The New Madrid Fault runs 125 miles through the central United States and was responsible for the strongest earthquakes ever recorded east of the Rocky Mountains in 1811-1812. The fault sits above the buried Reelfoot Rift formed 750 million years ago. While the region is overdue for another large earthquake, cities along the fault are unprepared as most buildings do not meet modern earthquake standards and three times as much economic damage could occur compared to the last major quakes. Proper precautions are needed to ready critical infrastructure for a high-magnitude seismic event.
Lindaura de Jesus Leocádio registrou sua candidatura a vereadora pelo PDT em Astorga (PR). Seu registro está cadastrado aguardando julgamento. Ela declarou bens no valor total de R$42.000, incluindo metade de uma casa e terras, e uma caderneta de poupança.
1) The document discusses earthquakes, including what causes them, where they are located, and their effects. Most earthquakes occur at plate boundaries where tectonic plates meet.
2) Specific examples of earthquake events are described, such as the 1906 San Francisco earthquake which was caused by movement on the San Andreas Fault.
3) Consequences of earthquakes like building damage, fires, landslides and tsunamis are explained. Mitigation strategies to reduce earthquake risks are also outlined.
1. The document discusses causes and predictions of earthquakes, summarizing their occurrence throughout history and defining key terms like focus, epicenter, magnitude, and intensity.
2. Major factors that cause earthquakes are the movement of tectonic plates and release of energy from within the Earth. Earthquakes typically occur along plate boundaries and faults in the lithosphere.
3. While long term earthquake predictions are possible based on historical patterns of activity, short term reliable prediction remains elusive given the unpredictability of the natural world. Preparedness through building codes, emergency planning, and public education can help mitigate damage from earthquakes.
This document discusses various seismic hazards caused by earthquakes, including primary hazards like ground shaking and secondary hazards like fires. It describes how ground conditions can amplify or attenuate ground shaking. It also discusses liquefaction and landslides that earthquakes can trigger. The document covers challenges with earthquake forecasting given limitations in historical earthquake data, and explains the concept of seismic gaps.
This document discusses earthquakes, including what causes them, different types, measurement scales, effects, and safety tips. Earthquakes are caused by the movement of tectonic plates and can range from unnoticeable to extremely powerful. There are three main types - tectonic, volcanic, and explosions. They are measured on the Richter scale and can damage buildings/infrastructure, trigger landslides/tsunamis, and lead to liquefaction. Safety tips during an earthquake include dropping, covering, and holding on until shaking stops. Earthquake engineering aims to make structures more resistant to seismic activity.
The document summarizes information about earthquakes, including:
1. It discusses major historical earthquakes like the 1877 Nebraska quake and the 1906 San Francisco earthquake.
2. It provides details on measuring earthquake magnitude, such as the largest quakes on record being the 1960 Chile quake at M9.5 and the 1964 Alaska quake at M9.2.
3. It describes the different types of plate boundaries like divergent, convergent and transform, and gives examples of each.
The document discusses the 2015 M7.8 Nepal earthquake. It was the largest earthquake in Nepal in over 80 years and caused around 8,000 fatalities due to strong shaking and secondary effects like landslides. The earthquake occurred along the collision zone between the Indian and Eurasian tectonic plates. Analysis of seismic and satellite data provided insights into the earthquake's effects, aftershocks, and rupture process, but further research is still needed to fully understand the regional seismic hazard in this area of high seismic activity.
Lindaura de Jesus Leocádio registrou sua candidatura a vereadora pelo PDT em Astorga (PR). Seu registro está cadastrado aguardando julgamento. Ela declarou bens no valor total de R$42.000, incluindo metade de uma casa e terras, e uma caderneta de poupança.
1) The document discusses earthquakes, including what causes them, where they are located, and their effects. Most earthquakes occur at plate boundaries where tectonic plates meet.
2) Specific examples of earthquake events are described, such as the 1906 San Francisco earthquake which was caused by movement on the San Andreas Fault.
3) Consequences of earthquakes like building damage, fires, landslides and tsunamis are explained. Mitigation strategies to reduce earthquake risks are also outlined.
1. The document discusses causes and predictions of earthquakes, summarizing their occurrence throughout history and defining key terms like focus, epicenter, magnitude, and intensity.
2. Major factors that cause earthquakes are the movement of tectonic plates and release of energy from within the Earth. Earthquakes typically occur along plate boundaries and faults in the lithosphere.
3. While long term earthquake predictions are possible based on historical patterns of activity, short term reliable prediction remains elusive given the unpredictability of the natural world. Preparedness through building codes, emergency planning, and public education can help mitigate damage from earthquakes.
This document discusses various seismic hazards caused by earthquakes, including primary hazards like ground shaking and secondary hazards like fires. It describes how ground conditions can amplify or attenuate ground shaking. It also discusses liquefaction and landslides that earthquakes can trigger. The document covers challenges with earthquake forecasting given limitations in historical earthquake data, and explains the concept of seismic gaps.
