The 8.9 magnitude earthquake off the coast of Japan on March 11, 2011 triggered a massive tsunami that caused widespread destruction and loss of life across Japan; the earthquake and tsunami had devastating primary impacts such as damaged infrastructure, loss of power and water supplies, and a tsunami over 24 feet high, as well as secondary impacts including fires, landslides, and an explosion at a nuclear power plant. While the impacts were immense, preparedness measures and policies in Japan helped to minimize loss of life.
This document discusses damage from the 1989 Loma Prieta earthquake in San Francisco. It includes several photos showing: 1) a 4-story building damaged by weak first story failure due to reduced shear wall strength and lack of bracing; 2) wreckage of downtown buildings; 3) soil liquefaction causing uneven settlement and tilting of apartment buildings in Niigata, Japan. The document continues with additional photos of earthquake damage from the 1989 earthquake and other large quakes.
Coastal Geologic Hazards and Sea-Level Rise: Climate Change in Rhode Islandriseagrant
Coastal Geologic Hazards and Sea-Level Rise: Climate Change in Rhode Island
This presentation was given at the Shoreline Change SAMP Stakeholder Meeting on April 4th, 2013 by Jon C. Boothroyd (Rhode Island Geological Survey and Department of Geosciences, University of Rhode Island) and Bryan A. Oakley (Environmental Earth Science Department, Eastern Connecticut State University).
The 2004 Indian Ocean earthquake was caused by subduction along the boundary between the India and Burma tectonic plates. As the India plate slid under the Burma plate, it displaced a massive amount of water and triggered devastating tsunamis across the Indian Ocean. There were no early warning systems in place in the Indian Ocean like in the Pacific, so the tsunamis came as a surprise to most areas. However, some communities like Simeulue Island were able to evacuate after recognizing the signs of an impending tsunami from local knowledge passed down over generations.
The document provides information about tsunamis presented by Harsh in standard VIII A. It defines tsunamis as a series of large ocean waves caused by earthquakes under the sea. The largest tsunami was in Lituya Bay, Alaska in 1958. Earthquakes are the main cause of tsunamis as the movement of tectonic plates under the sea can sometimes cause huge displacements of water. Proper warning systems and evacuation procedures help minimize loss of life from tsunamis.
An undersea earthquake off the coast of Indonesia in 2004 triggered a devastating tsunami across the Indian Ocean. The earthquake, caused by tectonic plate subduction, generated a massive displacement of water that produced 30-foot high waves. Over 250,000 people across 14 countries were killed, with over 130,000 deaths in Indonesia alone. The tsunami destroyed coastal infrastructure and displaced millions of people, while secondary impacts included disease outbreaks and loss of livelihoods. Major humanitarian aid and long-term reconstruction efforts were required.
The 2011 Tohoku earthquake in Japan was a 9.0 magnitude megaquake caused by subduction along the plate boundary where the Pacific plate dives beneath the Eurasian plate. It generated a massive tsunami that caused widespread damage. Over 15,000 people died, mostly from drowning, and economic costs are estimated at $185-309 billion, making it one of the most costly natural disasters ever. Strict building codes limited structural damage from the quake, but the tsunami overwhelmed coastal infrastructure and communities. The disaster highlighted the need to strengthen protections against both seismic events and tsunamis.
The 8.9 magnitude earthquake off the coast of Japan on March 11, 2011 triggered a massive tsunami that caused widespread destruction and loss of life across Japan; the earthquake and tsunami had devastating primary impacts such as damaged infrastructure, loss of power and water supplies, and a tsunami over 24 feet high, as well as secondary impacts including fires, landslides, and an explosion at a nuclear power plant. While the impacts were immense, preparedness measures and policies in Japan helped to minimize loss of life.
This document discusses damage from the 1989 Loma Prieta earthquake in San Francisco. It includes several photos showing: 1) a 4-story building damaged by weak first story failure due to reduced shear wall strength and lack of bracing; 2) wreckage of downtown buildings; 3) soil liquefaction causing uneven settlement and tilting of apartment buildings in Niigata, Japan. The document continues with additional photos of earthquake damage from the 1989 earthquake and other large quakes.
Coastal Geologic Hazards and Sea-Level Rise: Climate Change in Rhode Islandriseagrant
Coastal Geologic Hazards and Sea-Level Rise: Climate Change in Rhode Island
This presentation was given at the Shoreline Change SAMP Stakeholder Meeting on April 4th, 2013 by Jon C. Boothroyd (Rhode Island Geological Survey and Department of Geosciences, University of Rhode Island) and Bryan A. Oakley (Environmental Earth Science Department, Eastern Connecticut State University).
The 2004 Indian Ocean earthquake was caused by subduction along the boundary between the India and Burma tectonic plates. As the India plate slid under the Burma plate, it displaced a massive amount of water and triggered devastating tsunamis across the Indian Ocean. There were no early warning systems in place in the Indian Ocean like in the Pacific, so the tsunamis came as a surprise to most areas. However, some communities like Simeulue Island were able to evacuate after recognizing the signs of an impending tsunami from local knowledge passed down over generations.
The document provides information about tsunamis presented by Harsh in standard VIII A. It defines tsunamis as a series of large ocean waves caused by earthquakes under the sea. The largest tsunami was in Lituya Bay, Alaska in 1958. Earthquakes are the main cause of tsunamis as the movement of tectonic plates under the sea can sometimes cause huge displacements of water. Proper warning systems and evacuation procedures help minimize loss of life from tsunamis.
An undersea earthquake off the coast of Indonesia in 2004 triggered a devastating tsunami across the Indian Ocean. The earthquake, caused by tectonic plate subduction, generated a massive displacement of water that produced 30-foot high waves. Over 250,000 people across 14 countries were killed, with over 130,000 deaths in Indonesia alone. The tsunami destroyed coastal infrastructure and displaced millions of people, while secondary impacts included disease outbreaks and loss of livelihoods. Major humanitarian aid and long-term reconstruction efforts were required.
The 2011 Tohoku earthquake in Japan was a 9.0 magnitude megaquake caused by subduction along the plate boundary where the Pacific plate dives beneath the Eurasian plate. It generated a massive tsunami that caused widespread damage. Over 15,000 people died, mostly from drowning, and economic costs are estimated at $185-309 billion, making it one of the most costly natural disasters ever. Strict building codes limited structural damage from the quake, but the tsunami overwhelmed coastal infrastructure and communities. The disaster highlighted the need to strengthen protections against both seismic events and tsunamis.
