
How a Favored Migrant Route Became Invasive Species Superhighway to US
Based on facts, either observed and verified firsthand by the reporter, or reported and verified from knowledgeable sources.
Newsweek AI is in beta. Translations may contain inaccuracies—please refer to the original content.
The Darién Gap, long a perilous route for millions of migrants traveling north toward the United States, has also become a pathway for the northward spread of the New World screwworm—a parasitic fly now challenging decades of containment efforts.
The flesh-eating fly, whose larvae burrow into the wounds of living animals, has surged north through Central America since 2022, recently reaching the Mexican states of Oaxaca and Veracruz—roughly 700 miles from the Texas border. Scientists and federal officials now warn that the screwworm could cross into the U.S. as early as this summer if containment efforts falter.
For decades, the United States and Panama maintained a bi-national barrier to block the parasite at the Darién, using a program that dropped millions of sterilized screwworm flies over the jungle to prevent breeding. That system began unraveling in 2022, amid pandemic-era supply-chain disruptions and record human and animal movement through the region.
Aerial view showing migrants walking through the jungle near Bajo Chiquito village, the first border control of the Darien Province in Panama, on September 22, 2023. The clandestine journey through the Darien Gap usually lasts...
Aerial view showing migrants walking through the jungle near Bajo Chiquito village, the first border control of the Darien Province in Panama, on September 22, 2023. The clandestine journey through the Darien Gap usually lasts five or six days, at the mercy of all kinds of bad weather. More than 390,000 migrants have entered Panama through this jungle so far this year, far more than in all of 2022, when there were 248,000, according to official Panamanian data. More
Photo by Luis ACOSTA / AFP) (Photo by LUIS ACOSTA/AFP via Getty Images
Between 2021 and 2024, more than 1.2 million migrants crossed the Darién, according to data from Panama's National Migration Service and UNHCR. The crossings peaked at 520,000 in 2023 before falling to 302,000 in 2024. U.S. officials believe that mass movement contributed to operational breakdowns in the region's screwworm control infrastructure.
"There are many challenges in this containment and eradication program," Phillip Kaufman, a professor of entomology at Texas A&M University, said in an interview with Newsweek. "Producing sufficient numbers of sterile flies and getting them released in the correct places and at the right time is critical. If the flies move further north than the isthmus in southern Mexico, it becomes more and more challenging to contain them."
The screwworm, scientifically known as Cochliomyia hominivorax — roughly translated as "man-eater"—was eradicated from the U.S. by 1982 using the Sterile Insect Technique (SIT), which involves releasing sterilized male flies to prevent reproduction and collapse the population.
The parasite targets livestock, wildlife, pets — and occasionally humans — by burrowing into open wounds. Infected animals are once again being found in areas previously considered screwworm-free, triggering emergency responses from both governments.
Human and Animal Migration a Factor
Though the vast majority of screwworm cases are in livestock, human infections have surged in the wake of the parasite's northward spread. Nicaragua reported 30 human cases by February 2025. Costa Rica saw 42 confirmed cases between January and May, including two deaths. Honduras recorded 40 cases and three deaths, while Guatemala and Mexico have also reported infections.
In humans, the infestation—known as myiasis—typically occurs in individuals with untreated wounds, particularly those living in rural areas or sleeping outdoors. Treatment often requires surgical removal of larvae and follow-up care to prevent secondary infection or tissue loss.
While the root causes of the screwworm's northward march remain under study, scientists suspect a combination of human migration, illegal animal movement and weather patterns.
Migrants walk by the jungle near Bajo Chiquito village, the first border control of the Darien Province in Panama, on September 22, 2023. The clandestine journey through the Darien Gap usually lasts five or six...
