentennial, we invite abstracts addressing intraplate faulting from a wide range of disciplines. This session will highlight recent research on the NMSZ and the 1811-1812 earthquakes. Contributed abstracts on analog intraplate systems, crustal structure and seismicity, geodetic observations, geodynamic modeling, and intraplate earthquake cycles are welcome.

Town Hall Style meeting in Piedmont, Missouri

Hosted by the Central U.S. Earthquake Consortium, Missouri Sate Emergency Management, and the Missouri Dept. of Natural Resources

Location and Start Time TBD