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Impact of New Madrid Seismic Zone Earthquakes on the Central USA

Impact of New Madrid Seismic Zone Earthquakes on the Central USA
Author: Mid-America Earthquake Center
Publisher:
Total Pages: 139
Release: 2009
Genre: Earthquakes
ISBN:

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The information presented in this report has been developed to support the Catastrophic Earthquake Planning Scenario workshops held by the Federal Emergency Management Agency. Four FEMA Regions (Regions IV, V, VI and VII) were involved in the New Madrid Seismic Zone (NMSZ) scenario workshops. The four FEMA Regions include eight states, namely Illinois, Indiana, Kentucky, Tennessee, Alabama, Mississippi, Arkansas and Missouri. The earthquake impact assessment presented hereafter employs an analysis methodology comprising three major components: hazard, inventory and fragility (or vulnerability). The hazard characterizes not only the shaking of the ground but also the consequential transient and permanent deformation of the ground due to strong ground shaking as well as fire and flooding. The inventory comprises all assets in a specific region, including the built environment and population data. Fragility or vulnerability functions relate the severity of shaking to the likelihood of reaching or exceeding damage states (light, moderate, extensive and near-collapse, for example). Social impact models are also included and employ physical infrastructure damage results to estimate the effects on exposed communities. Whereas the modeling software packages used (HAZUS MR3; FEMA, 2008; and MAEviz, Mid-America Earthquake Center, 2008) provide default values for all of the above, most of these default values were replaced by components of traceable provenance and higher reliability than the default data, as described below. The hazard employed in this investigation includes ground shaking for a single scenario event representing the rupture of all three New Madrid fault segments. The NMSZ consists of three fault segments: the northeast segment, the reelfoot thrust or central segment, and the southwest segment. Each segment is assumed to generate a deterministic magnitude 7.7 (Mw7.7) earthquake caused by a rupture over the entire length of the segment. US Geological Survey (USGS) approved the employed magnitude and hazard approach. The combined rupture of all three segments simultaneously is designed to approximate the sequential rupture of all three segments over time. The magnitude of Mw7.7 is retained for the combined rupture. Full liquefaction susceptibility maps for the entire region have been developed and are used in this study. Inventory is enhanced through the use of the Homeland Security Infrastructure Program (HSIP) 2007 and 2008 Gold Datasets (NGA Office of America, 2007). These datasets contain various types of critical infrastructure that are key inventory components for earthquake impact assessment. Transportation and utility facility inventories are improved while regional natural gas and oil pipelines are added to the inventory, alongside high potential loss facility inventories. The National Bridge Inventory (NBI, 2008) and other state and independent data sources are utilized to improve the inventory. New fragility functions derived by the MAE Center are employed in this study for both buildings and bridges providing more regionally-applicable estimations of damage for these infrastructure components. Default fragility values are used to determine damage likelihoods for all other infrastructure components. The study reports new analysis using MAE Center-developed transportation network flow models that estimate changes in traffic flow and travel time due to earthquake damage. Utility network modeling was also undertaken to provide damage estimates for facilities and pipelines. An approximate flood risk model was assembled to identify areas that are likely to be flooded as a result of dam or levee failure. Social vulnerability identifies portions of the eight-state study region that are especially vulnerable due to various factors such as age, income, disability, and language proficiency. Social impact models include estimates of displaced and shelter-seeking populations as well as commodities and medical requirements. Lastly, search and rescue requirements quantify the number of teams and personnel required to clear debris and search for trapped victims. The results indicate that Tennessee, Arkansas, and Missouri are most severely impacted. Illinois and Kentucky are also impacted, though not as severely as the previous three states. Nearly 715,000 buildings are damaged in the eight-state study region. About 42,000 search and rescue personnel working in 1,500 teams are required to respond to the earthquakes. Damage to critical infrastructure (essential facilities, transportation and utility lifelines) is substantial in the 140 impacted counties near the rupture zone, including 3,500 damaged bridges and nearly 425,000 breaks and leaks to both local and interstate pipelines. Approximately 2.6 million households are without power after the earthquake. Nearly 86,000 injuries and fatalities result from damage to infrastructure. Nearly 130 hospitals are damaged and most are located in the impacted counties near the rupture zone. There is extensive damage and substantial travel delays in both Memphis, Tennessee, and St. Louis, Missouri, thus hampering search and rescue as well as evacuation. Moreover roughly 15 major bridges are unusable. Three days after the earthquake, 7.2 million people are still displaced and 2 million people seek temporary shelter. Direct economic losses for the eight states total nearly $300 billion, while indirect losses may be at least twice this amount. The contents of this report provide the various assumptions used to arrive at the impact estimates, detailed background on the above quantitative consequences, and a breakdown of the figures per sector at the FEMA region and state levels. The information is presented in a manner suitable for personnel and agencies responsible for establishing response plans based on likely impacts of plausible earthquakes in the central USA.


