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How changes in California culture have influenced the evolution of wild animals in Los Angeles

How changes in California culture have influenced the evolution of wild animals in Los Angeles

For decades, biologists have studied how cities affect wildlife by altering food supplies, fragmenting habitats and polluting the environment. But a new global study argues that these physical factors are only part of the story. Societal factors, the researchers claim, especially those tied to religion, politics and war, also leave lasting marks on the evolutionary paths of the animals and plants that share our cities.
Published in Nature Cities, the comprehensive review synthesizes evidence from cities worldwide, revealing how human conflict and cultural practices affect wildlife genetics, behavior and survival in urban environments.
The paper challenges the tendency to treat the social world as separate from ecological processes. Instead, the study argues, we should consider the ways the aftershocks of religious traditions, political systems and armed conflicts can influence the genetic structure of urban wildlife populations.
'Social sciences have been very far removed from life sciences for a very long time, and they haven't been integrated,' said Elizabeth Carlen, a biologist at Washington University in St. Louis and co-lead author of the study. 'We started just kind of playing around with what social and cultural processes haven't been talked about,' eventually focusing on religion, politics and war because of their persistent yet underexamined impacts on evolutionary biology, particularly in cities, where cultural values and built environments are densely concentrated.
Carlen's own work in St. Louis examines how racial segregation and urban design, often influenced by policing strategies, affect ecological conditions and wild animals' access to green spaces.
'Crime prevention through environmental design,' she said, is one example of how these factors influence urban wildlife. 'Law enforcement can request that there not be bushes … or short trees, because then they don't have a sight line across the park.' Although that design choice may serve surveillance goals, it also limits the ability of small animals to navigate those spaces.
These patterns, she emphasized, aren't unique to St. Louis. 'I'm positive that it's happening in Los Angeles. Parks in Beverly Hills are going to look very different than parks in Compton. And part of that is based on what policing looks like in those different places.' This may very well be the case, as there is a significantly lower level of urban tree species richness in areas like Compton than in areas like Beverly Hills, according to UCLA's Biodiversity Atlas.
The study also examines war and its disruptions, which can have unpredictable effects on animal populations. Human evacuation from war zones can open urban habitats to wildlife, while the destruction of green spaces or contamination of soil and water can fragment ecosystems and reduce genetic diversity.
In Kharkiv, Ukraine, for example, human displacement during the Russian invasion led to the return of wild boars and deer to urban parks, according to the study. In contrast, sparrows, which depend on human food waste, nearly vanished from high-rise areas.
All of this, the researchers argue, underscores the need to rethink how cities are designed and managed by recognizing how religion, politics and war shape not just human communities but also the evolutionary trajectories of urban wildlife. By integrating ecological and social considerations into urban development, planners and scientists can help create cities that are more livable for people while also supporting the long-term genetic diversity and adaptability of the other species that inhabit them.
This intersection of culture and biology may be playing out in cities across the globe, including Los Angeles.
A study released earlier this year tracking coyotes across L.A. County found that the animals were more likely to avoid wealthier neighborhoods, not because of a lack of access or food scarcity, but possibly due to more aggressive human behavior toward them and higher rates of 'removal' — including trapping and releasing elsewhere, and in some rare cases, killing them.
In lower-income areas, where trapping is less common, coyotes tended to roam more freely, even though these neighborhoods often had more pollution and fewer resources that would typically support wild canines. Researchers say these patterns reflect how broader urban inequities are written directly into the movements of and risks faced by wildlife in the city.
Black bears, parrots and even peacocks tell a similar story in Los Angeles. Wilson Sherman, a PhD student at UCLA who is studying human-black bear interactions, highlights how local politics and fragmented municipal governance shape not only how animals are managed but also where they appear.
'Sierra Madre has an ordinance requiring everyone to have bear-resistant trash cans,' Sherman noted. 'Neighboring Arcadia doesn't.' This kind of patchwork governance, Sherman said, can influence where wild animals ultimately spend their time, creating a mosaic of risk and opportunity for species whose ranges extend across multiple jurisdictions.
Cultural values also play a role. Thriving populations of non-native birds, such as Amazon parrots and peacocks, illustrate how aesthetic preferences and everyday choices can significantly influence the city's ecological makeup in lasting ways.
Sherman also pointed to subtler, often overlooked influences, such as policing and surveillance infrastructure. Ideally, the California Department of Fish and Wildlife would be the first agency to respond in a 'wildlife situation,' as Sherman put it. But, he said, what often ends up happening is that people default to calling the police, especially when the circumstances involve animals that some urban-dwelling humans may find threatening, like bears.
Police departments typically do not possess the same expertise and ability as CDFW to manage and then relocate bears. If a bear poses a threat to human life, police policy is to kill the bear. However, protocols for responding to wildlife conflicts that are not life-threatening can vary from one community to another. And how police use non-lethal methods of deterrence — such as rubber bullets and loud noises — can shape bear behavior.
