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Biologist stunned by unusual materials found packed inside bird nest: 'The oldest layer is as old as me'

Biologist stunned by unusual materials found packed inside bird nest: 'The oldest layer is as old as me'

Yahoo23-03-2025
Eurasian coots are making their nests out of our trash, reported ZME Science.
Researchers in Amsterdam have discovered that Eurasian coots are building nests using plastic waste dating back decades.
One nest contained 635 artificial items, including a 1994 FIFA World Cup souvenir and a 1996 McDonald's McChicken container.
"The oldest layer is as old as me — all my life, a bird was nesting here," said Auke-Florian Hiemstra, a biologist at the Naturalis Biodiversity Center in Leiden, Netherlands.
Unlike natural nests that decay each year, these plastic structures can last for decades. Some coots are even reusing old plastic nests rather than building new ones — an unusual behavior for these birds.
These nests reveal how deeply plastic has worked its way into nature. Like scientists use tree rings to study past climates, these nests contain a timeline of human trash production.
Unlike natural materials that decompose within months, the plastic in these nests won't break down for hundreds of years. This represents a dramatic shift in how wild animals interact with their environments.
While birds adapt to use these materials, we don't yet know how toxic chemicals in plastics might affect developing chicks or adult birds.
These "accidental archives" also serve as physical proof of how long our everyday trash stays in the environment — the McDonald's wrapper you tossed years ago might still be in a bird's home today.
Companies are developing biodegradable packaging alternatives that break down naturally if they end up in the environment. Many communities now offer plastic recycling programs that keep waste out of waterways.
Should tourists be responsible for cleaning up their own trash?
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In most cases
It depends on the place
No, they shouldn't
Click your choice to see results and speak your mind.
You can help by reducing single-use plastic in your daily life. Choose reusable water bottles and shopping bags. Pick up plastic litter when you see it, especially near water.Support businesses that use eco-friendly packaging. And remember: Proper disposal of plastic items means they're less likely to end up in a bird's nest.
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Wild tattoos of 2,500-year-old Siberian ‘ice mummy' revealed for first time
Wild tattoos of 2,500-year-old Siberian ‘ice mummy' revealed for first time

New York Post

time5 days ago

  • New York Post

Wild tattoos of 2,500-year-old Siberian ‘ice mummy' revealed for first time

The ornate tattoos of a 2,500-year-old Siberian 'ice mummy' have finally been revealed using advanced imaging technology, according to a report. High-resolution images derived using infrared technology show the long-dead 50-year-old woman was inked-up across her body with tribal animal designs, the BBC reported. 5 The mummy was pulled from the permafrost near Russia's Altai Mountains in 1993. M. Vavulin Advertisement The intricate and ornate tats show leopards, a stag, a rooster, and a griffin-like creature. Her arms were tattoo'd with the leopard and stag, the half-lion half-eagle beast was on her leg, and the rooster was tatted on the mummy's thumb, according to researchers. 'The insights really drive home to me the point of how sophisticated these people were,' the study's lead author Dr. Gino Caspari, from the Max Planck Institute of Geoanthropology, told BBC. Advertisement 5 Left forearm tatoo. D. Riday 5 Right forearm tattoo. D. Riday 'This made me feel like we were much closer to seeing the people behind the art, how they worked and learned. The images came alive,' Dr. Caspari said. The female mummy is one of three fleshickles plucked from the permafrost on the Okok Plateau in the Altai Mountains in Russia in 1993. She was part of a Pazyryk tribe — horse-riding nomads who dominated the Eurasian plains from the 6th to 3rd centuries BC. Advertisement 5 Hand tattoos, including rooster on the thumb. D. Riday The 'Ice Maiden's' tattoos have proved to be an insight into the mysterious Pazyryk tribe who were apparently dedicated and expert tattoo artists. 'If I was guessing, it was probably four and half hours for the lower half of the right arm, and another five hours for the upper part,' Dr. Caspari said, adding, 'That's a solid commitment from the person.' 'It would need to be performed by a person who knows health and safety, who knows the risks of what happens when the skin is punctured.' Advertisement Much like contemporary tattoos, the process included a stencil of the design on the skin first with the ink being inserted under the skin with a needle-like tool, the researchers claimed. 5 The infrared imaging of the mummy's skin showed the leopard print of one of the tattoos. M Vavulin 'And back in the day it was already a really professional practice where people put a lot of time and effort and practice into creating these images and they're extremely sophisticated,' said Dr. Caspari. 'It suggests that tattoos were really something for the living with meaning during life, but that they didn't really play much of a role in the afterlife.'