Migrants walk by the jungle near Bajo Chiquito village, the first border control of the Darien Province in Panama, on September 22, 2023. The clandestine journey through the Darien Gap usually lasts five or six days, at the mercy of all kinds of bad weather. More
LUIS ACOSTA/AFP via Getty Images
"Additional movement of animals and humans has helped facilitate the expansion of the flies' location," Sonja Swiger, a professor and extension specialist at Texas A&M AgriLife, told Newsweek. "This includes both the moving of infested animals unknowingly and by disrupting the operations of COPEG to release SIT flies in the area."
A Department of Agriculture (USDA) spokesperson told Newsweek the disruption was caused "both by the movement of infested animals unknowingly and by interference with COPEG's operations to release sterile flies in the area."
The USDA said it is working with regional governments to strengthen veterinary inspections and education. But officials noted that controlling illegal livestock movement often falls under national security, making enforcement more complex.
"We have raised this concern directly with officials in each affected country," a USDA official told Newsweek. "While regional governments acknowledge that uncontrolled animal and human movement undermines containment efforts, monitoring and controlling this activity is complex."
Recent enforcement appears to be having an effect. Under President Donald Trump's return to office in early 2025, crossings through the Darién fell sharply. Only 408 people crossed in February, and just 194 in March, effectively emptying camps along once-overrun migration routes, including Lajas Blancas.
Risk of Reintroduction
U.S. officials suspended live animal imports from Mexico in May after screwworm detections in cattle. The USDA has invested $21 million to retrofit a Mexican fruit-fly production facility in Metapa to manufacture an additional 60 to 100 million sterile screwworms weekly. That would double current output from a long-operating facility in Panama, which has been running at capacity.
"Should the screwworm continue moving north, having access to many more flies than the existing facility in Panama can produce will be important to protect U.S. agriculture," a USDA spokesperson told Newsweek. "We are exploring possible options for increasing our capacity to produce these sterile insects, which could include a facility here in the United States."
Secretary of Agriculture Brooke Rollins looks on as President Donald Trump signs executive orders in the Oval Office of the White House on April 9, 2025, in Washington, D.C.
Secretary of Agriculture Brooke Rollins looks on as President Donald Trump signs executive orders in the Oval Office of the White House on April 9, 2025, in Washington, D.C.The U.S. government now plans to open a second sterile fly production center in Texas by the end of 2025. Located at Moore Air Base, less than 20 miles from the Mexican border, the $8.5 million facility would eventually produce up to 300 million flies per week. Agriculture Secretary Brooke Rollins said on Wednesday the move is necessary to "protect the American cattle herd from the devastating threat of New World screwworm."
Texas alone houses 12 million cattle and calves—more than any other U.S. state—part of a thriving livestock industry valued at $15 billion. If screwworms re-enter Texas, the economic losses could be staggering. A USDA model projects that a statewide outbreak could cost producers $732 million annually and trigger $1.8 billion in broader economic costs. Nationwide, screwworm eradication since the 1960s has saved the livestock industry over $1.5 billion per year.
"These are not speculative numbers—they reflect the hard-earned lessons from the last century," Kaufman, the entomology professor, said.
A Long Road to Re-Eradication
Despite new investment, containment is already slipping. "It is going to take a long time to put this genie back in the bottle," Andrew Short, chair of the entomology department at the University of Florida, said in an interview with Newsweek. "We do not have good means of monitoring for screwworm aside from looking for already-infected animals."
Short called for urgent improvements. "We desperately need better trapping and surveillance methods to complement animal inspections," he added.
The sterile insect technique remains a cornerstone of eradication efforts, but experts say new technologies are in development to improve its efficiency. One potential breakthrough is a genetically modified strain that eliminates female flies during production, allowing for twice the output of sterilized males.
Cows are seen standing in a feedlot on June 14, 2023 in Quemado, Texas.
Cows are seen standing in a feedlot on June 14, 2023 in Quemado, Texas."This is done by preventing the development of the female flies when they are mass produced," Kaufman explained. "The result is near doubling of the production of flies in the sterile fly production facility."
The USDA said it would consider building a companion fly-breeding center alongside the new Texas facility, joining existing sites in Panama and Mexico. Together, these could generate as many as 500 million sterile flies per week to outnumber and outcompete wild screwworms.