This document discusses earthquakes, including what causes them, different types, measurement scales, effects, and safety tips. Earthquakes are caused by the movement of tectonic plates and can range from unnoticeable to extremely powerful. There are three main types - tectonic, volcanic, and explosions. They are measured on the Richter scale and can damage buildings/infrastructure, trigger landslides/tsunamis, and lead to liquefaction. Safety tips during an earthquake include dropping, covering, and holding on until shaking stops. Earthquake engineering aims to make structures more resistant to seismic activity.
The document summarizes information about earthquakes, including:
1. It discusses major historical earthquakes like the 1877 Nebraska quake and the 1906 San Francisco earthquake.
2. It provides details on measuring earthquake magnitude, such as the largest quakes on record being the 1960 Chile quake at M9.5 and the 1964 Alaska quake at M9.2.
3. It describes the different types of plate boundaries like divergent, convergent and transform, and gives examples of each.
The document discusses the 2015 M7.8 Nepal earthquake. It was the largest earthquake in Nepal in over 80 years and caused around 8,000 fatalities due to strong shaking and secondary effects like landslides. The earthquake occurred along the collision zone between the Indian and Eurasian tectonic plates. Analysis of seismic and satellite data provided insights into the earthquake's effects, aftershocks, and rupture process, but further research is still needed to fully understand the regional seismic hazard in this area of high seismic activity.
How Natural Disasters Impact the Environment 2013Jenny Dixon
This document discusses how various natural disasters impact the environment. It begins by defining different types of natural disasters such as earthquakes, hurricanes, fires, tsunamis, volcanoes, blizzards, floods, tornadoes, droughts and heat waves. For each disaster, it summarizes the typical damage caused, such as property destruction, loss of habitat, erosion, contamination of water supplies, and loss of power. Overall, the key environmental impacts of natural disasters discussed are property loss, loss of habitat, and damage to infrastructure.
- A series of great earthquakes between 1938 and 1965 ruptured almost the entire Alaska subduction zone. The average recurrence time for magnitude 9 earthquakes in this region is 700-900 years.
- During the 1964 Alaska earthquake, areas in the uplift zone were raised up to 6 meters while areas in the subsidence zone dropped over 2 meters. This vertical displacement contributed to tsunami generation and inundation.
- Tsunamis deposit distinct sediment layers that can be used to date past events. Analysis of sediment layers at sites like Girdwood has revealed evidence of tsunamis occurring every 280-295 years on average in that region of Alaska.
1) The document provides 10 interesting facts about earthquakes, including details on the largest recorded quakes, what defines an epicenter and hypocenter, earthquake magnitudes, and rates of movement along the San Andreas Fault.
2) It examines the 1960 Valdivia earthquake, the most powerful ever at magnitude 9.5, describing its effects and providing a map and footage of the resulting tsunami.
3) The document outlines different types of fault boundaries like divergent and thrust faults, and assigns homework for students to make a collage about earthquakes.
1) The document provides 10 interesting facts about earthquakes, including details on the largest recorded quakes, what defines an epicenter and hypocenter, earthquake magnitudes, and rates of movement along the San Andreas Fault.
2) It examines the 1960 Valdivia earthquake, the most powerful ever at magnitude 9.5, describing its effects and providing a map and footage of the resulting tsunami.
3) The document outlines different types of fault boundaries like divergent and thrust faults, and assigns homework for students to make a collage of earthquake pictures.
This document discusses earthquake hazards and mitigation. It notes that approximately 500,000 earthquakes occur each year, with around 100 being potentially dangerous. Major earthquakes typically occur annually and can release large amounts of seismic energy. Earthquakes cause damage through ground shaking, liquefaction, landslides, fires, and tsunamis. Mitigation strategies include avoiding hazard areas, building earthquake resistant structures using special materials and construction techniques, improving weak soils, and reducing seismic demand on structures. Proper architectural design and reinforcement of masonry and reinforced concrete buildings can also improve earthquake resistance.
Over 15,000 earthquakes have occurred in New Zealand. When two parts of the Earth's surface move suddenly along a fault line due to tectonic forces, an earthquake occurs. Earthquakes can cause massive damage through shaking and collapsing buildings, which then must be rebuilt. Most earthquakes happen along the boundaries of tectonic plates, which move due to convection currents in the Earth's mantle.
How Natural Disasters Impact the Environment 2013Jenny Dixon
This document discusses how various natural disasters impact the environment. It begins by defining different types of natural disasters such as earthquakes, hurricanes, fires, tsunamis, volcanoes, blizzards, floods, tornadoes, droughts and heat waves. For each disaster, it summarizes the typical damage caused, such as property destruction, loss of habitat, erosion, contamination of water supplies, and loss of power. Overall, the key environmental impacts of natural disasters discussed are property loss, loss of habitat, and damage to infrastructure.
- A series of great earthquakes between 1938 and 1965 ruptured almost the entire Alaska subduction zone. The average recurrence time for magnitude 9 earthquakes in this region is 700-900 years.
- During the 1964 Alaska earthquake, areas in the uplift zone were raised up to 6 meters while areas in the subsidence zone dropped over 2 meters. This vertical displacement contributed to tsunami generation and inundation.
