SHOCKING! Tibet’s 7.0 Quake Splits Ground, Topples Hundreds of Homes—Bigger Man-Made Disaster Ahead

A magnitude 7 earthquake struck Baqian County in Nachu, Tibet at 10.33pm on October 22nd. The epicenter was in Maru Township, about 43 miles from the county seat. Security footage shows supermarket shelves shaking as bottles, plates and other goods fall to the floor. Customers checking out and store employees immediately run outside. In another security video from a restaurant, the camera shakes as workers rush out the door. Videos from local residents soon began showing conditions near the epicenter. One showed visible cracks in the ground, some more than four inches wide. Other reports said people had been injured in pastoral areas. There's been an earthquake here in Nachu. The shaking was really strong. Look at the ground. The quake split it open. That's a pretty big crack. I'm in Maru Township, and we could really feel it here. The earthquake also triggered rockfalls that disrupted traffic. A driver filming at night showed large rocks on the road, forcing vehicles to make dangerous detours around them. Holy crap, that rock is huge. Take a look. Left or right? All right, go, go. This is too dangerous. Speed up. We have to speed up. There are more rocks ahead. Strong shaking also hit high-rise apartments in the Bachen County seat, farther from the epicenter. One resident on the 18th floor said the shaking was so strong they could barely walk. The lights kept swinging, and it was terrifying. One user wrote in the comment, the epicenter is sparsely populated, but there are still several villages and a town within three miles. The China Earthquake Network Center measured the quake at magnitude 7, with an epicenter at 32.4 degrees north, 92.79 degrees east, at a depth of just six miles. The U.S. Geological Survey also measured it at 7.0, at a depth of about 11 miles. A powerful shallow quake can cause far more damage near the epicenter than the number 7 on a map conveys. Shaking was felt across Nachu, as well as Changdu, Ningqi, and Lhasa. Parts of Yushu near Qinghai were also felt strong shaking. Neighboring Biru County, south of Bachen, is more than 60 miles from the epicenter. One local resident said, The shaking drove everyone outside. It lasted so long that a lot of people were terrified. Some came out wrapped in blankets. People with homes in the countryside were heading there. We won't be sleeping well tonight. The shaking reached as far as Zaduo County, Qinghai. A local livestreamer said viewers from Qinghai and Tibet kept posting messages, saying they felt it. Word spread almost as quickly as the seismic waves. The earthquake in Nachu also affected us here in Zaduo County, Qinghai. I started my live stream at 10.30, and right away someone said there had been an earthquake. I quickly checked online and found that a magnitude 7.0 quake had hit Nachu. Then viewers from Zaduo joined and said they felt it too. You see, live streaming gives me access to a lot of information, because many of my followers are from Qinghai and Tibet. Local viewers here in Qinghai said Zaduo felt a shaking. I checked, and it was magnitude 4.6 in Zaduo. I wanted to update everyone right away. No casualty figures have been released yet. Now, someone from Bachen County has joined too. Look, this viewer is from Bachen County and says the shaking was especially strong. Street security footage shows a man running out of a shop. After just a few steps, he loses his balance, falls, and tumbles forward. Bricks and roof tiles fall from nearby buildings as the shaking continues. He later films his hands, showing several swollen, scraped areas. After the earthquake, more residents stayed outside, afraid to return home right away. A survivor, Yexie Zomou, told the Tibet Daily, We had only gone to bed when the house suddenly started shaking. Everything inside fell down. That's when we realized it was an earthquake. We ran downstairs before we even had time to get dressed. My legs kept trembling as I went down. By the time I could collect myself, I was already crying from fear. A lot of people in town came outside tonight. Everyone is afraid to go back inside, so they're pitching tents along the road or spending the night in their cars. By early October 23rd, officials reported at least 16 deaths and 46 injuries, including 11 serious injuries and 35 minor ones. Homes belonging to 339 households had collapsed or been damaged, along with 20 livestock shelters. Multiple aftershocks, ranging from magnitude 3 to 5 followed. Parts of the Qinghai-Tibet Railway were temporarily closed for inspections, and rockfalls hit national highways. The area near the epicenter averages nearly 15,700 feet above the sea level. Northern Tibet is already cold by late October, with snow possible in the coming days. Earlier that same day, at 9.07 a.m., a magnitude 3 quake hit Nagchu's Shuanghu County. A magnitude 4.7 earthquake struck Nima County on August 27, followed by a magnitude-4 earthquake in Zaina County on September 19. Data from the Tibet Earthquake Agency show repeated quakes of magnitude-3 to 4 or higher this year in Ngari, Ningshi, Shigatse, Nagchu, and other areas. A magnitude-3 quake also struck Lhasa County, Shigatse on October 17. These cannot simply be treated as warning signs of the Magnitude 7 quake. They do show that the Tibetan Plateau remains tectonically active. The Indian Plate continues to push north into Eurasia each year. Over tens of millions of years, that collision thickened and lifted the crust, creating the Himalayas and the Tibetan Plateau, which averages more than 13,100 feet above sea level. The plateau is not one solid slab of rock. Continued compression from north to south shortens the crust while stretching