Why the Russia Earthquake Didn't Cause a Huge Tsunami
Why the Russia Earthquake Didn't Cause a Huge Tsunami

Scientific American

time6 days ago

  • Scientific American

Why the Russia Earthquake Didn't Cause a Huge Tsunami

The moment seismologists got word that a magnitude 8.8 earthquake had struck near Russia's Kamchatka peninsula, they felt an acute sense of anxiety. This location—where the Pacific tectonic plate is plunging below the Eurasian plate—can produce widespread, highly destructive tsunamis. It did just that in 1952, when a magnitude 9 quake effortlessly washed away a nearby Russian town while also causing extensive damage in far-off Hawaii. Today, when the seafloor next to Kamchatka violently buckled at 11:24 a.m. Wednesday local time (7:24 EDT), everything seemed primed for a dangerous tsunami. Early forecasts by scientists (correctly) predicted that several countries around the Pacific Ocean would be inundated to some degree. Millions of people were evacuated from coastal Japan, and many in Hawaii were ordered to seek higher ground. People across swaths of Central and South America were also advised to flee from the receding ocean. And as an initial smaller tsunami formed on the northern Japanese island of Hokkaido, there was some preliminary concern that waves could reach a height of nearly 10 feet. But for the most part (at the time of writing) plenty of countries in the firing line didn't get hit by an extremely lethal wall of water. It appears that waves of just over four feet hit Japan and Hawaii—two locations that have now significantly downgraded their tsunami alerts and rescinded some evacuation notices. One tourist in Hawaii told BBC News that 'the disaster we were expecting did not come.' Parts of California have seen water up to 8 feet, but without considerable damage. On supporting science journalism If you're enjoying this article, consider supporting our award-winning journalism by subscribing. By purchasing a subscription you are helping to ensure the future of impactful stories about the discoveries and ideas shaping our world today. This raises a key question: Considering that the Kamchatka oceanic megaquake had a magnitude of 8.8— one of the most powerful ever recorded —why wasn't the resulting tsunami more devastating? The answer, in short, is this: the specific fault that ruptured produced pretty much exactly the tsunami it was capable of making, even if it intuitively felt like it should have been worse. 'First, it's important to recognize that the issuance of any warning at all is a success story,' says Diego Melgar, an earthquake and tsunami scientist at the University of Oregon. A tsunami doesn't have to be 30 feet tall to cause intense destruction and death; even a relatively modest one can wash people and structures away with ease. So far, it looks like there won't be a high number of casualties—and that's in part because 'the warnings went out, and they were effective,' Melgar says: people got out of danger. It's also fair to say that for Kamchatka and its surroundings, there actually was some localized destruction. The earthquake itself severely shook the eastern Russian city of Petropavlovsk-Kamchatsky and did scattered damage to buildings there, and tsunami waves reached heights of up to 16 feet in Severo-Kurilsk, a town in the northern Kuril Islands just south of Kamchatka. Houses and sections of a port have been wrecked or swept out to sea. The way each nation issues a tsunami warning differs slightly. But in general, if a tsunami is very likely incoming and is thought to be potentially dangerous, an evacuation order for those on the afflicted coastline is issued. When such alerts go out, some tsunami wave height estimates are often given, but these numbers are initially difficult to nail down. One reason is because, when a tsunami-making quake happens, 'the tsunami energy is not distributed symmetrically,' says Amilcar Carrera-Cevallos, an independent earthquake scientist. A tsunami does not move outward in all directions with the same momentum, because faults don't rupture in a neat linear break, nor does the seafloor movement happen smoothly and in one direction. 'Initial warnings are based only on the estimated size and location of the source, but this alone doesn't determine how much water is displaced or where waves will concentrate,' Melgar says. 'To forecast impacts accurately, scientists need to know how much the fault slipped, over what area, and how close to the trench the slip occurred.' And that information is usually gleaned one or two hours after the tsunami has appeared. A tsunami like today's is tracked by a network of deep-ocean pressure sensors, which helps scientists update their forecasts in real time. But 'the network is sparse. It doesn't always catch the full complexity of wave energy radiating across the basin,' Melgar notes. This means it gives scientists only a partial understanding of the ocean-wide tsunami. Another issue is that the tsunami's wave height when it reaches the shore is influenced by the shape and height (technically called the bathymetry) of the seafloor it's passing over. Tsunamis are also hindered, or helped, by the shape and nature of the coastline they slam into. 'Features like bays can amplify wave heights; tsunami waves can also be diffracted (bent) around islands,' says Stephen Hicks, an earthquake scientist at University College London. It may also be tempting to compare today's magnitude 8.8 quake with the 2011 magnitude 9.1 quake that struck off eastern Japan, triggering a tsunami with a maximum wave height of 130 feet—one that killed more than 18,000 people. The 2004 magnitude 9.2 earthquake and tsunami in the Indian Ocean—one that claimed the lives of over 220,000 people across a vast area—may also come to mind. That's understandable, but today's magnitude 8.8 quake was not quite powerful as one might think. The magnitude scale for earthquakes is not linear; in other words, a small increase in magnitude equals a huge jump in energy unleashed. According to the U.S. Geological Survey, a magnitude 9.1 quake (like the 2011 Japanese example) is nearly three times stronger than today's. The 2004 and 2011 cataclysms 'were actually quite a lot larger than this event,' says Judith Hubbard, an earthquake scientist at Cornell University. They were simply more capable of pushing a giant volume of water across the ocean than today's temblor. Not knowing the exact height of an incoming tsunami at multiple locations all around the Pacific, though, is a secondary concern. What matters most is that the tsunami warnings went out to those in harm's way quickly, while giving accurate times as to when the tsunamis would arrive at each coastline. 'The current strategy of preventative evacuation does a good job of saving lives,' Hubbard says.

