At least 340,000 Americans died from radioactive fallout between 1951 and 1973

Domestic nuclear testing wreaked havoc on thousands of families.

At least 340,000 Americans died from radioactive fallout between 1951 and 1973
Wikimedia Commons
  • Hiroshima and Nagasaki resulted in the deaths of hundreds of thousands. But new research shows that domestic U.S. nuclear tests likely killed more.
  • The new research tracked an unlikely vector for radioactive transmission: dairy cows.
  • The study serves as a reminder of the insidious and deadly nature of nuclear weapons.

When we think of nuclear disasters, a few names probably come to mind. There's the Chernobyl disaster, which killed around 27,000 people, although estimates are fuzzy. After Fukushima, there were no deaths due to radiation poisoning, but this event occurred relatively recently, and radiation poisoning often kills slowly over decades. When the U.S. dropped atomic bombs on Hiroshima and Nagasaki, estimates put the death toll at around 200,000 people, but again, exact numbers are difficult to calculate.

One name that almost certainly didn't come to mind is Nevada. When the Soviet Union detonated their first atomic bomb in 1949, the U.S. was shocked into action. America's prior nuclear testing had been carried out in the Pacific, but it was logistically slow and costly to conduct tests there. In order to maintain dominance over the growing Soviet threat, the U.S. selected a 1,375 square-mile area in Nye County, Nevada.

This was an ideal spot for several reasons. It was closer than Bikini Atoll. The weather was predictable and very dry, reducing the risk that radioactive fallout would be dispersed by rainstorms. It was sparsely populated. There was an understanding that there would be some amount of risk posed to nearby civilians, but it was deemed acceptable at the time. The trouble is, our understanding of radioactive fallout was still in its infancy. It was a catch-22; the only way to learn more was to test nuclear weapons.

New research with a wider scope

Subsidence craters at the Nevada test site. These craters result from underground weapons testing, typically from nuclear weapons. Federal Government of the United States [Public domain], via Wikimedia Commons

In the 1950s, the U.S. government downplayed the danger of radioactive fallout, asserting that all radioactivity was confined to the Nevada test site. Despite this, a national estimate attributed 49,000 cancer deaths to nuclear testing in the area.

But the results of new research suggest that this number is woefully inaccurate. Using a novel method, and today's improved understanding of radioactive fallout, Keith Meyers from the University of Arizona discovered that U.S. nuclear testing was responsible for the deaths of at least as many — and likely more — as those killed by the nuclear bombs in Hiroshima and Nagasaki. Specifically, between 340,000 and 690,000 Americans died from radioactive fallout from 1951 to 1973.

Prior studies generally looked at the areas surrounded the Nevada test site and estimated the deaths caused by fallout from the area. This number was relatively low, owing to the dry, predictable weather mentioned earlier. However, the bulk of the deaths were actually dispersed throughout the country, primarily in the Midwest and Northeast regions. These deaths were caused by an unfortunate synergy between meteorology, radiation, and — perhaps oddly enough — cows.

An unforeseen vector of radiation poisoning

Through an unforeseen chain of events, dairy cows became a vector for radioactive poisoning. ROBYN BECK/AFP/Getty Image

Out of all the radioactive elements produced by a nuclear explosion, iodine-131 was the biggest killer. I-131 has an eight-day half-life, tends to accumulate in the thyroid gland, and emits beta and gamma radiation. While alpha radiation is generally weak and doesn't penetrate material very well, beta and gamma radiation are highly energetic and shoot through clothing and flesh, ripping up DNA as it goes along.

Prior studies had examined the radioactive fallout dispersed by low-altitude winds, which would generally settle around the Nevada test site. However, a significant amount of I-131 was caught up in high-altitude winds. These winds carried the radioactive particles to other regions of the U.S., where it mixed with rain clouds.

The now-radioactive rain fell onto the grasslands in the Midwest and Northeast. Then, cows ate the now-radioactive grass. The cows then produced radioactive milk. Dairy practices during the study period were different than they are today — most people drank milk that had recently been extracted from local cows.

Thanks to a National Cancer Institute database that contains broad data on radiation exposure, Meyers was able to track the amount of I-131 found in local milk and compare this with the number and nature of deaths on a county level. In this way, Meyers was able to determine that a significant number of these deaths were due to drinking poisoned milk. These civilians would have had no idea that the milk they were drinking had been irradiated by nuclear explosions hundreds of miles away.

Ironically, the area around the Nevada test site didn't have this problem. Although they too drank fresh milk from local cows, they imported hay from other parts of the country. Since their cows weren't eating irradiated hay, the local Nevadans took in significantly less radioactive material than their less-fortunate, distant countrymen.

Although our understanding of radiation and nuclear fallout is much improved since the dawn of the nuclear age, the study serves as a warning of the insidious nature of nuclear weapons. Containing nuclear fallout is challenging, even when you know where all of the vectors of radioactive transmission are. The complexity and intertwining nature of our ecological and social systems means that words like "clean," "precise," or "surgical" will likely never apply to nuclear weapons.

A landslide is imminent and so is its tsunami

An open letter predicts that a massive wall of rock is about to plunge into Barry Arm Fjord in Alaska.

Image source: Christian Zimmerman/USGS/Big Think
Surprising Science
  • A remote area visited by tourists and cruises, and home to fishing villages, is about to be visited by a devastating tsunami.
  • A wall of rock exposed by a receding glacier is about crash into the waters below.
  • Glaciers hold such areas together — and when they're gone, bad stuff can be left behind.

The Barry Glacier gives its name to Alaska's Barry Arm Fjord, and a new open letter forecasts trouble ahead.