it east to west. That has left the plateau crisscrossed with strike slip, normal, and thrust faults. The U.S. Geological Survey describes the Tibetan plateau as roughly 620 miles from north to south and 1,550 miles from east to west. Major faults including the Kunlun, Haiyuan, and Altyn Tagh cut across it, along with many normal faults running north to south. The collision between India and Eurasia continues, and stress keeps building in the crust. Preliminary analysis of the magnitude 7 Ba Chen earthquake also points mainly to normal faulting, consistent with east-west stretching inside the Tibetan Plateau. The force did not suddenly appear that day. It was more like a rope stretched tight for a long time than snapping once it reached its breaking point. Today, the Tibetan Plateau faces more than the natural tectonic forces that have shaped it for tens of millions of years. As stress builds and releases underground, changes at the surface are becoming more pronounced. Retreating glaciers, thawing permafrost, and more high mountain landslides are making already fragile slopes even less stable. Natural changes and construction are increasingly overlapping in the same high-risk areas. A study published in National Science Review this April examined 8,607 climate-related landslides in the eastern Himalayan Syntaxis, a region where the mountain range bends sharply. The study covers the time period from 1987 to 2022. Above 9,800 feet, the total volume of material displaced by landslides each year increased roughly sixfold over more than 30 years. As glaciers retreat and permafrost thaws, landslide activity is also moving to higher elevations. That means some slopes, once held in place by ice, snow, and frozen ground are gradually losing that support. Another study of glaciers in southeastern Tibet found that about 365 square miles of glaciers face a potential collapse risk. It identified eight river basins at extremely high risk, affecting 85 settlements, 131 roads, and 52 rivers. Researchers said warming, precipitation, earthquakes, and steep terrain are combining to drive those risks. In other words, Tibet faces more than earthquake risk alone. Earthquakes, melting glaciers, degrading permafrost, landslides, ice and rock avalanches, debris flows, and blocked rivers can compound one another in the same area. Meanwhile, large mining, hydropower, road, tunnel, and power transmission projects continue expanding into these mountain valleys. A massive ice and rock avalanche and flooding struck the Gyirong area along the China-Nepal border on August 26 this year. Huge amounts of ice, rock, and sediment suddenly poured into the valley, sending floodwaters into Nepal. By early September, Reuters reported that the death toll in Nepal had exceeded 1,000. Many hydropower plants and infrastructure facilities were destroyed. Hundreds of hydropower workers were temporarily missing or trapped in tunnels. Later, U.S. geological survey data showed that shaking initially mistaken by some for an earthquake had actually come from the massive collapse of ice and rock. The disaster was caused by unstable glaciers and mountain slopes. Afterward, Tibetan groups abroad and some activists raised another question. They asked whether expanding mining, roads, hydropower, and construction had further disturbed already fragile slopes, on top of climate and natural geological conditions. After the flood, the Tibetan Truth website pointed to prospects for mining lithium, beryllium, niobium, tantalum, and other rare metals around Gyirong. It questioned whether drilling, blasting, road excavation, and waste rock piles could increase slope instability. Chinese researchers published a case study this year on a construction project along the northeastern edge of the Tibetan Plateau. They found that an initially small, localized landslide kept expanding during road and tunnel construction. Excavation at the front of the slope changed the balance of forces. Tunneling and other construction disturbances further affected groundwater and stress in the soil. A deep landslide eventually developed, collapsing the tunnel and halting work. The authors explicitly said construction can trigger or amplify landslides in the plateau's fragile geological environment. Excavation, blasting, cutting slopes, drilling tunnels, and changing drainage can all become links in that chain of risk. Tibet is also undergoing rapid expansion of major construction projects. Works on the hydropower project on the lower Yarlung Tsangpo River officially began in July 2025. The Chinese Communist Party plans to build five hydropower stations in a series along the river. Their projected annual output is about 300 billion kilowatt hours, several times that of the Three Gorges Project. Officials have called it a project of the century. By July this year, Chinese geologists have publicly raised concerns. Researchers confirmed that the highly active Paizhen Fault lies near this project. It has remained active since the Pleistocene and could directly affect the stability of nearby dams, roads, bridges, tunnels, and reservoir areas. They called for stronger slope protection to prevent landslides and collapses. Officials keep emphasizing descriptions such as the world's largest mega project and clean energy, along with a huge investment. Meanwhile, Chinese geologists are discussing active faults, landslides, collapses, and reservoir stability. The 2025 Tengri earthquake damaged four reservoirs. A Reuters investigation at the time found 68 large dams already operating in the Himalayan region, with another 101 planned or under construction. Several geological experts said adding large reservoirs in a major earthquake zone requires stricter seismic risk assessments. Storing