Scientists didn't expect the 8.8 magnitude Russian megaquake for many more years. Why now?
Scientists didn't expect the 8.8 magnitude Russian megaquake for many more years. Why now?

National Geographic

time6 days ago

  • National Geographic

Scientists didn't expect the 8.8 magnitude Russian megaquake for many more years. Why now?

Here's what we know about what caused the earthquake off Russia's Far East and why the tsunami it generated weren't as big as anticipated. The aerial view of the city of Severo-Kurilsk shows flooding due to tsunami waves triggered by the 8.8 magnitude earthquake struck off the coast of Russia's Kamchatka Peninsula. The quake struck at 11:24 a.m. local time on July 30 (9:24 p.m. eastern time on July 29), and its epicenter was 20.7 kilometers (12.8 miles) deep. Photograph by Kamchatka of Geophysical Survey/Anadolu/Getty Images Just offshore from Russian's far-eastern Kamchatka peninsula, a major earthquake shook the region on Wednesday. At magnitude 8.8, it released several times more energy than the largest nuclear bomb ever detonated. 'It's a massive-scale earthquake,' says Harold Tobin, the director of the Pacific Northwest Seismic Network at the University of Washington. In fact, Earth hasn't seen a quake this big since 2011, when a magnitude 9.1 tremblor off the coast of Japan resulted in the Fukushima nuclear disaster. 'It's within the top 10 largest earthquakes ever recorded by seismometers,' says Steven Hicks, an earthquake scientist at University College London. It didn't just cause the seafloor to jolt upward. 'It broke the seafloor,' he says. And immediately, the danger was clear: The seafloor break generated a dangerous, ocean-spanning tsunami. As a result, tsunami warnings were speedily issued for many of the countries bordering the Pacific Ocean, including the entire western seaboard of North America, as well as parts of Central and South America. (Here's what to do to prepare for a tsunami.) This earthquake took place along a tectonic schism that's known for creating truly devastating temblors and tsunamis. So far, it looks like the worst-case scenarios of widespread death and devastation haven't played out. But the tsunami could still impact various shores throughout the day, and powerful aftershocks are occurring, so the danger hasn't passed just yet. What caused this megaquake? Such extreme events are called megathrust earthquakes or megaquakes because of their sheer size and where they occur. Its epicenter falls within a geologic battleground known as a subduction zone. Here, the Pacific tectonic plate collides with and sinks below the Eurasian plate in what is known as a subduction zone. 'Where these two plates collide, the megathrust fault becomes stuck and locked, storing up the accumulated plate motion for hundreds of years,' says Hicks. 'This stored energy suddenly gets released in great earthquakes.' So, it's not surprising that a major earthquake took place off the coast of Kamchatka. 'Big quakes have happened here in the past, so with this one, we knew to expect something there,' says Christine Houser, a geophysicist at the Tokyo Institute of Technology. In response to tsunami warning, the Enoden train service was suspended in Kamakura City, Kanagawa Prefecture on July 30, 2025. Photograph by The Yomiuri Shimbun/AP Images A TV news program reports the issuance of tsunami warning at city hall as shelter after the issuance of tsunami warning in Tanabe City, Wakayama Prefecture on July 30, 2025. Photograph by The Yomiuri Shimbun/AP Images According to the U.S. Geological Survey (USGS), this was also a reverse faulting event. This involves a large block of the crust above the active fault suddenly moving up over another block of the crust below the fault. In this case, a fault line ruptured over a length of a few hundred miles in a matter of seconds, releasing as much energy as roughly 240 million tons of TNT. 'It's a big earthquake. There's no doubt about that,' says Tobin. The nearest large city was Petropavlovsk-Kamchatsky, on Kamchatka, home to over 180,000 people. At least a quarter of a million people in the region felt severe, damaging shaking, USGS estimates. There have been at least two-dozen aftershocks from this mainshock, including a magnitude 6.9 event; aftershocks like this are expected to continue for several days, at least. A possible prelude to the main event Although the megaquake's location isn't too strange, there is something unusual about its timing. Back in 1952, very close to today's colossal temblor, a highly destructive magnitude 9.0 quake struck the region—one that also generated a powerful tsunami. A gap of several decades between this megaquake and today's event may seem like a long time. But not for megaquakes. In general, for these major events, 'stress builds up, then you have a big earthquake to relieve that stress,' says Houser. And then there's a gap of perhaps several centuries. That clearly didn't happen. 