Meanwhile, the growing prevalence of security cameras and motion-triggered alerts has provided residents with new forms of visibility into urban biodiversity. 'That might mean that people are suddenly aware that a coyote is using their yard,' Sherman said. In turn, that could trigger a homeowner to purposefully rework the landscape of their property so as to discourage coyotes from using it. Surveillance systems, he said, are quietly reshaping both public perception and policy around who belongs in the city, and who doesn't.
Korinna Domingo, founder and director of the Cougar Conservancy, emphasized how cougar behavior in Los Angeles is similarly shaped by decades of urban development, fragmented landscapes and the social and political choices that structure them. 'Policies like freeway construction, zoning and even how communities have been historically policed or funded can affect where and how cougars move throughout L.A.,' she said. For example, these forces have prompted cougars to adapt by becoming more nocturnal, using culverts or taking riskier crossings across fragmented landscapes.
Urban planning and evolutionary consequences are deeply intertwined, Domingo says. For example, mountain lion populations in the Santa Monica and Santa Ana mountains have shown signs of reduced genetic diversity due to inbreeding, an issue created not by natural processes, but by political and planning decisions — such as freeway construction and zoning decisions— that restricted their movement decades ago.
Today, the Wallis Annenberg Wildlife Crossing, is an attempt to rectify that. The massive infrastructure project is happening only, Domingo said, 'because of community, scientific and political will all being aligned.'
However, infrastructure alone isn't enough. 'You can have habitat connectivity all you want,' she said, but you also have to think about social tolerance. Urban planning that allows for animal movement also increases the likelihood of contact with people, pets and livestock — which means humans need to learn how to interact with wild animals in a healthier way.
In L.A., coexistence strategies can look very different depending on the resources, ordinances and attitudes of each community. Although wealthier residents may have the means to build predator-proof enclosures, others lack the financial or institutional support to do the same. And some with the means simply choose not to, instead demanding lethal removal., 'Wildlife management is not just about biology,' Domingo said. 'It's about values, power, and really, who's at the table.'
Wildlife management in the United States has long been informed by dominant cultural and religious worldviews, particularly those grounded in notions of human exceptionalism and control over nature. Carlen, Sherman and Domingo all brought up how these values shaped early policies that framed predators as threats to be removed rather than species to be understood or respected. In California, this worldview contributed not only to the widespread killing of wolves, bears and cougars but also to the displacement of American Indian communities whose land-based practices and beliefs conflicted with these approaches.
Wildlife management in California, specifically, has long been shaped by these same forces of violence, originating in bounty campaigns not just against predators like cougars and wolves but also against American Indian peoples. These intertwined legacies of removal, extermination and land seizure continue to influence how certain animals and communities are perceived and treated today.
For Alan Salazar, a tribal elder with the Fernandeño Tataviam Band of Mission Indians, those legacies run deep. 'What happened to native peoples happened to our large predators in California,' he said. 'Happened to our plant relatives.' Reflecting on the genocide of Indigenous Californians and the coordinated extermination of grizzly bears, wolves and mountain lions, Salazar sees a clear parallel.
'There were three parts to our world — the humans, the animals and the plants,' he explained. 'We were all connected. We respected all of them.' Salazar explains that his people's relationship with the land, animals and plants is itself a form of religion, one grounded in ceremony, reciprocity and deep respect. Salazar said his ancestors lived in harmony with mountain lions for over 10,000 years, not by eliminating them but by learning from them. Other predators — cougars, bears, coyotes and wolves — were also considered teachers, honored through ceremony and studied for their power and intelligence. 'Maybe we had a better plan on how to live with mountain lions, wolves and bears,' he said. 'Maybe you should look at tribal knowledge.'
He views the Wallis Annenberg Wildlife Crossing — for which he is a Native American consultant — as a cultural opportunity. 'It's not just for mountain lions,' he said. 'It's for all animals. And that's why I wanted to be involved.' He believes the project has already helped raise awareness and shift perceptions about coexistence and planning, and hopes that it will help native plants, animals and peoples.
As L.A. continues to grapple with the future of wildlife in its neighborhoods, canyons and corridors, Salazar and others argue that it is an opportunity to rethink the cultural frameworks, governance systems and historical injustices that have long shaped human-animal relations in the city. Whether through policy reform, neighborhood education or sacred ceremony, residents need reminders that evolutionary futures are being shaped not only in forests and preserves but right here, across freeways, backyards and local council meetings.
The research makes clear that wildlife is not simply adapting to urban environments in isolation; it is adapting to a range of factors, including policing, architecture and neighborhood design. Carlen believes this opens a crucial frontier for interdisciplinary research, especially in cities like Los Angeles, where uneven geographies, biodiversity and political decisions intersect daily. 'I think there's a lot of injustice in cities that are happening to both humans and wildlife,' she said. 'And I think the potential is out there for justice to be brought to both of those things.'
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Why the Russia Earthquake Didn't Cause a Huge Tsunami
Why the Russia Earthquake Didn't Cause a Huge Tsunami