The document discusses tsunamis, including their causes, characteristics, and historical examples. It provides details on underwater earthquakes triggering tsunamis and describes tsunamis as consisting of multiple waves rather than a single wave. Examples of destructive tsunamis throughout history are given for various regions.
The largest tsunami on record was triggered by a 9.15 magnitude earthquake under the Indian Ocean on December 26, 2004. The tsunami waves reached heights of up to 49 feet and caused catastrophic damage across multiple countries in Southeast Asia and East Africa. Over 310,000 people lost their lives or were injured across Indonesia, Sri Lanka, India, Thailand and other nations impacted by the devastating waves. The earthquake and resulting tsunami are considered one of the deadliest natural disasters in history.
New microsoft office power point presentationbharatbarman
The document compares and contrasts the 2011 Japan tsunami and the 2004 Indian Ocean tsunami. It notes that while both disasters were deadly, the death toll was much higher for the 2004 tsunami which killed over 200,000 people across several countries. In contrast, the 2011 Japan tsunami has resulted in around 10,000 deaths reported so far. A key difference was that Japan had early warning systems and tsunami preparedness measures in place, while coastal areas in South Asia caught by the 2004 tsunami had little to no warning. Both earthquakes that triggered the tsunamis were extremely large at 9.0 magnitudes.
Earthquakes occur along fault lines when tectonic plates collide or scrape against each other. The San Andreas Fault in California is responsible for some of the most destructive quakes in U.S. history due to the North American and Pacific plates scraping past each other there. Major quakes can cause tsunamis, massive ocean waves caused by underwater seismic activity that can devastate coastal areas.
The document provides safety tips for tsunamis, including making an evacuation plan and list of essential items, elevating coastal homes above 10 feet to avoid most tsunami waves, taking precautions to prevent flooding, using local media for updates, and following instructions from local authorities. It advises that if a warning is issued, families in tsunami-prone areas should evacuate to higher ground and stay away from rivers and streams, while those on beaches should move to high ground if they feel the earth shaking.
This presentation took place on Tuesday 17th of march 2015 at Faculty of Engineering, Cairo University. I was asked by the professor to prepare a report and presentation about the lessons learned from Pakistan 2005 earthquake.
This document discusses tsunamis, which are giant waves caused by earthquakes or volcanic eruptions under the sea. Tsunamis can cause massive damage and loss of life by destroying homes and infrastructure. While impossible to prevent, their effects can be minimized through preparation measures like building in safe areas, establishing evacuation routes, and early warning systems. The document outlines dos and don'ts for before, during, and after a tsunami and emphasizes the importance of quickly evacuating coastal areas if a tsunami is detected or warned.
The document summarizes details of the 2011 Tōhoku earthquake and tsunami in Japan. It was a 9.0 magnitude earthquake that struck off the coast of Japan on March 11, 2011. It caused widespread damage including over 5,000 deaths and triggered a large tsunami with waves as high as 33 feet in some areas. The earthquake was one of the most powerful ever recorded and had devastating impacts across Japan such as fires, power outages, and nuclear plant issues.
The document provides information about tsunamis, including what causes them, warning signs, and safety precautions. It describes how tsunamis are caused by large displacements of water from earthquakes or volcanic eruptions. It lists evacuation plans and safety tips, such as knowing evacuation routes and staying away from coastal areas when there is a tsunami warning. The document also summarizes details about the devastating 2004 Indian Ocean tsunami and the 2011 Tohoku earthquake and tsunami in Japan.
A tsunami is a series of waves caused by the displacement of a large volume of water, generally in an ocean or large lake. Earthquakes, volcanic eruptions, and other disturbances under water have the potential to generate tsunamis. The 2004 Indian Ocean tsunami was one of the deadliest natural disasters in recorded history, caused by an earthquake under the Indian Ocean with a magnitude of 9.1-9.3 that killed over 227,000 people across 14 countries, mostly in Indonesia, Sri Lanka, India, and Thailand. It highlighted the need for improved warning systems for tsunamis in the Indian Ocean.
The 2004 Indian Ocean earthquake was a 9.1-9.3 magnitude earthquake that triggered a series of devastating tsunamis. It killed over 225,000 people across 11 countries, with Indonesia, Sri Lanka, India, and Thailand impacted most severely. Waves as high as 30 meters inundated coastal communities. It was one of the deadliest natural disasters in history and caused global seismic effects.
The 2004 Indian Ocean tsunami caused widespread damage and loss of life. It was triggered by a large earthquake off the coast of Sumatra, Indonesia. Over 226,000 people were killed and approximately $10 billion in property damage occurred across 13 affected countries. Malaysia was also impacted, with 75 deaths, hundreds injured and displaced, and over 1500 homes and boats damaged despite being partially shielded from the full force of the waves. The tsunami highlighted the risks of future disasters and Malaysia's vulnerability despite not being as severely affected as other nearby countries.
1. A massive 9.3 magnitude earthquake struck off the coast of Sumatra, Indonesia on December 26, 2004, triggering a devastating tsunami across the Indian Ocean.
2. The tsunami waves reached heights of over 30 meters in some areas of Indonesia and over 10 meters in many other places. Over 230,000 people were killed or went missing across 14 countries.
3. Countries around the Indian Ocean have worked to establish tsunami early warning systems and increase public education to help save lives from future events, but the 2004 tsunami highlighted the massive destruction such an event can cause.
The document discusses the devastating 2004 Indian Ocean tsunami and lessons that can be learned from it. It provides background on tsunamis that have impacted India historically. It describes the large loss of life and damage from the 2004 tsunami, particularly in Tamil Nadu, the Andaman and Nicobar Islands, and among coastal communities like fishermen. It discusses whether tsunami walls could help protect small island countries in the future.
Alfred Wegener first proposed the theory of continental drift in the early 20th century, which suggested that the continents were once joined together in a supercontinent called Pangaea and have since drifted apart. However, his theory was rejected by other scientists at the time because he could not explain the force driving the continental movement. It was not until the 1940s with the discovery of sea floor spreading that scientists began to accept plate tectonics as the mechanism for continental drift.
1) The Snook Islands project reconstructed 10 acres of red mangroves, 2.8 acres of Spartina marsh, and 2.3 acres of oyster reef by transporting 1.2 million cubic yards of dredge spoil from Peanut Island over 1,560 barge loads to fill in areas of the Lake Worth Lagoon that had been dredged and bulkheaded.
2) The Lake Worth Lagoon had lost around 80% of its mangroves and shallow waters to dredging and filling over the past century. The Snook Islands project aimed to remediate this loss of habitat by reconstructing intertidal and shallow subtidal areas.