Fault-Zone Properties and Earthquake Rupture Dynamics

Fault-Zone Properties and Earthquake Rupture Dynamics
Author: Eiichi Fukuyama
Publisher: Academic Press
Total Pages: 333
Release: 2009-04-24
Genre: Science
ISBN: 0080922465

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The dynamics of the earthquake rupture process are closely related to fault zone properties which the authors have intensively investigated by various observations in the field as well as by laboratory experiments. These include geological investigation of the active and fossil faults, physical and chemical features obtained by the laboratory experiments, as well as the seismological estimation from seismic waveforms. Earthquake dynamic rupture can now be modeled using numerical simulations on the basis of field and laboratory observations, which should be very useful for understanding earthquake rupture dynamics. Features: * First overview of new and improved techniques in the study of earthquake faulting * Broad coverage * Full color Benefits: * A must-have for all geophysicists who work on earthquake dynamics * Single resource for all aspects of earthquake dynamics (from lab measurements to seismological observations to numerical modelling) * Bridges the disciplines of seismology, structural geology and rock mechanics * Helps readers to understand and interpret graphs and maps Also has potential use as a supplementary resource for upper division and graduate geophysics courses.


Seismic Loss Assessment of Sequential Rupture of New Madrid Seismic Zone on the Central US

Seismic Loss Assessment of Sequential Rupture of New Madrid Seismic Zone on the Central US
Author: Anisa Como
Publisher:
Total Pages:
Release: 2010
Genre:
ISBN:

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The New Madrid Seismic Zone (NMSZ) is described as a low probability high risk event. In case of a repetition of the 1811-1812 earthquake series, the expected consequences will cause catastrophic impacts to directly affected areas and beyond. An accurate earthquake impact assessment of the NMSZ is essential to generate an efficient response from FEMA and its associates and to educate and prepare the general population. The objective of this project is to provide scientifically defensible earthquake impact assessments with the most improved hazard, inventory, and fragility data to save lives and protect property. The study region encompasses eight states: Alabama, Arkansas, Illinois, Indiana, Kentucky, Mississippi, Missouri, and Tennessee. The implemented scenario aspires to recreate the events of 1811-1812 as accurately as possible within modeling constrains. The resulting scenario is a 7.7 magnitude earthquake event with sequential rupture of all three segments of the NMSZ simultaneously. Hazard improvements include complete liquefaction and shaking maps, while multiple inventory datasets are incorporated and added to the existing default assets. An advanced methodology for fragility derivation is applied and improved fragility functions are included for buildings and bridges, based on inelastic response. Additionally, secondary effects of flooding due to dam failure are analyzed. The analytical analysis is executed in HAZUS-MH MR3 developed by FEMA. Several damage criteria were developed to determine the most critically impacted counties. The results of the impact assessment are staggering, with 140 impacted counties and over 700,000 damaged buildings. Essential facilities such as schools and hospitals incur severe damage. Transportation and utility lifelines experience serious functionality impairments. Catastrophic consequences result in nearly 86,000 casualties and approximately $300 billion in direct economic loses. Finally, essential components of future research work are identified. The employed approaches and lesson learned in this project are applicable for worldwide earthquake impact assessments.


The New Madrid Earthquake

The New Madrid Earthquake
Author: Myron L. Fuller
Publisher: Care Publications
Total Pages: 138
Release: 1993-07
Genre: Nature
ISBN: 9780934426497

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This is an unabridged reprint of the first book and first thorough scientific work ever published on the great New Madrid earthquakes of 1811-12. The winter of 1811-12 experienced the greatest burst of seismic energy in the history of the original 48 states. Geologist, Myron Fuller, spent several years in the field between 1900-1905 scouting the New Madrid fault zone on foot and on horseback, mapping the consequences of these giant cataclysms that had so permanently and so profoundly changed the landscape of this region 90 years before. Originally published by the U.S. Geological Survey, this book is the starting point for all serious researchers on these world-class temblors. Foreword to this 1995 printing is by seismologist, David Stewart, Ph.D.