Scientific American

time3 hours 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.

Massive earthquake off Russia's east coast is one of the most powerful ever recorded
Massive earthquake off Russia's east coast is one of the most powerful ever recorded

NBC News

time3 hours ago

  • NBC News

Massive earthquake off Russia's east coast is one of the most powerful ever recorded

The earthquake that struck Russia's eastern Kamchatka region and triggered tsunami warnings across the Pacific is among the most powerful temblors to have been recorded in modern history. The U.S. Geological Survey (USGS) may revise the magnitude of the earthquake, but if it remains at 8.8, this quake would be tied with the sixth strongest ever, which struck central Chile in 2010, killing more than 500 people and destroying over 370,000 homes. Russian authorities have called the latest quake a 'remarkable event.' It struck at a depth of an estimated 13 miles, about 74 miles off the coast of Petropavlovsk-Kamchatsky, the regional capital on the Kamchatka Peninsula, with a population of 180,000. Despite its strength, early reports indicate that there have been no deaths or significant damage from the event and that recorded tsunami waves reached a maximum of 9.8 to 13.1 feet in Russia, 4.9 feet in Japan and 5.7 feet in Hawaii. David Tappin, principal researcher at the British Geological Survey, said he's surprised by this. 'When I first saw it was 8.8, I must admit, I thought, 'Oh, we're going back to maybe Japan,'' he said, referring to the 2011 earthquake that triggered a huge tsunami, killing more than 20,000 people and causing a meltdown at the Fukushima Daiichi nuclear power plant. Now referred to as the 'Great Tohoku Earthquake,' it had a magnitude of 9.1, the fourth most powerful ever recorded. The waves from that tsunami reached as high as 130 feet, according to the National Oceanic and Atmospheric Administration, hitting the coast at a height of about 50 feet. 'At the present time, it seems quite anomalous. 8.8 magnitude generating a 4-meter tsunami seems very unusual but … the information on the tsunami impact is still quite limited,' Tappin said, adding that he would have expected a tsunami of at least 10 meters, or about 33 feet. He said the relatively insignificant damage reported so far could be due to the remoteness of the epicenter and the effectiveness of the warning systems. 'It seems to me that the warning system kicked in, and warnings were given in Japan initially, Hawaii and off the West Coast of the U.S. So it just demonstrates the importance of having these warning systems,' Tappin said. 'In this instance, perhaps the tsunami wasn't large, but it saves people's lives.' The fifth-strongest earthquake ever recorded, a 9.0 tremor, also hit the Kamchatka region in 1952. Its epicenter was less than 19 miles from this one. In that disaster, the waves reached up to 50 feet and killed at least 1,790 people, with some historians putting the death toll as high as 8,000, according to the Russian Military Historical Society. The region has experienced nearly 700 earthquakes with magnitudes over 5.0 since 1990, according to the USGS. The most powerful earthquake ever recorded was the magnitude-9.5 'Valdivia' or 'Great Chilean' earthquake, which hit central Chile in 1960, killing more than 1,600 people and leaving 2 million homeless. One of the world's most deadly earthquakes was the third most powerful ever recorded, which struck off the coast of Sumatra, Indonesia, on Boxing Day in 2004. The 9.1-magnitude quake triggered massive tsunamis reaching up to 100 feet and killed an estimated 280,000 people.

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

time4 hours 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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