3) Spoil from
The 2004 Indian Ocean tsunami was one of the deadliest natural disasters in history. An undersea earthquake near Sumatra triggered a series of devastating tsunamis that impacted coastal areas around the Indian Ocean. Over 230,000 people were killed in multiple countries, with Indonesia, Sri Lanka, India, and Thailand hit especially hard. The tsunami caused widespread damage through the immense force of the waves and carried debris that destroyed homes, ports, roads, and fishing vessels. International aid efforts mobilized over $14 billion for relief and recovery in the affected regions.
1) The document discusses how different types of buildings are affected by earthquakes depending on the building's height and the frequency of seismic waves. Tall buildings are more affected by long period waves while small buildings are more affected by high frequency waves.
2) A demonstration is described showing how spaghetti noodles can be used to model how buildings of different heights resonate at different frequencies, with potential building damage.
3) Examples are given of the 1985 Mexico City earthquake where medium height buildings between 6-15 stories suffered most damage due to resonance with amplified seismic frequencies in the local subsurface geology.
The document provides information about tsunamis, including what causes them, how they behave in deep ocean versus shallow coastal waters, examples of destructive past tsunamis, and tips for preparing for tsunamis. It discusses how tsunamis are formed by earthquakes, landslides, volcanic eruptions and other events. It also explains that while tsunamis have long wavelengths and travel fast in deep ocean, they slow down and grow taller as they reach shallow coastal waters, potentially reaching over 100 feet high. Examples of destructive tsunamis discussed include those in Hawaii in 1975 and 1960, Alaska in 1964, Chile in 1960, and Peru in 1996.
This document provides information about tsunamis through several examples of destructive tsunamis throughout history. It discusses what causes tsunamis, how they propagate and grow in shallow water, and their devastating effects on coastlines. Specific tsunamis summarized include the 1929 Grand Banks tsunami that killed 29 in Newfoundland, the 1946 Aleutian tsunami that caused over $165 million in damage and deaths in Hawaii, and the 1996 Peru tsunami that struck cities along 590 km of coastline.
The document discusses tsunamis, including their causes, characteristics, and historical examples. It provides details on underwater earthquakes triggering tsunamis and describes tsunamis as consisting of multiple waves rather than a single wave. Examples of destructive tsunamis throughout history are given for various regions.
The largest tsunami on record was triggered by a 9.15 magnitude earthquake under the Indian Ocean on December 26, 2004. The tsunami waves reached heights of up to 49 feet and caused catastrophic damage across multiple countries in Southeast Asia and East Africa. Over 310,000 people lost their lives or were injured across Indonesia, Sri Lanka, India, Thailand and other nations impacted by the devastating waves. The earthquake and resulting tsunami are considered one of the deadliest natural disasters in history.
New microsoft office power point presentationbharatbarman
The document compares and contrasts the 2011 Japan tsunami and the 2004 Indian Ocean tsunami. It notes that while both disasters were deadly, the death toll was much higher for the 2004 tsunami which killed over 200,000 people across several countries. In contrast, the 2011 Japan tsunami has resulted in around 10,000 deaths reported so far. A key difference was that Japan had early warning systems and tsunami preparedness measures in place, while coastal areas in South Asia caught by the 2004 tsunami had little to no warning. Both earthquakes that triggered the tsunamis were extremely large at 9.0 magnitudes.
Earthquakes occur along fault lines when tectonic plates collide or scrape against each other. The San Andreas Fault in California is responsible for some of the most destructive quakes in U.S. history due to the North American and Pacific plates scraping past each other there. Major quakes can cause tsunamis, massive ocean waves caused by underwater seismic activity that can devastate coastal areas.
The document provides safety tips for tsunamis, including making an evacuation plan and list of essential items, elevating coastal homes above 10 feet to avoid most tsunami waves, taking precautions to prevent flooding, using local media for updates, and following instructions from local authorities. It advises that if a warning is issued, families in tsunami-prone areas should evacuate to higher ground and stay away from rivers and streams, while those on beaches should move to high ground if they feel the earth shaking.
This presentation took place on Tuesday 17th of march 2015 at Faculty of Engineering, Cairo University. I was asked by the professor to prepare a report and presentation about the lessons learned from Pakistan 2005 earthquake.
This document discusses tsunamis, which are giant waves caused by earthquakes or volcanic eruptions under the sea. Tsunamis can cause massive damage and loss of life by destroying homes and infrastructure. While impossible to prevent, their effects can be minimized through preparation measures like building in safe areas, establishing evacuation routes, and early warning systems. The document outlines dos and don'ts for before, during, and after a tsunami and emphasizes the importance of quickly evacuating coastal areas if a tsunami is detected or warned.
The document summarizes details of the 2011 Tōhoku earthquake and tsunami in Japan. It was a 9.0 magnitude earthquake that struck off the coast of Japan on March 11, 2011. It caused widespread damage including over 5,000 deaths and triggered a large tsunami with waves as high as 33 feet in some areas. The earthquake was one of the most powerful ever recorded and had devastating impacts across Japan such as fires, power outages, and nuclear plant issues.
The document provides information about tsunamis, including what causes them, warning signs, and safety precautions. It describes how tsunamis are caused by large displacements of water from earthquakes or volcanic eruptions. It lists evacuation plans and safety tips, such as knowing evacuation routes and staying away from coastal areas when there is a tsunami warning. The document also summarizes details about the devastating 2004 Indian Ocean tsunami and the 2011 Tohoku earthquake and tsunami in Japan.
A tsunami is a series of waves caused by the displacement of a large volume of water, generally in an ocean or large lake. Earthquakes, volcanic eruptions, and other disturbances under water have the potential to generate tsunamis. The 2004 Indian Ocean tsunami was one of the deadliest natural disasters in recorded history, caused by an earthquake under the Indian Ocean with a magnitude of 9.1-9.3 that killed over 227,000 people across 14 countries, mostly in Indonesia, Sri Lanka, India, and Thailand. It highlighted the need for improved warning systems for tsunamis in the Indian Ocean.
The 2004 Indian Ocean earthquake was a 9.1-9.3 magnitude earthquake that triggered a series of devastating tsunamis. It killed over 225,000 people across 11 countries, with Indonesia, Sri Lanka, India, and Thailand impacted most severely. Waves as high as 30 meters inundated coastal communities. It was one of the deadliest natural disasters in history and caused global seismic effects.
