A Report On Marine Geophysicists

The most noticeable difference between a tsunami and a hurricane is the cause of each. A tsunami is the aftermath of an underwater earthquake or volcanic eruption. The force of the earthquake or eruption, along with the moving of the tectonic plates, sends large amounts of water in all directions. The waves can be thousands of feet high when they reach the shoreline. These giant waves can arrive at a moment's notice with no warning. The tsunami is a large natural phenomenon originating from the ocean, but it is not the only phenomenon to start in the ocean.

Tsunamis are caused by earthquakes underneath the ocean, which can results in gigantic waves that cause devastation and change the Earth’s surface by causing radiation and causing underwater landslides. In the article “Is Santa Catalina Island Sinking or Rising?” it describes how an effect of tsunamis. It states, “A tsunami could have struck the coast from Catalina when the underwater landslide occured” (Los Angeles Times 2). Therefore, tsunamis can strike coasts and can create landslides underwater, changing the ocean floor by creating caves and canyons. Also, tsunamis can wear away beaches. When giant waves crash into coasts of masses of land, they can wear away the coast. Finally, tsunamis can cause radiation. In the article “Dangerous Tsunami Threat off U.S. West Coast,” it explains, “It [the tsunami] also damaged a nuclear power plant, causing a meltdown and spreading dangerous radiation in the area” (Los Angeles Times). Consequently, tsunamis can destroy and interfere with human made buildings which may contain toxic gases which may be released into the air and cause damage the environment. Incidentally, damaging the environment can lead to killing plant and animal life, and the Earth in that area could potentially become barren and

Ever since I was an infant, I have spent almost every summer on my father's boat in Ocean City, New Jersey. Whether it be fishing or jumping off the boat to go swimming, I have always been familiar and had an immense love for both the boat and the ocean. Up until this year, I had never known that there was an option for me to be able to take online classes at my high school. Since I have already taken all of the science classes that are honors that were available, I needed to find another science class. I had found the honors oceanography class in the catalog online, and I instantly signed up for the course. I enrolled because of my interest for the ocean and it's inhabitants. Although I'd like to think that I know a lot about the ocean, I

The Boxing Day Tsunami had occurred on the 26th of December 2004. The tsunami had started under water, in the Indian Ocean. The cause of the tsunami was that the Indo-Australian plate had subducted below the Eurasian plate, this process is called a convergent plate boundary. This resulted with an underwater earthquake, making waves approximately 20-30 metres high and travelling at speeds up to 500km/ph. Theses waves travelled throughout Indonesia, Sri Lanka, India and Thailand and left each country in terrible conditions. The earthquake that occurred underwater had

Tsunamis occur when an earthquake happens in the ocean and the energy goes to the water creating huge waves. Tsunamis are very dangerous they can be so strong that they wash away the city, harm thousands, and cause hundreds of thousands to billions of dollars in damage. “A giant tsunami along the West Coast would wash away coastal towns, destroy U.S. Highway 101 and cause $70 billion in damage. More than 100 bridges would be lost, power lines toppled and coastal towns isolated. Residents would have as few as 15 minutes’ notice to flee to higher ground, and as many as 10,000 would die” (Dangerous tsunami threat off U.S. West Coast). This shows what kind of damage this geo-process can

Since these earthquakes are caused by tectonic plate movement therefore displacing the ocean floor they are almost always accompanied by massive ocean waves, sometimes reaching heights of over 100 ft and reaching speeds of 500 mph, known as seismic sea waves or more commonly known as Tsunamis4. Alongside the catastrophic events that megathrust earthquakes ensue on an affected region these colossal Tsunami waves further destruct costal lines in their path, sometimes reaching many miles inland.

Distant tsunami: A series of gravity waves in the ocean originating from a source typically thousands of kilo-meters away from the shoreline that is inundated. These waves are produced by the displacement of the entire water column of the ocean by an underwater earthquake, landslide, volcanic eruption, or extra terrestrial impact.

The Tsunami that took place after the initial quake was caused by a portion of seabed rupturing upwards, and displacing a large portion of the water being displaced. This water traveled at 450 miles, at 8 feet tall, to the Chilean and Peruvian coast. Early viewers of the tsunami later reported waves being up to 10 feet tall. This rupture was believed to be caused by 2 unusually dense pieces of seabed that had been previously undetected by scientists, and consequently caused a large displacement of water. There were also small ruptures of seismic

As survivors from the quake rushed around in fear and confusion, they were greeted by yet another disaster. Shortly after the earthquake, a tsunami occurred. The tsunami’s waves struck the coastline beginning at twenty feet. But as more waves hit the coast, the height of the tsunami grew to just under forty feet, taking out everything that hadn’t already been destroyed by the earthquake, reducing the entire city to rubble. The tsunami stretched across sixty-two miles of coastline near Messina, and another twenty-four miles of coastline near Calabria. The damage from the tsunami was greater near the Calabria coast, where waves were higher and the water quickly swallowed houses and bridges, and flooded rivers. The tsunami that occurred in Messina still holds the title for one of the biggest tsunamis in today’s history. Recently, however, geologists have revisited origin of the tsunami, which is now widely debated. Some