'Would I have predicted another nearly-magnitude 9.0 event within only several decades? Probably not,' says Tobin. The short period between these two megathrust quakes suggests that these ginormous subduction zones can build up an explosive degree of stress over a relatively short period. And, for the time being, scientists aren't certain how this happened. 'It shows our ignorance,' says Houser. It's worth underscoring, though, that the largest of quakes don't operate according to neatly timed schedules. 'It's not a clockwork,' says Tobin. Understanding why is one of the most crucial open questions in the geosciences—an unsolved puzzle that means that, for now, nobody can predict exactly when the next major quake will take place. The first waves of the tsunami have arrived Japan's Pacific coast after the magnitude 8.7 strong earthquake strikes off Kamchatka Peninsula on July 30, 2025 in Shiogama, Miyagi, Japan. Photograph by TheCars are at a standstill along the Pan-American Highway in Panama City, Wednesday, July 30, 2025, following a tsunami warning after a earthquake struck off the coast of Russia early Wednesday. Photograph by Matias Delacroix, AP On a related note: just over a week prior, a magnitude 7.4 earthquake (which also briefly threatened to generate a tsunami) exploded along the very same subduction zone. Earthquake scientists are now speculating as to whether that significant temblor was some sort of precursor, or at least a possible warning, of today's catastrophic event. For now, 'we have no way of telling that a magnitude 7.0 will be followed at some point by a larger quake,' says Lucile Bruhat, an earthquake scientist working in the insurance industry. But there is a chance that the magnitude 7.4 quake from earlier this month 'could have triggered today's earthquake. But it will be after analyzing the slip and rupture pattern that we'll be able to confirm that assumption.' In some ways, today's magnitude 8.8 event 'is a near-repeat of the magnitude 9.0,' says Tobin. But earthquakes of similar magnitudes can release vastly different amounts of energy, and despite its only slightly higher rating, the 1952 quake was twice as energetic as today's, which goes some way to explaining why the previous event was more destructive and decidedly lethal. As frightening as that quake itself would have been, much of the concern immediately focused on the tsunami it undoubtedly unleashed. 'These shallow subduction megathrust events cause large tsunamis because the portion of fault that moves during the earthquake reaches close to, if not directly penetrates, the seafloor, displacing vast volumes of water in the sea above,' says Hicks. (Here's why no one was prepared for the deadliest tsunami in history.) Calculating the possible wave heights of tsunamis can be tricky, as the shape and depth profile of the shoreline can really affect its development from location to location. 'The wave energy is guided by the depth of the water in any given location,' says Tobin. Either way, based on the nature of the quake itself, the threat was obvious. 'Issuing a tsunami warning was absolutely right thing to do.' Nations across the Pacific were immediately placed on alert. So far, the worst-hit region is that of southeastern Kamchatka, where tsunami waves reaching a heigh of over 16 feet have been observed. Structures have been seen being washed away in some locations, although no deaths have currently been reported. 'It's a very sparsely populated region too, so there wasn't a lot in harm's way, fortunately,' says Tobin. Meanwhile, a vast volume of water was pushed out into the wider ocean, triggering evacuation notices in Japan, several Pacific islands, and, eventually, across Hawaii. In Japan, initial smaller tsunami wave had heights of around one foot. But later, waves as high as 4.3 feet were recorded, with the possibility of waves double that height possible for some shorelines. Hawaii has also seen waves several feet high. Aftershocks—including those capable of generating smaller tsunamis—will continue for some time. But even if the damage from the mainshock's tsunami is still being assessed, it seems much of the Pacific has dodged a decidedly grim fate. 'It's kind of looking like the amplitude of the tsunami is less than at least the worst-case scenarios,' says Tobin.

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