The 2004 Indian Ocean tsunami caused widespread damage and loss of life. It was triggered by a large earthquake off the coast of Sumatra, Indonesia. Over 226,000 people were killed and approximately $10 billion in property damage occurred across 13 affected countries. Malaysia was also impacted, with 75 deaths, hundreds injured and displaced, and over 1500 homes and boats damaged despite being partially shielded from the full force of the waves. The tsunami highlighted the risks of future disasters and Malaysia's vulnerability despite not being as severely affected as other nearby countries.
1. A massive 9.3 magnitude earthquake struck off the coast of Sumatra, Indonesia on December 26, 2004, triggering a devastating tsunami across the Indian Ocean.
2. The tsunami waves reached heights of over 30 meters in some areas of Indonesia and over 10 meters in many other places. Over 230,000 people were killed or went missing across 14 countries.
3. Countries around the Indian Ocean have worked to establish tsunami early warning systems and increase public education to help save lives from future events, but the 2004 tsunami highlighted the massive destruction such an event can cause.
The document discusses the devastating 2004 Indian Ocean tsunami and lessons that can be learned from it. It provides background on tsunamis that have impacted India historically. It describes the large loss of life and damage from the 2004 tsunami, particularly in Tamil Nadu, the Andaman and Nicobar Islands, and among coastal communities like fishermen. It discusses whether tsunami walls could help protect small island countries in the future.
Alfred Wegener first proposed the theory of continental drift in the early 20th century, which suggested that the continents were once joined together in a supercontinent called Pangaea and have since drifted apart. However, his theory was rejected by other scientists at the time because he could not explain the force driving the continental movement. It was not until the 1940s with the discovery of sea floor spreading that scientists began to accept plate tectonics as the mechanism for continental drift.
1) The Snook Islands project reconstructed 10 acres of red mangroves, 2.8 acres of Spartina marsh, and 2.3 acres of oyster reef by transporting 1.2 million cubic yards of dredge spoil from Peanut Island over 1,560 barge loads to fill in areas of the Lake Worth Lagoon that had been dredged and bulkheaded.
2) The Lake Worth Lagoon had lost around 80% of its mangroves and shallow waters to dredging and filling over the past century. The Snook Islands project aimed to remediate this loss of habitat by reconstructing intertidal and shallow subtidal areas.
3) Spoil from
The 2004 Indian Ocean tsunami was one of the deadliest natural disasters in history. An undersea earthquake near Sumatra triggered a series of devastating tsunamis that impacted coastal areas around the Indian Ocean. Over 230,000 people were killed in multiple countries, with Indonesia, Sri Lanka, India, and Thailand hit especially hard. The tsunami caused widespread damage through the immense force of the waves and carried debris that destroyed homes, ports, roads, and fishing vessels. International aid efforts mobilized over $14 billion for relief and recovery in the affected regions.
1) The document discusses how different types of buildings are affected by earthquakes depending on the building's height and the frequency of seismic waves. Tall buildings are more affected by long period waves while small buildings are more affected by high frequency waves.
2) A demonstration is described showing how spaghetti noodles can be used to model how buildings of different heights resonate at different frequencies, with potential building damage.
3) Examples are given of the 1985 Mexico City earthquake where medium height buildings between 6-15 stories suffered most damage due to resonance with amplified seismic frequencies in the local subsurface geology.
The document provides information about tsunamis, including what causes them, how they behave in deep ocean versus shallow coastal waters, examples of destructive past tsunamis, and tips for preparing for tsunamis. It discusses how tsunamis are formed by earthquakes, landslides, volcanic eruptions and other events. It also explains that while tsunamis have long wavelengths and travel fast in deep ocean, they slow down and grow taller as they reach shallow coastal waters, potentially reaching over 100 feet high. Examples of destructive tsunamis discussed include those in Hawaii in 1975 and 1960, Alaska in 1964, Chile in 1960, and Peru in 1996.
This document provides information about tsunamis through several examples of destructive tsunamis throughout history. It discusses what causes tsunamis, how they propagate and grow in shallow water, and their devastating effects on coastlines. Specific tsunamis summarized include the 1929 Grand Banks tsunami that killed 29 in Newfoundland, the 1946 Aleutian tsunami that caused over $165 million in damage and deaths in Hawaii, and the 1996 Peru tsunami that struck cities along 590 km of coastline.
The document provides information about tsunamis, including what they are, how they are caused, common misconceptions, and details about some significant historical tsunamis. It also discusses recommendations for preparing for, responding to, and recovering from tsunamis based on guidance from organizations like the American Red Cross.
Earthquakes are caused by the shaking and vibration of the earth's crust. They occur around the world and can cause devastating effects such as landslides, avalanches, tsunamis, and damage to buildings and infrastructure. While some regions are more prone to earthquakes, they are difficult to predict precisely and can strike with little or no warning. Scientists study earthquake mechanisms and seismic waves to build more earthquake resistant structures, but risk can never be fully eliminated.
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A few minutes of intense shaking, followed by a devastating tsunami, producing widespread destruction. FEMA's best-case scenario, 13,000 people will lose their lives, (Schultz, 2015). The question is not if it's going to happen, it's when. The countdown to catastrophe is on for the Pacific Northwest. We're talking about the Cascadia Subduction Zone. Throughout this paper, I will discuss the who, what, where, when, and how this overdue megaquake will strike.
The Cascadia subduction zone is a 620-mile-long crack in the earth's crust. It is in the pacific northwest where the North American tectonic plate meets the Juan de Fuca plate, (Tarbuck, Lutgens, Tasa, 2017). Tectonic plates are pieces of crust that move across the earth's surface over millions of years, (Oskin, 2015). The subduction zone is where two tectonic plates meet. One eventually bends underneath the other, which is what we see in the North Pacific. The Juan de Fuca plate is sliding under the weaker, North American plate. Eventually, the North American plate will buckle, result in a devastating earthquake, followed by massive Tsunami.
Subduction zones are found all along the edge of the Pacific in what is called, "The ring of fire." Off the coasts of Washington, Canada, Alaska, Russia, and Indonesia birthed the most devastating earthquakes, tsunamis and volcanic eruptions in history, (Oskin, 2015). The bigger the subduction zone, the higher magnitude of the earthquake. A subduction zone earthquake with a magnitude of 7.5 or greater will likely produce a tsunami. The Cascadia subduction zone is a big one. It runs 620 miles long and 62 miles wide. It has all the ingredients necessary to produce massive devastation.
