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Deirdre Langeland - Meltdown: Earthquake, Tsunami, and Nuclear Disaster in Fukushima

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Meltdown: Earthquake, Tsunami, and Nuclear Disaster in Fukushima: summary, description and annotation

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Deirdre Langelands Meltdown explores for middle grade readers the harrowing story of the deadly earthquake, tsunami, and nuclear meltdown that caused the 2011 Fukushima power plant disasterOn March 11, 2011, the largest earthquake ever measured in Japan occurred off the northeast coast. It triggered a tsunami with a wall of water 128 feet high. The tsunami damaged the nuclear power plant in Fukushima triggering the nightmare scenario--a nuclear meltdown.For six days, employees at the plant worked to contain the meltdown and disaster workers scoured the surrounding flooded area for survivors.This book examines the science behind such a massive disaster and looks back at the people who experienced an unprecedented trifecta of destruction.

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The author and publisher have provided this e-book to you for your personal use only. You may not make this e-book publicly available in any way. Copyright infringement is against the law. If you believe the copy of this e-book you are reading infringes on the authors copyright, please notify the publisher at: us.macmillanusa.com/piracy.

For my mother, Ricky Langeland, who taught me how to be curious, do my research, and think like a scientist.

Most of the area of Japan is made up of four major islands The largest of - photo 3

Most of the area of Japan is made up of four major islands. The largest of these, Honshu, is divided into five distinct regions. The northernmost, the area most affected by the March 11, 2011, earthquake, is known as Tohoku (shown here in dark blue).

Fukushima. To people all around the world, the name has come to mean one thing: nuclear disaster. They remember several long weeks in March 2011 when they turned on the news every day and saw thick smoke billowing from nuclear reactors, carrying potentially deadly radiation into the environment.

In reality, Fukushima is a prefecture in Japana government district similar to a state in America. Its the southernmost prefecture in the Tohoku region, an area of about 25,000 square miles that is famous for its remote beauty. Dense forests and volcanic peaks define the landscape. Fog drifting in from the northern Pacific Ocean blankets its rice paddies, apple orchards, and cattle farms. Before the disaster, Fukushima was known as a lush farming area that supplied produce, dairy products, and seafood to the rest of Japan. But in the space of a few days, all of that changed.

Roughly midway along the Fukushima coast, six nuclear reactors were lined up in a neat row along the shore. Owned by the Tokyo Electric Power Company, or TEPCO, they were part of the Fukushima Daiichi power plant. (Dai-ichi means one in Japanese. A second power plant, called Fukushima Daini, meaning two, was located about 6 miles down the shore.)

On March 11, 2011, the plants were hit by a one-two punch: First, there was the earthquake, the strongest ever measured in Japan. Then came the tsunami, an inescapable wall of water that killed tens of thousands. Together, they crippled the reactors at Fukushima Daiichi, setting off a chain of events that threatened the safety of millions.


Like most disasters, the Great Tohoku Earthquake and tsunami came with little warning. There had been foreshocks, smaller earthquakes that shook the countryside for days before the main event, but theres nothing unusual about earthquakes in Japan. On average, Japan experiences about two thousand earthquakes that are strong enough to be felt every year. In real time, its impossible to know whether an earthquake is its own event or a precursor of something bigger on the way. Only afterward, once the Big One has come and gone, can seismologists go back and see the pattern that led up to it. And so, the millions of residents of Tohoku went about their business that afternoon in March as they had on all of the others before.

That was certainly true for Ryoichi Usuzawa, a sixty-two-year-old grandfather with salt-and-pepper hair who was working from his home in the town of Otsuchi. He was pleased with himself because he had just finished writing a report and was binding it into a folder and adding tabs. His wife was downstairs with the family dog, a Shiba Inu named Taro. It seemed like a pretty ordinary Friday afternoon, and Ryoichi was happy to be wrapping up the weeks work.

But what happened next was anything but ordinary. Suddenly, there was a[n] enormous earthquake, he later told a journalist. Nothing like what wed experienced in the pasta truly terrifying quake. It made me wonder if our house would collapse; if I might die. The printer, computer, bookshelf, recordseverything came tumbling down. I couldnt move a step.

When the shaking stopped, just a little past 2:50 P.M., Ryoichi did what he had probably done after the hundreds of smaller earthquakes that had shaken his house in the past: He began to clean up the mess. Even when his wife told him there was a tsunami warning, he didnt think it was a serious threat. After all, his family had lived there for decades and the water had never reached their land. For the next half hour, he straightened up and tried to fix the television as his sons, his daughter-in-law, and a grandchild gathered outside the house. He tried to calm his nerves, which had been jangled by the unusually strong earthquake.

Then he heard his wife shouting: Oto-San, run from the tsunami!


Like hundreds of thousands of others who lived along the coast of Tohoku, Ryoichi was at the start of what would be a long, terrifying ordeal. By nightfall, much of his hometown, including his own house, would be swallowed by waves.

But Ryoichi had no way of knowing that. He only knew that his wifes last words as she ran for safety were Look after Taro! So he headed up the stairs, in the direction he had last seen the dog going.

Moments later, muddy water surged up the stairs after him.

Friday, March 11, 2011, 2:46 P.M.

Reactor Status

Reactor 1: Fully operational

Reactor 2: Fully operational

Reactor 3: Fully operational

Reactor 4: Shut down for inspection

Reactor 5: Shut down for inspection

Reactor 6: Shut down for inspection

Standing on Earth, its difficult to appreciate its movement. The entire planet spins on its axis at more than 1,000 miles per hour (mph) and hurtles along its orbit through space at 66,660 mph. Its no wonder, then, that those of us sitting on its surface hardly notice the slow creep of its tectonic plates. But miles beneath the soil and sand, the mountains and oceans, Earths lithosphere is broken into a clumsy jigsaw puzzle of rock. The puzzle pieces, called tectonic plates, sit on the asthenosphere, a layer of Earth that shifts and flows.

Rocks in the asthenosphere are under so much pressure that they move in and out of solid formsometimes they are solid rocks, sometimes liquid magma. Resting on top of this constantly changing layer, the plates creep over, under, and past each other at a rate so slow it would make a snail blush.

More than anything else, Japan has been shaped by the push and pull of plate tectonics. Just off its east coast, deep beneath the seafloor, giant chunks of Earths lithosphere and crust are being sucked beneath the country in a process called subduction. Rock from the subducting plates turns to magma when it reaches the mantle, creating hot spots that, over millennia, melt through the crust and break through as lava, forming volcanoes. That upwelling magma is responsible for the breathtaking mountainous landscape of Japan, and those subducting plates cause most of the earthquakes that shake the country.

Japan is an archipelago, a cluster of islands that sit on a particularly active spot in the tectonic neighborhood, where a thin finger of the North American Plate extends down between the Eurasian and Pacific Plates. The largest of the islands, Honshu, is in an especially precarious position, straddling the boundary between the Eurasian and North American Plates. To the east of the island, the North American and Pacific Plates meet in a section of the seafloor called the Japan Trench. There, the Pacific Plate slides beneath the North American Plate in whats known as a subduction fault.

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