Thanks to global warming, the glacier has been retreating, so far removing two-thirds of its support for a steep mile-long slope, or scarp, containing perhaps 500 million cubic meters of material. (Think the Hoover Dam times several hundred.) The slope has been moving slowly since 1957, but scientists say it's become an avalanche waiting to happen, maybe within the next year, and likely within 20. When it does come crashing down into the fjord, it could set in motion a frightening tsunami overwhelming the fjord's normally peaceful waters .

"It could happen anytime, but the risk just goes way up as this glacier recedes," says hydrologist Anna Liljedahl of Woods Hole, one of the signatories to the letter.

The Barry Arm Fjord

Camping on the fjord's Black Sand Beach

Image source: Matt Zimmerman

The Barry Arm Fjord is a stretch of water between the Harriman Fjord and the Port Wills Fjord, located at the northwest corner of the well-known Prince William Sound. It's a beautiful area, home to a few hundred people supporting the local fishing industry, and it's also a popular destination for tourists — its Black Sand Beach is one of Alaska's most scenic — and cruise ships.

Not Alaska’s first watery rodeo, but likely the biggest

Image source: whrc.org

There have been at least two similar events in the state's recent history, though not on such a massive scale. On July 9, 1958, an earthquake nearby caused 40 million cubic yards of rock to suddenly slide 2,000 feet down into Lituya Bay, producing a tsunami whose peak waves reportedly reached 1,720 feet in height. By the time the wall of water reached the mouth of the bay, it was still 75 feet high. At Taan Fjord in 2015, a landslide caused a tsunami that crested at 600 feet. Both of these events thankfully occurred in sparsely populated areas, so few fatalities occurred.

The Barry Arm event will be larger than either of these by far.

"This is an enormous slope — the mass that could fail weighs over a billion tonnes," said geologist Dave Petley, speaking to Earther. "The internal structure of that rock mass, which will determine whether it collapses, is very complex. At the moment we don't know enough about it to be able to forecast its future behavior."

Outside of Alaska, on the west coast of Greenland, a landslide-produced tsunami towered 300 feet high, obliterating a fishing village in its path.

What the letter predicts for Barry Arm Fjord

Moving slowly at first...

Image source: whrc.org

"The effects would be especially severe near where the landslide enters the water at the head of Barry Arm. Additionally, areas of shallow water, or low-lying land near the shore, would be in danger even further from the source. A minor failure may not produce significant impacts beyond the inner parts of the fiord, while a complete failure could be destructive throughout Barry Arm, Harriman Fiord, and parts of Port Wells. Our initial results show complex impacts further from the landslide than Barry Arm, with over 30 foot waves in some distant bays, including Whittier."

The discovery of the impeding landslide began with an observation by the sister of geologist Hig Higman of Ground Truth, an organization in Seldovia, Alaska. Artist Valisa Higman was vacationing in the area and sent her brother some photos of worrying fractures she noticed in the slope, taken while she was on a boat cruising the fjord.

Higman confirmed his sister's hunch via available satellite imagery and, digging deeper, found that between 2009 and 2015 the slope had moved 600 feet downhill, leaving a prominent scar.

Ohio State's Chunli Dai unearthed a connection between the movement and the receding of the Barry Glacier. Comparison of the Barry Arm slope with other similar areas, combined with computer modeling of the possible resulting tsunamis, led to the publication of the group's letter.

While the full group of signatories from 14 organizations and institutions has only been working on the situation for a month, the implications were immediately clear. The signers include experts from Ohio State University, the University of Southern California, and the Anchorage and Fairbanks campuses of the University of Alaska.

Once informed of the open letter's contents, the Alaska's Department of Natural Resources immediately released a warning that "an increasingly likely landslide could generate a wave with devastating effects on fishermen and recreationalists."

How do you prepare for something like this?

Image source: whrc.org

The obvious question is what can be done to prepare for the landslide and tsunami? For one thing, there's more to understand about the upcoming event, and the researchers lay out their plan in the letter:

"To inform and refine hazard mitigation efforts, we would like to pursue several lines of investigation: Detect changes in the slope that might forewarn of a landslide, better understand what could trigger a landslide, and refine tsunami model projections. By mapping the landslide and nearby terrain, both above and below sea level, we can more accurately determine the basic physical dimensions of the landslide. This can be paired with GPS and seismic measurements made over time to see how the slope responds to changes in the glacier and to events like rainstorms and earthquakes. Field and satellite data can support near-real time hazard monitoring, while computer models of landslide and tsunami scenarios can help identify specific places that are most at risk."

In the letter, the authors reached out to those living in and visiting the area, asking, "What specific questions are most important to you?" and "What could be done to reduce the danger to people who want to visit or work in Barry Arm?" They also invited locals to let them know about any changes, including even small rock-falls and landslides.

Your genetics influence how resilient you are to the cold

What makes some people more likely to shiver than others?

KIRILL KUDRYAVTSEV/AFP via Getty Images
Surprising Science

Some people just aren't bothered by the cold, no matter how low the temperature dips. And the reason for this may be in a person's genes.

Keep reading Show less

Harvard study finds perfect blend of fruits and vegetables to lower risk of death

Eating veggies is good for you. Now we can stop debating how much we should eat.

Credit: Pixabay
Surprising Science
  • A massive new study confirms that five servings of fruit and veggies a day can lower the risk of death.
  • The maximum benefit is found at two servings of fruit and three of veggies—anything more offers no extra benefit according to the researchers.
  • Not all fruits and veggies are equal. Leafy greens are better for you than starchy corn and potatoes.
Keep reading Show less
Quantcast