So how do we know that the Pacific Northwest is in danger? Tsunamis are a direct result of an earthquake, volcanic eruption or a massive landslide. The once dubbed, "Orphan Tsunami," hit the eastern coast of Japan on January 27th, 1700, (Atwater et al., 2015). The year 1700 in the Pacific Northwest was considered prehistory, meaning there were no written records of events. Japan, on the other hand, have produced numerous ancient writings of stories that told of flooded fields, wrecked houses, fire, a shipwreck, and evacuations. The Japanese knew that tsunamis were a result of an earthquake, and because they didn't feel any shaking prior, they called the event a high tide. At the time, it wasn't known that tsunamis could occur from earthquakes that happened from faraway lands. Outsiders of Northwestern North America scarcely knew of its existence. At that time, leading European geographers left that part of the map blank. So, for this mystery, the Japanese didn't even know the Pacific Northwest existed, much less that it had produced the earthquake that generated the tsunami, (Atwater et al., 2015).
The Chilean earthquake that struck on May 22, 1960, generated a tsunami that surged a ...
Tsunami is a Japanese word meaning harbor wave. Tsunamis are series of large waves generated by earthquakes, landslides, volcanic eruptions, or other disturbances that displace large volumes of water. The first recorded tsunami was in 1480 BC in the Mediterranean. Tsunamis cause devastating damage when they reach coastal areas due to their ability to flood large areas inland with fast-moving water. Proper warning systems and evacuation of coastal areas can help reduce loss of life from tsunamis.
This document discusses tsunamis, including:
1) The 2011 Tohoku earthquake and tsunami in Japan caused over 15,000 deaths and $235 billion in damage.
2) Tsunamis are produced by earthquakes at subduction zones, where the rapid uplift of the seafloor generates a wave of ocean water.
3) Important characteristics of tsunamis include their long period of 20-60 minutes, long wavelength of over 800 km, and ability to flood coastlines for 10-15 minutes, behaving differently than wind waves.
The document discusses various types of tsunamis including those caused by landslides, meteorological conditions, and human activities. It provides examples of destructive meteotsunamis and discusses attempts to artificially trigger tsunamis through explosions. The characteristics of tsunamis are explained, noting that while waves have short wavelengths in deep ocean, they have much longer wavelengths and travel very quickly. The document also discusses drawback effects, forecasting tsunami probability, anatomy of tsunamis, facts about tsunamis, and preparation and safety during and after tsunamis.
A tsunami is a series of enormous ocean waves generated by earthquakes, landslides, volcanic eruptions, or meteor impacts that displace large volumes of water and cause catastrophic damage when they reach land. Tsunamis are very difficult to detect when they approach coastal areas out in the open ocean, and can travel at over 500 mph. Areas near fault lines in the Pacific Ocean called "seismic zones" are particularly at high risk of experiencing tsunamis. On December 26, 2004, a 9.3 magnitude earthquake in the Indian Ocean triggered a devastating tsunami that killed over 230,000 people across 14 countries, with deaths reported as far away as Africa.
A tsunami is a series of water waves caused by the displacement of a large volume of water, often from earthquakes, volcanic eruptions, landslides or other disturbances below or above water. Tsunami waves have a very long wavelength and can cause enormous destruction in coastal areas, with wave heights over tens of metres. The 2004 Indian Ocean tsunami was one of the deadliest natural disasters, killing over 290,000 people across 14 countries.
The document discusses evidence that mega-tsunamis from volcanic eruptions and flank collapses destroyed ancient civilizations over 50,000 years ago. Specifically, it notes that as the last glacial period ended around 12,000 years ago, stress imbalances triggered eruptions of stratovolcanoes located on shelves surrounding Asia. Landslides of these volcanoes would have generated mega-tsunamis over 100 meters high, capable of wiping out coastal settlements and islands across the northern hemisphere. The waters northeast of Taiwan in particular contain evidence of undersea volcanoes and faults that could have historically generated tsunamis impacting ancient civilizations.
This document discusses plate tectonics and related landforms, earthquakes, and volcanoes. It begins by describing the four main types of plate boundaries and associated landforms such as mid-oceanic ridges, trenches, and island arcs. It then covers causes of earthquakes including sudden stress release along faults, and factors that influence earthquake damage such as magnitude, building design, and population density. Prediction methods like elastic rebound theory and seismic gaps are also mentioned. Finally, it discusses volcanoes, noting where they form at plate boundaries and hotspots, how scientists monitor and predict eruptions, associated hazards from lava to tsunamis, and ways to reduce risks like controlling lava flows and using hazard maps.
The document discusses tsunamis, which are large sea waves caused by earthquakes, volcanic eruptions, landslides, or cosmic impacts. Tsunamis are among the most destructive natural disasters and can cause massive loss of life and property damage. The deadliest tsunami on record was the 2004 Christmas tsunami in the Indian Ocean, which killed an estimated 300,000 to 350,000 people after a 9.2 magnitude earthquake generated a series of large waves. Proper planning through early warning systems and evacuation of coastal areas can help reduce loss of life from future tsunamis.
Earthquakes are caused by movements in the earth's crust that generate shaking and vibrations. They can cause significant damage depending on their magnitude and intensity. While earthquakes occur frequently around the world, some areas are more prone to them than others. Major earthquakes since 1900 include a 9.5 magnitude quake in Chile in 1960 and a 9.0 magnitude quake off the coast of Indonesia in 2004 that triggered a devastating tsunami. Scientists have gained significant understanding of where earthquakes are likely to occur but still cannot reliably predict specific future events. Structures can be designed to better withstand shaking but no building can be completely earthquake-proof.
This document provides information about earthquakes. It discusses that earthquakes are caused by the sudden release of energy stored in the Earth's crust along fault lines. Major earthquakes usually occur along belts that coincide with tectonic plate boundaries, particularly the Circum-Pacific Belt. Earthquakes can also be caused by human activities like reservoir construction. The effects of earthquakes include ground shaking, rupture, landslides, tsunamis, liquefaction, and fires. The document outlines safety rules both before, during, and after an earthquake to minimize injury.
A tsunami is a giant wave caused by sudden movement under the ocean. Tsunamis travel very fast, like jet planes, so there is little time to escape when they hit shorelines. They can cause widespread death, homelessness, and economic problems. The most destructive tsunami was in 2004 in the Indian Ocean, where an earthquake in Indonesia generated waves that killed thousands across 11 countries. This document provides information about tsunamis, their effects, terminology, safety, detection methods, history in the US, and recent events.
