
Seismic Potential in the Midwestern
and Southeastern US (2013-4):
Preparation for the Next Large-Scale Event!



Cartography: Paul Paddock
Data: US Geological Survey,
US Census Bureau
These maps were produced to visualize the current seismic hazard areas residing in the 3-4 o'clock zone of the US using Geospatial analysis. The map with the red frame shows the peak horizontal acceleration (PHA) of three areas which experience earthquakes almost daily. The quakes are small (1.0 to 3.0 on the Richter Scale), but they may be precursors for more devastating quakes in the future in this region.
What is curious about these miniature rumblings is that they are in the middle of North America's continental tectonic plate. The nearest major fault lines are the San Andreas on the West Coast and the Mid-Atlantic over a thousand miles east of the East Coast. Apparently there are weak rock layers deep in the Earth's mantle and research even shows that underneath the Mississippi River used to exist a fault line during ancient times. At this point it is unclear whether this is the reason for the resurgence in activity here. Further study is currently conducted in this area.
The map with the yellow frame shows quake activity firing up in Oklahoma in addition to the New Madrid Seismic Zones. According to the US and Oklahoma Geologic Surveys, within the four years preceding, at least 200 larger earthquakes have plagued the state, as opposed to one to three happening for 33 years prior (AP). This is a hazardous concern, which again, is conveyed pictorially through GIS to raise awareness and preparation can commence. Current research shows that this is due to fracking, which might further fuel a larger earthquake in the future.
*%g refers to percentage of objects falling due to gravity. Peak horizontal acceleration (PHA) is the rate at which the ground moves (USGS). Measuring quake intensity predictions help to identify the zones most vulnerable to quake action.
**UTC--Coordinated Universal Time is used by seismologists to record the standard time for the instant when a tremor occured. This reduces confusion between time zones. UTC is always recorded in military time within the time zone of Greenwich, UK.
Basemaps: ESRI Data: US Geological Survey,
Cartography: Paul Paddock US Census Bureau
Evacuation Suggestions: New Madrid Seismic Zone By States
Missouri


Arkansas

Although it is nearly impossible to predict an earthquake, practices in advance warning systems are in place, based on previous events, though far from ideal. The latest resurgings in activity may show signs of a looming mega-earthquake, probably a 7.0 or higher in the near future, and this region is ill-equipped for it. Disaster might be unavoidable, but impact can be minimized though GIS analysis.
These maps show suggested evacuation routes out of the hazard zone, shown in warm colors on the map. Should an advisory be declared, residents would evacuate using the color-coded roads and interstates out of the zone via the Evacuation Guides on the maps. Generally, since each zone is laid out almost east and west of each other, the ideal option is to venture north or south to safety.
About the Maps
A 140-mile radius was spatially defined about the highest-risk area in Missouri (New Madrid) and a 75-mile each for those in SC and TN, and street detail is more emphasized in these buffers for guidance. The buffer size was based on post-reactionary analysis from the 1811-1812 mega-earthquakes in northern Arkansas and New Madrid, MO (USGS). Even though quakes of this magnitude could be felt as far away as New York, as it was at that time, and evacuation does not guarantee 100% safety, an evacuation using this analysis would still minimize the death toll by a large stretch. Interstates are best for travel, but secondary roads are best for safety especially in the open rural plains. It does not matter where residents go, as long as they are outside and away from tall buildings or objects. Depending on where residents live, they can follow the nearest highlighted routes for guidance. Again, these routes are the most direct ways out of the area, but other paths can be taken if more direct, especially in the outer edges of the zones. For more information about these seismic hazard areas, consult USGS.
Illinois, IN, & KY


Tennessee, MS, & AL

Basemaps: ESRI
Cartography: Paul Paddock
Data: US Geological Survey,
US Census Bureau
Evacuation Suggestions: Southern Appalachians, South Carolina, & Oklahoma
Eastern Tennessee



South Carolina
Oklahoma


Basemaps: ESRI
Cartography: Paul Paddock
Data: US Geological Survey,
US Census Bureau
Additional Works Consulted
Glover, Lynn III and Gates, Alexander E. Central and Southern Appalachian Sutures: Results of the EDGE Project and Related Studies. Boulder, CO: The Geological Society of America, Inc., 1997. Google Books.
Howard, J. Michael. "Rockhounding Arkansas." Arts & Ideas Studio. 2018. http://rockhoundingar.com/fault.php.
Dunn, Meredith M. and Chapman, Martin C. "Fault Orientation in the Eastern Tennessee Seismic Zone: A Study Using the Double-Difference Earthquake Location Algorithm." Seismological Research Letters. 77, no. 4 (2006): 494-504. doi: 10.1875.
Gardner, David. "Think living in Tennessee makes you safe from earthquakes? The earthquake map of America that will make you think again." Daily Mail. March 16, 2011. https://www.dailymail.co.uk/news/article-1366603/Earthquake-map-America-make-think-again.html.