| Earthquake Awareness and Preparedness |
![]() | Buried sand-blow deposits within the Mississippi River Valley are believed to be the by- | |
| product of strong ground shaking associated with large past earthquakes. | ||
![]() | Several of the largest historical earthquakes to strike the continental United States occurred | |
| in the winter of 1811-1812 from the New Madrid Fault. | ||
![]() | The three main earthquakes of magnitude 7.0-8.0 occurred on December 16, 1811; January | |
| 23, 1812; and February 7, 1812. | ||
![]() | The New Madrid Fault stretches from the west of Memphis in Tennessee into Southern | |
| Illinois and consists of three fault segments: the northeast and the southwest segments which are strike-slip fault lines, and the central segment known as the Reelfoot which is a thrust fault. Figure 2 shows my best-estimate dimensions and locations of the southwest and Reelfoot faults along with the location of the metropolitan areas of St. Louis, Missouri, and Memphis, Tennessee. | ||
![]() | Any New Madrid Fault segment can generate a magnitude 7.7 earthquake as predicted by the | |
| USGS. | ||
![]() | The region of potential impact due to earthquake activity from the New Madrid Fault is | |
| comprised of eight states: Alabama, Arkansas, Illinois, Indiana, Kentucky, Mississippi, Missouri, and Tennessee. |
![]() | The region surrounding the New Madrid Fault is home to millions of people, including those in the | |
| metropolitan areas of St. Louis Missouri and Memphis Tennessee, where most buildings were not built to withstand earthquake ground shaking. Earthquake damage to buildings in Memphis is expected to be extensive due to its large number of highly-vulnerable unreinforced masonry homes that will be significantly affected. In addition, earthquake awareness and earthquake preparedness in the Midwestern States have lagged far behind the West Coast. |
![]() | Tennessee would incur the highest level of economic loss, earthquake damage, and social | |
| impact. Over 250,000 buildings are expected to be moderately or severely damaged from rupture of the southwestern segment of the New Madrid Fault. Over 260,000 people would be displaced and over 60,000 casualties (injuries and fatalities). Total direct economic losses surpass $56 billion. | ||
![]() | Missouri would also incur substantial economic loss and earthquake damage. Over 80,000 | |
| buildings are expected to be damaged leaving more than 120,000 people displaced, and causing over 15,000 casualties. Total direct economic losses reach $40 billion. | ||
![]() | Kentucky and Illinois are expected to incur significant losses with total direct economic losses | |
| reaching approximately $45 and $35 billion, respectively. | ||
![]() | Arkansas and Mississippi would incur nearly $19 and $9.5 billion in direct economic loss, | |
| respectively. | ||
![]() | Indiana and Alabama would experience limited earthquake damage and total direct economic | |
| losses of approximately $1.5 and $1.0 billion, respectively. |
| Figure 2 - New Madrid Fault |
![]() | Several times in the past century, moderate-to-large earthquakes have been widely felt in the WVSZ | |
| as shown in Figure 1. | ||
![]() | The WVSZ can generate a magnitude 7.1 earthquake according to the USGS. | |
![]() | The region of potential impact due to earthquake activity in the WVSZ is comprised of three states: | |
| Illinois, Indiana, and Kentucky. |
| Figure 3 - New Madrid vs. California Earthquakes permission from Prof. Herrmann of St. Louis University |
| Figure 1 - NMSZ & WVSZ Earthquakes USGS permission, Dr. E. Schweig |
![]() | Earthquakes in the Central and Eastern United States (CEUS) are less frequent than in the Western | |
| United States (WUS). However, they affect much larger areas because of the regional geology being different east and west of the Rocky Mountains. | ||
![]() | The CEUS is a more stable region in which the energy released from a medium-to-large earthquake | |
| is transmitted into the surrounding regions more efficiently, while the energy is relatively quickly absorbed in the WUS. | ||
![]() | Figure 3 illustrates the affected areas from two large earthquakes of similar magnitude: the 1906 San | |
| Francisco Earthquake whose magnitude was 7.8 and the December 16, 1811 New Madrid Earthquake whose best-estimated magnitude is 7.7. San Francisco Earthquake was felt 350 miles away in the middle of Nevada, while church bells rang in Boston Massachusetts which is 1,000 miles away from the New Madrid Fault. Therefore, seismic activity in the NMSZ and similarly the WVSZ is capable of causing widespread damage over a large region in Midwestern States. |
![]() | Back- and forth- ground shaking, soil amplification, liquefaction, landslides, and | |
| fires are the main reasons for structural damage to buildings. Soil amplification would occur in deep soils of the Mississippi River Valley resulting in stronger ground shaking as compared to shallow stiff alluvial soils on the bedrock. Areas of liquefaction are within: a) The Central Mississippi River Valley including the Reelfoot Scarp, the New Madrid Fault, and the Western Lowlands liquefaction features; and b) The Mississippi and Ohio Rivers Regions including the Wabash Valley and St. Louis-Cape Girardeau liquefaction features. Structural damage is influenced by construction materials, year built, and number of stories, and occurs if the building is not effectively bolted to the concrete foundations, the cripple walls are not braced, or the existence of a soft story in homes with large openings (e.g. garage doors or windows) at the first level without effective bracing. | ||
![]() | The Mid-America Earthquake Center at the University of Illinois at Urbana- | |
| Champaign documented that residential buildings in the Midwest would incur more structural damage than any other building usage. Timber frame houses are the most prevalent residential building type in the Midwest, while unreinforced masonry houses comprise a much smaller portion of the regional building inventory. However, estimates show that structural damage to unreinforced masonry construction are at much higher percentage than wooden houses even from moderate ground shaking. Tennessee alone shows 50,000 moderate-to- severe structural damage of its unreinforced masonry construction from rupture of the southwestern segment of the New Madrid Fault. It is reasonable to assume that several hundred thousand unreinforced masonry buildings could be damaged in the eight Midwestern States if successive ruptures of the three segments occur, as the case of the 1811-1812 series of earthquakes. |
| Personal Survival Kits |
| Household Emergency Kit |
| Emergency Sleeping Bag |
| Emergency Tent |