The document provides information about tsunamis, including how they are formed by earthquakes, volcanic eruptions, or landslides under water. It discusses how tsunamis can affect people mentally, emotionally, and financially by destroying homes and infrastructure. The document outlines tsunami awareness steps before, during, and after a tsunami occurs, such as evacuating to higher ground if warned and helping others after the tsunami passes.
A tsunami is a series of waves generated by large displacements of water, often caused by earthquakes, volcanic eruptions, landslides or other disturbances. Tsunami waves have extremely long wavelengths of up to hundreds of kilometers and grow dramatically in height and destructive power when reaching shallow coastal waters. Notable historic tsunamis include the 2004 Indian Ocean tsunami that killed over 230,000 people across 14 countries making it one of the deadliest natural disasters in modern times. Current research focuses on better understanding why some quakes trigger tsunamis while others don't and improving tsunami forecasting across ocean basins.
This document summarizes information about tsunamis from multiple sources. It discusses how the 2004 Sumatra earthquake generated a tsunami that killed over 280,000 people due to the lack of an early warning system in the Indian Ocean. It then provides definitions and characteristics of tsunamis, explaining how their long wavelengths allow them to travel vast distances with little energy loss. As they reach shallow coastal waters, their speed decreases while height increases due to shoaling. Tsunamis can be generated by earthquakes, volcanic eruptions, landslides, explosions, and meteorite impacts, with most caused by displacement of the seafloor during subduction zone earthquakes. Examples of deadly tsunamis from Alaska and
This is a PowerPoint presentation about the 1964 earthquake that hit Alaska on Good Friday, March 27th, at 5:37 pm. A 9.2 on the Moment Magnitude Scale, this was the second largest earthquake in recorded history, generated huge tsunamis, killed 131 people, and cost over 300 million dollars in property damage.
The document appears to contain a single year - 2013 - with no other context or details provided. In just one word, it does not give enough information to generate a multi-sentence summary.
The document discusses how business continuity has gone mainstream and provides examples of business continuity in mainstream media. It also addresses how this has impacted expectations from employees and challenges for business continuity programs. The presentation covers various topics related to ensuring business continuity programs adapt and succeed as the discipline becomes more mainstream.
William Moorehead, President, All Clear Emergency Management Group
Using situational analysis, participants will learn to identify common legal issues in emergency
management and how to enhance response through agreements. This session will examine common
legal issues encountered within emergency management and emergency response including liability and
the formation of mutual aid agreements. The audience will analyze hypothetical scenarios and news
stories to identify potential liability issues. The session will highlight the challenges and barriers to
implementing agreements, benefits of prepositioned contracts, and the importance of putting agreement
in place now before they are needed. The goals of the session are to review the fundamentals of
liability, examine common legal issues, discuss best practices, and analyze situations common in
emergency management.
Speaker: Kathryn Koelemay, Medical Epidemiologist, Public Health – Seattle & King County
All hospitals should be prepared to receive pediatric patients in a mass casualty incident and to provide
appropriate short-term acute care and more definitive management, depending upon the nature of the emergency and the extent of its impact on the region. Hospitals of the King County (WA) Healthcare
Coalition are in the process of implementing a regional pediatric disaster response plan, with the goal of
providing consistent, efficient and age-appropriate medical care to pediatric patients at every County
hospital with emergency services in an MCI that involves children. Our “pediatric toolkit,” which was
recognized as a 2010 NACCHO Model Practice winner, suggests guidelines for development of the
hospital‟s pediatric response plan. The regional plan also includes countywide adoption of a color-
coding system based on a length-based resuscitation tape to expedite accurate medication and equipment
deployment.
Speaker: Dick Bower, Building/Fire Safety/Emergency Management Director, City of Gig Harbor
Lack of coordination between members of the emergency management community adversely affects our
ability to protect citizens. While a host of federal, state and local sources provide the emergency
management community with guidance through the four phases of emergency management, such
guidance falls short of emphasizing the full value of an established multi-agency coordination (MAC)
entity and system. By building relationships between the governmental agencies, response partners,
private sector, non-governmental and faith based organizations that make up the community, effective
multi-agency collaboration spanning the entire emergency management continuum can be developed.
Such collaboration provides effective, efficient, and cost-effective emergency management across the
full continuum of emergency management activities. By redefining Multi-Agency Coordination to
include pre-incident/event collaboration planning, mitigation, response and recovery activities can be
greatly improved.
Speakers: David Shannon, Program Manager/ Community Disaster Education, American Red Cross
Donna Platt, Emergency Education Program Manager, Hearing, Speech & Deafness
Center
This session will provide an overview on the Disaster Preparedness Skills Training for Deaf, Deaf-Blind
and Hard of Hearing event which was coordinated by several organizations (emergency responders and
non-profit agencies). This event which was held twice in Seattle turned out to be educational for both
emergency responders and attendees as they learned each other‟s needs and responsibilities in
emergency preparedness. Also this event drew attention from other community based organizations and
emergency responders who expressed an interest in setting up in their location. Tips on setting up an
event and mini-activities will be given. Also pros and cons (or lessons learned) will be discussed.
Sharon Badger, Community Education Coordinator, Northwest Renal Network
This presentation will provide an overview of the end stage of renal disease and the treatments that must
be maintained by the patient until there is a kidney transplant or the patient dies. The presentation will
encourage the disaster planning community to incorporate the special requirements of the kidney
community into local and regional emergency and disaster plans. It will encourage the emergency
managers to utilize both the Network and the individual facilities to create a plan that can best serve this
vulnerable population
Speaker: Bob Mellinger, President, Attainium Corp
Chances are that while you read this, an unexpected disaster is causing an organization stress and
confusion and is affecting its long-term ability to provide products and services to its customers. Are the
organization‟s leaders prepared to handle it? Will they be able to recover? Disasters of every shape, size,
look and feel happen all the time, affecting businesses, people's jobs, lives and families. This session
has been designed to put you in the throes of a real-life disaster situation, as it unfolds. You will make
the critical decisions any organization will have to make - and deal with the consequences of those
The document discusses emergency preparedness planning between counties and municipalities in Washington State, outlining requirements for comprehensive emergency management plans and how counties can coordinate planning efforts with local cities and towns. Examples are provided of different counties' emergency management organizations and hazards they prepare for, along with lessons learned around overcoming challenges in the planning process and benefits derived from completing a coordinated plan.