vast amounts of water adds weight to the ground. Water can also seep into cracks in the rock, changing pressure within those cracks and pores. If a nearby fault is already close to rupture, how much this added disturbance could affect it remains a subject of geophysical research. Earthquakes near some large Chinese reservoirs have sparked similar debates. For Tibet, though, the broader issue may go far beyond whether one particular earthquake can be directly blamed on one particular reservoir. Climate change is rapidly increasing the volume of high-altitude landslides in Tibet. Glaciers and permafrost are becoming less stable. Earthquakes continue. And geologists keep identifying active faults and risk of glacier collapses and massive landslides. Yet hydropower, mining, tunnel, and road projects continue expanding into these areas on a huge scale. These projects often cross Tibetan grazing lands, villages, and monasteries. The Gangtua hydropower project triggered large protests in Derge, a Tibetan area of Sichuan in 2024. Local Tibetans and monks feared the project would flood or force the relocation of six monasteries and two villages, and protested the project. Radio Free Asia initially reported more than 100 arrests. Later reports put the number detained at more than 1,000. Some people who were released remained under strict surveillance and communication restrictions. Similar disputes arose over mining projects in 2025. The International Campaign for Tibet reported that Tibetans in Sichu County, Sichuan, protested after discovering gold mining on traditional grazing land. Tibetan organizations abroad said about 80 people were then detained and communications were blocked. That points to a key difference in how environmental risks are handled in Tibet. Under normal public oversight, a major hydropower, mining, or tunnel project entering a geologically hazardous area should face environmental impact assessments, scrutiny from independent experts, media investigations, and input from local residents. In Tibet, someone who believes a mine is damaging grazing land, or a hydropower station will flood a village, may face police before ever getting a public hearing. After the Gyirong flood, writer Shang Xue, who lives abroad, called for more than explanations such as ice avalanche or natural disaster. She urged further investigation into how years of road, hydropower, tunnel, and mining construction had changed local slopes. Officials can quickly announce investment totals, power output, and construction scale. Equally detailed independent geological risk assessments are rarely made available to the public. The public sees figures such as 1.2 trillion yuan, five hydropower stations, and 300 billion kilowatt hours. It's much harder to find out how many villages a major landslide, earthquake, or blocked river could affect in a worst-case scenario, how residents would evacuate, or whether they could refuse relocation. Since the Gyirong flood this August, another, broader change has come into focus. Researchers from Beijing Normal University and other institutions published a study in Nature Communications this August. They concluded that the Tibetan Plateau's moisture and climate systems are becoming less stable. The lead researcher later said publicly that rising soil moisture and faster glacier melt would bring more disasters of this kind. The entire region known as Asia's water tower is changing. Glaciers and rivers on the Tibetan Plateau affect more than 10 Asian countries and supply water to hundreds of millions of people. The Yarlung Tsangpo becomes the Brahmaputra River after leaving Tibet. As China develops its massive hydropower project, India has publicly voiced concerns about water flows, ecosystems, and security risks. Beijing says the project will not harm downstream countries and stresses that it has undergone scientific review. The CCP's recent construction push in Tibet goes far beyond hydropower. It also includes railways, roads, airports, and a broader network of border and national defense infrastructure. During the 14th Five-Year Plan alone, Tibet's road network reached about 77,800 miles. Thousands of miles of major routes into and out of Tibet were upgraded. Work continues on the Sichuan-Tibet Railway, and construction has begun on the Bomi-Ranwu Railway. National highways are being upgraded, while the network of airports and general aviation airfields keeps expanding. These projects serve purposes beyond tourism and everyday needs. Tibet's official 2026 plan explicitly calls for stronger border defense mobilization, strategic supply storage and logistics, and military supply stations. It also calls for further connecting the border highways G219 and G685, while expanding communications, power grids, Beidou navigation, and logistics facilities along the border. The plateau's expanding roads, railways, than airports carry troops and supplies in normal times. In special circumstances, however, they could rapidly move troops, transport equipment, supply border areas, and support strategic logistics. Once projects are completed in Tibet, slopes will still shift, permafrost will still thaw, and landslides and rockfalls will repeatedly cut off roads. For the CCP, major projects are primarily part of national strategy. Whether local residents are willing to accept relocation, environmental damage, and long-term geological risks often gets little weight in those decisions. The CCP can use administrative orders to push through one project of the century after another. It cannot keep an increasingly developed and disturbed plateau permanently stable. The danger extends beyond earthquakes to a totalitarian system that places political power above people's lives and local risks.