Despite the costs of containment, USDA economists estimate that maintaining the eradication program delivers annual economic benefits exceeding $1 billion—far outweighing the expense of operations like the COPEG fly factory in Panama. In contrast, responding reactively to an outbreak, rather than preventing it, could drain public and private resources for decades.
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National Geographic
2 days ago
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A Swiss village was buried under a mountain. This town could be next.
In the past century, scientists have observed more rockfalls and avalanches in the Alps, a looming threat to nearby villages. In this aerial view, rubble and ice fill a portion of the Loetschental Valley following a landslide on June 3, 2025 in Blatten, Switzerland. Over 317 million cubic feet of rubble, mud, and ice fell on to Blatten on May 28. Photograph by Robert Hradil, Getty Images Last month, Lukas Kalbermatten-Ritler stood in a hamlet overlooking the small Swiss village of Blatten opposite the Birch Glacier, holding up his camera phone up in disbelief. 'It was like a bomb went off,' says Kalbermatten-Ritler, who's home and historic third-generation family-owned Hotel Edelweiss was destroyed on May 28. 'There were black rocks coming like a wall over the glacier, like it was a big hand taking the village. This was the moment I stopped filming. I didn't want to film when my village was falling.' 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It sits in the shadow of an unstable cliffside called Spitze Stei could trigger a landslide with twice the ice and rock debris that flattened Blatten. Scientists say it should have fallen by now. 'We can't predict exactly when disasters like this will happen,' says Matthias Huss, senior glaciologist at the Swiss Federal Institute of Technology and director of the Swiss glacier monitoring network. Even with the best rockfall, landslide, and avalanche monitoring systems in the world, Alpine towns remain in uncertain danger. Magazine for all ages starting at $25/year In the worst-case scenario, over 700 million cubic feet of limestone and marl will come crashing down into Lake Oeschinen, itself a result of landslides 3,200 years ago. The splash would send a wave 2.5 miles into the center of Kandersteg, covering around 25 percent of the town, including hotels, homes, and the school. Other less-severe, likelier, models show smaller, still destructive debris flows surpassing safety dams built by the village, according to Nils Hahlen, head of the natural hazard division for the Office of Forest and Natural Hazards in the Swiss canton, or state, of Bern. The landslide that devastated the town of Blatten was unexpected. In other, nearby villages, scientists have identified unstable cliff faces that might trigger similar tides of rock, water, and debris in the future. Photograph by Michael Buholzer, Keystone/AP 'But mountain people are robust. They don't move out of their villages because of changing threats unless authorities decide it's too risky to stay,' says Markus Stoffel, a geomorphologist at the University of Geneva who grew up near Blatten and Kandersteg. Most of the town's 1,300 residents remain. On mountain watch Four hours into what was billed as a 'short' (eight-mile) hike, I rest on a mossy stump while my 75-year-old mountain guide smokes a pipe. Mountain guides don't eat much, Fritz Loretan tells me. He's also a man of few words (clocking it down the trail in loafer sneakers with no tread), and when he talks about the looming threat in Kandersteg, he explains: 'When you grow up in the mountains, then you are used to them, and you won't feel safe in other places.' In 2018, while paragliding over Spitze Stei, Loretan's friend saw 'a cut in the mountain,' and alerted authorities. Experts realized the outer rock section could fall at any moment. That was the year Spitze Stei became the most watched rock in Switzerland via high-tech drones, radar surveys, GPS, and cameras. 