Speakers: Mary Schoenfeldt, Public Education Coordinator, City of Everett Office of Emergency
Management
Rebekah Green, Associate Director, Resilience Institute
CJ Huxford, Project Coordinator, Resilience Institute
Riley Grant, Project Coordinator, Resilience Institute
Public Education Campaigns come and go. Some are good, even great, but if we don‟t deliver the
message correctly, no one really hears us. The message is only as good as the messenger. Everett
Office of Emergency Management, Snohomish County, and Western Washington University teamed up
to research the effectiveness of Who Depends on You, Are You Prepared for Disaster? And, they found
some interesting results. For instance, in some areas more people have plans for their pets than for their
children. Does that tell us about parents or about our messaging? Does our message catch the attention of those with a high school education more than those with a college education? Is our message missing
important recipients? Come hear the results of the research, discuss their meaning, and participate to
help us design message delivery systems that work. If a public education message falls in the forest and
no one is listening…
Speaker: Althea Rizzo, Geologic Hazards Program Coordinator, Oregon Emergency Management
Public education has consistently been shown to be an effective emergency preparedness and mitigation
strategy when done well. This presentation will give the attendees an effective road map to developing,
implementing and evaluating a public education and outreach program. Using real world examples, the
presenter will show best practices and how to design your outreach campaign to create positive
preventative action by the public.
Speakers: Joan Gomberg, Research Geophysicist, US Geological Survey
Brian Sherrod, Research Geologist, US Geological Survey
Tim Walsh, Division of Geology & Earth Resources, Chief Hazards, Washington State
Department of Natural Resources
This session will communicate, in lay terms, the latest scientific discoveries relevant to assessing and
responding to earthquake hazards in the Pacific Northwest. We will describe recent advances in
understanding of regional faults, forecasts of the ground shaking and impacts from earthquakes on these
faults, and lessons learned for the Pacific Northwest from recent significant earthquakes around the
globe. The scientific programs underway and planned also will be discussed, emphasizing their linkages
to improved earthquake hazard assessments and mitigation and response tools.
Speaker: Dave Nichols, Volunteer Manager & Workforce Manager, Public Health of Seattle & King
County
The MRC is a relative newcomer to the disaster response world. It is another tool in your emergency
management toolkit; but only if you know about it and how it works during a medical emergency or
disaster. This presentation has been designed to introduce, inform, and answer questions about the
Medical Reserve Corps program and how it fits into the disaster. I will also offer some ways that you
can involve them in your exercises to help them learn your area and your operation.
Speakers: Mark Fedderson, Lieutenant, Tacoma Police Department
Frank Krause, Sergeant, Tacoma Police Department
Birney Elementary – Teacher Homicide occurred on February 26, 2010 in Tacoma, Washington. This
presentation discusses the dispatch, intervention, investigation, and partnerships at work.
Speakers: Lauren Zeigler, Lead Case Manager, Catholic Community Services of Western
Washington
Barbara Nelson, Public Education Outreach Specialist - Pierce County Department of
Emergency Management
Susan Vaughn, Regional Chief of Operations, Catholic Community Services of Western
Washington
Victims of disasters often require case management services to help them regain self-sufficiency and
return to their pre-disaster condition. Prior to Hurricanes Katrina and Rita there was no federal authority
to support case management of disaster victims. Consequently, case management was provided through
donated funds and by voluntary agencies. For disasters on a much smaller scale, such as an apartment
fire or flooding, recent experience in Washington State has demonstrated a similar need for a system that
assesses individual and family needs and assists with connecting them with the appropriate services to
address immediate circumstances and longer-term needs. Pierce County and King County have both
developed models to respond to typically unmet needs in their communities.
Speaker: Ted Buehner Warning Coordination Meteorologist National Weather Service
This session provides an extension of information presented in the basic session (see D4). Topics
include: - How to obtain and use National Weather Service (NWS) all-hazards weather support -
Significant Pacific Northwest weather patterns - Storm Surveys – what they are, when are they done
and the local emergency manager‟s participation in them - Washington‟s Presidentially weather-related
disaster rankings and fatality statistics - How to use the NWS web page such as interpreting the weather
radar and satellite imagery, climate/historical data, spotter reports, new digital forecasts and use in your
GIS operations (live demo is planned) - StormReady and TsunamiReady communities – what do they
mean to you and how to apply and get recognized for the work you do - Address your questions.
Speakers: Kathy Woods, Director, Business Continuity, Premera
Jennie Clinton, Program Manager, Crisis Management & Personal Preparedness, Premera
Our presentation will provide a case study on our approach to overall preparedness the personal aspect
being a large component; b. Program component; c. How we engage execs, employees, and community
partners. In this presentation we will: 1. Share how we are getting our employee base more prepared to
support keeping the company in business; 2. How to motivate and provide incentives for employees to
take action; and, 3. Demonstrate how we partner and engage the public sector to do this.
Speaker: Nimisha Ghosh Roy, Program Developer and Coordinator, Cross Cultural Health Care
Program
The evolving demographics of our communities as well as the dramatic challenges surfacing in the field
of emergency management have resulted in the magnification of issues facing the provision of emergency services for racial and ethnic minority communities. Issues of diversity are present in every
human interaction and must be acknowledged and addressed competently in all emergency management
activities. The Cross Cultural Health Care Program (CCHCP) has worked with organizations and
communities across the nation addressing topics such as effective cross cultural communication skills
for diverse populations and disaster training for medical interpreters. In 2010 CCHCP hosted a
community event to explore the challenges in emergency management facing communities in the Puget
Sound. Through an interactive presentation style involving multimedia and case studies from CCHCP
projects, this presentation will define and discuss the imperative for cultural competency and share best
practices and strategies for culturally competent emergency management.
Speaker: Chris Utzinger, Emergency Logistics Program Manager, Washington State Emergency
Management Division
This presentation provides insight and guidance for local distribution of resources using Community
Points of Distribution (CPODS). The target audience for this session is volunteer organizations
interested in providing distribution assistance and emergency managers that need help getting CPOD
planning started in their jurisdictions. The session is based upon the IS-26 Guide to Points of
Distribution course provided by FEMA‟s Independent Study program and includes an overview of
CPOD layouts, staffing, operations, and public interactions. A sample CPOD kit is presented
highlighting needed personal protective gear and other equipment. The Adopt-A-Pod program, wherein
jurisdictions work with volunteer groups to staff and manage CPODs, is also highlighted. Audience
interest and understanding is enhanced by a hands-on sand table exercise where participants design their
own CPOD layout. Audience participation is highly encouraged, especially with attendees that have
dealt with distribution issues in previous events and can provide case studies for discussion.