- Tsunamis deposit distinct sediment layers that can be used to date past events. Analysis of sediment layers at sites like Girdwood has revealed evidence of tsunamis occurring every 280-295 years on average in that region of Alaska.
1) The document provides 10 interesting facts about earthquakes, including details on the largest recorded quakes, what defines an epicenter and hypocenter, earthquake magnitudes, and rates of movement along the San Andreas Fault.
2) It examines the 1960 Valdivia earthquake, the most powerful ever at magnitude 9.5, describing its effects and providing a map and footage of the resulting tsunami.
3) The document outlines different types of fault boundaries like divergent and thrust faults, and assigns homework for students to make a collage about earthquakes.
1) The document provides 10 interesting facts about earthquakes, including details on the largest recorded quakes, what defines an epicenter and hypocenter, earthquake magnitudes, and rates of movement along the San Andreas Fault.
2) It examines the 1960 Valdivia earthquake, the most powerful ever at magnitude 9.5, describing its effects and providing a map and footage of the resulting tsunami.
3) The document outlines different types of fault boundaries like divergent and thrust faults, and assigns homework for students to make a collage of earthquake pictures.
This document discusses earthquake hazards and mitigation. It notes that approximately 500,000 earthquakes occur each year, with around 100 being potentially dangerous. Major earthquakes typically occur annually and can release large amounts of seismic energy. Earthquakes cause damage through ground shaking, liquefaction, landslides, fires, and tsunamis. Mitigation strategies include avoiding hazard areas, building earthquake resistant structures using special materials and construction techniques, improving weak soils, and reducing seismic demand on structures. Proper architectural design and reinforcement of masonry and reinforced concrete buildings can also improve earthquake resistance.
Over 15,000 earthquakes have occurred in New Zealand. When two parts of the Earth's surface move suddenly along a fault line due to tectonic forces, an earthquake occurs. Earthquakes can cause massive damage through shaking and collapsing buildings, which then must be rebuilt. Most earthquakes happen along the boundaries of tectonic plates, which move due to convection currents in the Earth's mantle.
Similar to New Madrid Fault_Brendan_BJS comments (7)
2. History
Reelfoot Rift
Failed breakup of Supercontinent Rodinia (750
million years ago)
Sand Blows
Formed about 4800 B.C. and 3500 B.C.
Similar to New Madrid
3. Current Area
Four-segment, zig-zag fault
system
125 miles long
Fault extends from Marked
Tree, Arkansas to Cairo,
Illinois
Rocks in the region are
harder, colder, dryer, and less
fractured
4. Earthquakes of 1811-12
Strongest earthquake recorded east of Rocky
Mountains
Five major earthquakes (magnitude 7.0), 15
earthquakes (6.5-8.0), 189 earthquakes (5.0-6.5)
Reelfoot Lake created
5. Worst Case
$300 Billion in Direct Economic
Loss (Three times worst than
Phase I)
3,500 Fatalities
2.6 Million Households without
power
Bedrock In Downtowns
St. Louis - 10 feet below surface
Memphis - 3,000 feet below
surface
9. Summary
The region is We are overdue for a earthquake the
size of a 6.3 by 30 years
Majority of buildings are not up to date on earthquake
standards
No change in the foreseeable future
Editor's Notes
Crust in the New Madrid Area is weaker than much of the crust in the rest of the United States.
Geologists call this an aulacogen (a scar or zone of weakness)
Scientists do not know much history about the seismic zone since it is so far below the surface, explain later.
Marianna sand blows predate paleoearthquakes attributed to NMFZ. Used the rock record to determine these.
Earthquake is not on the surface (San Andreas). Hidden bellow 100-200 ft. thick layers of alluvium.
Shake and damage are 20 times larger compared to California and most other seismic zones.
Five earthquakes took place between December 16,1811 and February 7, 1812.
Rang church bells on East Coast, cracked sidewalks in Washington D.C.
James Madison, sitting president was awakened in the middle of the night.
Two thousand more were felt by people, crude seismograph and personal journals
Louisville, Kentucky, and Cincinnati, OH. (250 and 350 miles away respectively)
Picture
Landslide trench and ridge in the Chickasaw Bluffs east of Reelfoot Lake, Tennessee
Minor shocks and tremors between releasing small amounts of energy
Federal Emergency Management Agency (FEMA) (Phase I, 2008; Phase II, 2010)
Phase One looked at possibilities if various segments erupted
Fatalities belong to 2:00am scenario
715,000 Damaged Buildings
Involves a complete rupture of the fault throughout the region
Other studies project even worse
Picture
NMSZ liquefaction susceptibility of Evansville
Cities are not ready. Until there is a loss of life, governments will not update the current earthquake standards.
NGA - built in the early 1900s, mostly brick and concrete on the inside. Government workers work include analyze natural disasters (Haiti, 2010). Separate from the U.S. Geologic Survey.
Monsanto Center - Built in 1997, designed to be “earthquake proof” with 41 base isolators placed beneath the building and mounted footings that reach to the bedrock (10 feet)
This is an example of the base isolators that are found underneath the Monsanto Center.
The building itself is floating on these base isolators.