'At Spitze Stei the main water sources are snowmelt and rain. The exact amount of water in the mountain is one of the unknown factors,' says Hahlen. Since Earth's last ice age, rockfaces have been routinely dislodged from Alpine peaks as a result of natural movement. But in the past century, scientists have seen more rockfalls and avalanches. Glaciers and permafrost—the high-altitude frozen soil, rock, and sediment that acts like glue to hold the mountains together—are melting as a result of the warming temperatures caused by greenhouse gas emissions. A view of a landslide in Brienz, three days apart, from November of last year. As the region warms, ice and frozen soil are melting and unsticking the glue that once held parts of the mountain together. Photograph by Gian Ehrenzeller, Keystone/AP (Top) (Left) and Photograph by Gian Ehrenzeller, Keystone/AP (Bottom) (Right) As this icy glue melts, it allows water to penetrate cracks in the mountain, build pressure, and eventually rupture, triggering more frequent and severe landslides, rockslides, rockfalls, and avalanches, especially after intense rain and snow, another hazard of warming temperatures. 'In the next few years and decades, we expect an increase in risk from permafrost rock,' says Felix Pfluger, chair of landslide research at the Technical University of Munich. While catastrophic rock and snow fall can go virtually unnoticed in the remote regions of Alaska, Siberia, or northern Canada, they're an existential threat to many Alpine communities. The landslide that covered Blatten isn't the first tragedy in the Alps from a rockfall. This past June, residents of the Swiss village of Brienz/Brinzauls evacuated for the fourth time in two years from a rockslide threat (after debris stopped just shy of the village in 2023). Eight hikers and ten homes in the valley of Bondo didn't survive a devastating landslide in 2017. Stoffel says he expects more chain-reaction disasters with bigger consequences in the Alps—rock avalanches overloading glacier ice and causing it to liquify and slide down the slope, like in Blatten. His research shows 'a clear tendency for such [catastrophic chain-reaction] events to become more frequent in a warming world,' he says. '...especially after heavy rain.' A view of Kandersteg, Switzerland in October, 2023. While the region is being closely monitored, it remains safe. Photograph by Noemie Vieillard, Hans Lucas/Redux 'If you ask the older people in the village, they'll tell you there was always falling debris,' says Kandersteg's Mayor Maeder René-François. Growing up in Kandersteg, he remembers poking a pole into the cracks between ice and snow to search for bodies after an avalanche took out half a hotel in high season. There's a long history of rockfall and landslides, he says, as recent as 2023 and even this past May five died here in an avalanche. 'With climate change, it's happening faster. It rains harder, the days are hotter, and the fog sets in thicker over the mountain,' he says. 'But people here are not scared, it's life in the mountains. They respect that they must act in the correct way and follow the evacuation plan.' Since 2021, Kandersteg has enforced a ban on all new construction to minimize potential damage in the village district, closed a section of town, and built dams to reroute lake water. 'Big disasters normally start smaller. Instabilities with rock fall over a certain time start with cracks opening. A mountain doesn't just disappear out of the blue. There are always precursor signs,' says Stoffel. 'And if you take them seriously and observe the changes continuously, then, then you may not be able to protect the buildings or the village, but you can save lives.' While no one knows exactly when or what section of Spitze Stei will start sliding down the mountain, when it starts to crumble, residents and tourists should have at least 24 to 48 hours to evacuate. On a warm mid-June day, I followed tourists with hiking packs and poles to a mountain chalet built in 1880 and pulled up a lunch chair under an apple-red umbrella that matched a nearby Swiss flag and took in the brilliant turquoise of Lake Oeschinen–glistening and undisturbed by falling rocks, for now. Swimmers and paddlers snap selfies; a bride and groom pose by cows grazing near a roped-off section of the beach—their bells clanging measure with the chirping birds. 'None of them know they're right under it,' my server, David Brunoldi, told me when I asked him which rock is Spitze Stei. He points to the 9,800-foot frosty peak above us. 'More rocks are coming down every day.' Brunoldi says mountain people stay in Kandersteg for generations because it's home. On this picture-perfect, rugged Alpine terrain, where rockfall has always been a risk, his grandfather worked and died on a mountain train. Last year alone, an increasing 2.8 million cubic feet of rock crumbled down into the lake. 'No need to worry though, Brunoldi adds. 'It's not falling today.'