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1. Tsunami Hazards in Cascadia :
by
Timothy J. Walsh
Washington Department of Natural
Resources
Division of Geology and Earth Resources
Partners in Emergency
Preparedness
April 27, 2011
2. •On April 1, 1946, a
magnitude 8.0 (Mw)
earthquake with the
source in the
Aleutian Islands to
the south of Unimak
Island generated a
tsunami that
destroyed this five-
story lighthouse,
located 9.8 m above
sea level.
3. •Only the
foundation and
part of the
concrete sea wall
remained. All five
occupants were
killed. The waves
deposited debris
as high as 35 m
above the sea.
Although little
damage occurred
in Alaska, except
at Scotch Cap, the
tsunami was one
of the most
destructive ever to
occur in the
Hawaiian Islands.
Photo credit: U.S.
8. •At least 24 people were killed here, many of whom were children
playing by the waterfront. The tragedy of the 1946 tsunami
prompted the U.S. Coast and Geodetic Survey to establish the
Tsunami Warning System
9.
10. Abridged from
Seismicity of the
United States,
1568-1989
(Revised), by
Carl W. Stover
and Jerry L.
Coffman, U.S.
Geological
Survey
Professional
Paper 1527,
United States
Government
Printing Office,
Washington:
1993.
Prince William Sound, Alaska
1964 March 28 03:36:14 UTC (March 27
local) Magnitude 9.2
11. Valdez sits on the edge of an outwash delta 150 km from the epicenter. During
the shaking, the unstable, saturated material failed. A slice of the delta, 1,220
m long and 183 m wide, slid into the sea, carrying the docks and part of the
town with it. The slide generated a wave which slammed the waterfront 2 to 3
minutes after the onset of the quake. The wave demolished the rest of the
waterfront, destroyed the fishing fleet, and reached 2 blocks into town, killing 30
people
12. Tsunami damage from the
Highway 109 bridge over 1964 Alaska earthquake
Copalis River
The wave here was about
10-12 feet.
Highway 109 bridge
House torn apart over Joe Creek
at Pacific Beach
13. This earthquake also generated a Pacific Ocean-wide tsunami that killed 110
people, 8 here in Crescent City, CA. Note fire in background. This event led to
the opening of a second tsunami warning center in Palmer, Alaska.
14. 1993
Okushiri
Island
A view of tsunami and related fire damage on southeast Okushiri
Island in the community of Aonae. Photo orientation is looking
northeast. Numerous fires broke out following the tsunami, adding
to the property loss and misery. More than 120 people were killed
in Japan (Okushiri and Hokkaido Islands) by the tsunami.
15. On the west side of Okushiri Island many locations experienced a maximum runup of
over 20 m. This small valley leading to the ocean experienced a spectacular runup of 31
m. Note the debris in the foreground, including a broken steel reinforced concrete utility
pole. Discolored and dead plants and grasses are evident on the hillside. This well-
studied earthquake and tsunami led to significant advances in modeling tsunamis.
16.
17. Placer
River Silt
Earthquake-induced
ground crack
Drowned forest in Girdwood, Alaska, killed in 1964
A.D. 1700
Ground
surface
1,100 year
old ground
surface
from Brian Atwater
Drowned forest along the Copalis River,
Washington, killed in A.D. 1700
18. Right, subsided marsh
along the Niawiakum River,
Tsunami sands
southwest Washington.
Below, note pitfalls of
working in tidal marshes.
A.D. 1700 ground
surface
19. The realization that Cascadia was active was instrumental to the creation of
the National Tsunami Hazard Mitigation Program, which develops tsunami
inundation maps for vulnerable coastlines. These are based on a combination
of numerical modeling, and , where possible, paleoseismology.
23. Tsunami parade at Hiro.
Storm surge trace
REMEMBER
THE PAST
Tsunami monument
from Nobuo Shuto
24. A TRAGEDY OF FOREIGN TOURIST WHO
COULD NOT UNDERSTAND WARNING
Her last position
from Nobuo Shuto
25. Washington has a limited historical record, so we rely on
modeling to establish tsunami hazard zones
26. A tsunami generated by a Cascadia
subduction zone earthquake will
arrive in less than 45 minutes. For
these events, as was the case in
Banda Aceh, the earthquake must be
the warning. Citizens must know
where to evacuate from and where to
evacuate to, and must do so quickly
and on foot.
Note the long peninsulas or spits of
low-lying ground. Ocean Shores
peninsula is 7 miles long and Long
Beach peninsula is 20 miles long with
little or no high ground over those
distances. For these areas, tsunami
defenses are appropriate.
27. After
TWO BUILDINGS
IN AONAE,
1993
During
Before (北海道新聞社)
from Nobuo Shuto
28. THE TWO
BUILDINGS
THAT REMAINED.
Tsunami trace
This building stopped a house and boats.
29. Those two buildings
and other Japanese
tsunami defense
structures formed
the basis of a study
of buildings that
survived
devastating
tsunamis when
everything else in
the area was
destroyed.
30. DEFENCE
STRUCTURES
SEA WALLS
TSUNAMI BREAKWATERS
TSUNAMI GATE
HIGHTENING OF RIVER DIKES
from Nobuo Shuto
38. At Minami-
Sanriku town,
an apartment
building was
situated right
next to the
coast and
designated as
an evacuation
building as
shown by
evacuation
signs, but there
were traces
that tsunami
also had
reached the 4th
floor.
39. This three-story
building (below) was
the disaster
management center
of the town which
was also designed
to function as a
tsunami evacuation
building. At the time
of tsunami, about
thirty municipal
officials evacuated
to the rooftop but
only ten of them
survived. A young
female official who
kept delivering
evacuation message
to the villagers until
the last moment has
not been found yet.
40. We formed a partnership
with FEMA and the
Applied Technology
Council to provide
building code style
guidance for building
facilities to withstand a
magnitude 9 earthquake
and be suitable for
vertical evacuation.
Planning for the right size
earthquake is critical.
41. Project Safe Haven:
Tsunami Vertical
Evacuation
Long Beach Peninsula/Pacific County
42. Safe Haven Options (from FEMA 646):
Towers –
• Limited Space
• Blocks Views
• Few Options for Shelter
Buildings –
• Expensive
• Better get it right the first time!
• Very Large, Likely to Block Views
• May require Private Development
• Incentives for Height?
Berms –
• Least Expensive Option
• Can be Multi-Purpose
• May be Placed to Limit View Blocking
43. Vertical Evacuation Safe
Haven Project
• Community-based,
‘bottom-up’ approach
• All options (buildings,
towers, berms, etc.) are on
the table for consideration
Common Themes:
• School Safety
• Seniors and special needs
populations
• More conservative travel
times