Tsunamis occur when there is sudden movement in an extensive body of water such as earthquakes, landslides on the sea floor, major volcanic eruptions or meteorite impacts. The most common source of a tsunami is earthquakes, which are another type of geomorphic hazard that is caused by the friction and stress that tectonic plates put on each other. Tsunamis primarily occur in coastal or island regions where there is a tectonic border or what is known as the ring of fire. As shown in the diagram below the ring of fire is located along the coastal and island regions of the world.As a result of the Pacific Plate diving beneath the Eurasian plate, on March 11, 2011, there were 2 geomorphic hazards, a magnitude-9 earthquake struck north Japan, which caused a deadly tsunami that reached heights of 39 meters. The destructive dilemma was dubbed ‘The Great Sendai Disaster’. The earthquake was caused by multiple centuries of stress on the tectonic plates surrounding the island. The earthquake caused a tsunami that reached the height of 39 meters (128 feet). Japanese scientists had previously discovered that there was another tsunami just like the one in 2011 that took place in 869 AD. But their warning was unhindered. The tsunami, which occurred in 869 AD, was caused by the same tectonic fault as the 2011 tsunami. The epicenter of the earthquake was off the northeast cost of Japan leading to a devastating tsunami that killed many and left many wishing they were. The massive earthquake caused an upward wave that headed towards the city of Sendai. Researches have recently uncovered a thin layer of clay that lubricated the fault zone causing the deadly tectonic slip, thus creating a tsunami that could wipe out an entire city as it did in 2011.The aftermath of the 2011 tsunami and earthquake was not pretty; it caused many deaths, injuries, traumas, financial difficulties, destruction of property, health bills and the destruction of the landscape as a whole. The natural disaster caused nearly 16,000 casualties and there are an estimated 2,500 people still reported missing. Although drowning caused most deaths others include, crushed by debris, suicide and diseases caused by nuclear radiation (cancer) spilled from nuclear

THESIS: The tsunami is a dangerous natural disaster that should be analyzed and studied to prevent unnecessary deaths.

From the case study above we can see that human influences were the main cause in the severity of the impact, but that’s not always the case, physical factors are just as important. This can be seen in the great Sumatra- Andaman earthquake which took place on the 26th of December 2004 and registered a 9.1 magnitude, one of the third biggest recorded quakes. The subduction of the Indo-Australian plate under the Burma plate triggered the tsunami responsible for the greatest loss of life in a tectonic event. A 15-20m slip occurred along 1600km of fault line in two phases over a period of around 3-4 minutes, the longest rupture ever recorded in an earthquake. The focus was located just 30km below sea level, which resulted in serval billion tonnes of water being displaced across

The 2004 Indian Ocean and Tsunami, everyone has heard about this tragic experience before. It is the third-largest earthquake ever recorded on a seismograph and had the longest duration of faulting ever observed, between 8.3 and 10 minutes. A Tsunami is a long high sea wave caused by an earthquake, submarine landslide, or other disturbance. For the book, Wave, there was family of four where the brother, mom and dad went to Thailand to spend their winter break. The daughter had decided to spend her winter break in New York City. In Thailand, there was a Tsunami that had struck the resort where the family had been staying at. The dad and his son went out to go and help others while the mom stayed back in the hotel lobby. Or what was left of it.

The most severe impacts were observed on the Chilean coastline adjacent to the epicenter from San Antonio – Tirua, and 670 km offshore on the Juan Fernandez Archipelago (Synolakis, 2011; Yamazaki and Cheung, 2011). The tsunami hit many areas close to the epicenter within 30 minutes of the main event, however due to bathymetry and coastline shape, tsunami directions, impacts, and arrival times vary. (Synolakis, 2011; Yamazaki and Cheung, 2011). For example, Talcahuano Harbor located in The Bay of Concepcion 100 kilometers south of the epicenter experienced an impact from a resonated 129 minute period oscillating wave three hours after the main event (Yamazaki and Cheung, 2011). Resonance such as this occurred in various areas along the Chilean coastline, and was caused by standing and partial standing wave systems produced along the coast due to wave reflection between the continental shelf and the headlands, resulting in radiated tsunami energy to become trapped over the continental margin (Yamazaki and Cheung, 2011).

A tsunami is a series of huge waves occurring when there is a major disturbance on the ocean floor. Tsunamis often occur due to earthquakes, volcanoes, or landslides (Park 16). Underwater earthquakes may produce waves that travel in all different directions. Some tsunamis lose power and die out under water, others may produce large waves as they approach land. Tsunamis may look like an onrushing tidal wave as they approach land, but do not occur because of tides (Park 6). Their walls of water can move across the open ocean at speeds of up to 560 miles per hour. When the waves hit the coast, they can reach up to 100 feet (Park 5). The tsunami in Japan is believed to have occurred after two of Earth’s tectonic plates collided in the