Earthquake in Nepal Right Now: What to Do, How to Check It, and Aftershock Safety Guide

You are sitting at home when the glass on the table starts to rattle. For a second you wonder whether it was a truck outside. Then the floor moves, just slightly, and does not stop right away.

Your first question in that moment is almost never "what magnitude was that." It is simpler than that: was that actually an earthquake? And once the shaking stops, a second question follows immediately: is another one coming?

This guide is built to answer both questions in order, without the panic and rumors that usually follow a real earthquake in Nepal. It starts with what to do while the ground is still moving, then how to safely confirm what happened, then what aftershocks mean, then what Nepal's own earthquake history and preparedness experience can teach you before the next one.

If an Earthquake Happens Right Now

Before anything else, here is the short version. The rest of this guide expands on every line below, but if you have thirty seconds and shaking has just started, this is everything that matters most.

What to Do During an Earthquake

The drop, cover and hold on sequence above is the single most important thing to remember, but exactly how you apply it depends on where you are when the shaking starts.

If You Are Inside

Stay inside while the building is shaking. Get under a sturdy table or desk and hold onto it, or crouch against an interior wall and cover your head and neck with your arms if no table is available. Stay away from windows, glass, tall furniture, shelves, heavy objects and anything hanging that could fall. Do not run down stairs while the building is still shaking; most people who are injured indoors during an earthquake are hurt while trying to move, not while staying still.

If You Are Outside

Move to an open area away from buildings, walls, power lines, poles and trees. Once you are in the open, drop to the ground and stay there until the shaking stops. Buildings and their facades are one of the most common sources of outdoor injury during an earthquake, so the safest place outside is simply as far from anything tall as you can get in the time available.

If You Are Driving

Slow down and pull over somewhere away from bridges, overpasses, power lines, large structures and slopes that could drop rocks onto the road. Stay inside the vehicle with your seatbelt on until the shaking stops. A car is actually a reasonably protective space during shaking; the greater danger is usually what is above or beside the road, not the vehicle itself.

If You Are in the Mountains

This matters more in Nepal than almost anywhere else. Be alert for rockfalls, landslides, falling trees and slopes that were already unstable before the earthquake, especially on steep trails and in narrow valleys. Move away from cliff edges and loose scree if you can do so safely once the shaking has stopped, and be aware that saturated or already-cracked slopes can continue to fail for hours or days after the shaking itself has ended.

What NOT to Do During an Earthquake

Some of the most dangerous mistakes during an earthquake come from instinct rather than panic. Knowing what not to do is often more useful than another list of things to do.

This guidance follows the general Drop, Cover and Hold On standard used by earthquake safety authorities including USGS, adapted with Nepal-specific detail for mountain and rural conditions. It is general safety information, not a substitute for official instructions during an active emergency.

How to Check Whether an Earthquake Just Happened in Nepal

Once you are safe, the next useful step is confirming what actually happened rather than guessing from feel alone. Here is the process, and what each term on a live earthquake feed actually means.

Magnitude, Depth, Epicenter, Distance and Intensity: What Each One Actually Means

Magnitude measures the total energy released at the earthquake's source, as a single number. Depth describes how far below the surface the rupture began; Nepal's earthquakes are typically shallow, in the range of 5 to 20 kilometres, which is part of why they tend to feel strong close to the epicenter. Epicenter is the point on the surface directly above where the earthquake originated underground. Distance is simply how far a given place is from that epicenter. Intensity is different from all of these: it describes what people and buildings actually experience at a specific location, and it depends on magnitude, depth, distance and local ground conditions together, not on magnitude alone.

Magnitude and intensity are not the same thing. A single earthquake has one magnitude, but many different intensities depending on where you are standing when it happens.

Why You Can Feel an Earthquake Whose Epicenter Is Nowhere Near You

Whether you feel an earthquake, and how strong it feels, depends on magnitude, depth, distance, local geology, the type of building you are in and even where you happen to be standing inside it. This is why "I felt it in Kathmandu" does not automatically mean the epicenter was in Kathmandu. Nepal's own experience illustrates this clearly: the September 2011 magnitude 6.9 earthquake centred near the Nepal-Sikkim border was felt strongly in Kathmandu, more than a hundred kilometres away, causing a small number of deaths from a collapsed wall in the city even though the epicenter itself was nowhere near the valley. Understanding this distinction helps you read live earthquake data correctly instead of assuming every nearby report explains what you personally felt.

How to Read the Nepal Earthquake Live Tracker

If you came to this page because you just felt your house shake, the fastest next step is to check the live earthquake data rather than guessing from feel alone. The Merokalam tracker shows a stats strip at the top with the total number of recorded events over the last 30 days, the largest magnitude, the count of significant M5.5+ events, moderate M4+ events, shallow events under 35 kilometres, and the time of the most recent event in Nepal time. Below that, filter tabs let you narrow the feed to all events, M4+ only, M5+ only, or significant M5.5+ only, which is most useful right after a notable earthquake when you want to track the mainshock and its larger aftershocks specifically. Each individual event card below the filters shows a colour-coded magnitude badge, the location with Nepal district context where relevant, the depth in kilometres, and the time. If a location is listed under a border town in India, that is simply the nearest place name in the global database used to identify the event, not a sign that the earthquake happened outside Nepal; the tracker explains the actual Nepal-region relevance next to any such entry.

Nepal's Earthquake History: A Timeline of Major Earthquakes

Reading a live feed is easier once you understand the pattern behind it. Nepal has not been shaking randomly for the last seven centuries; it has been slowly, unevenly releasing the strain built up by one of the most active mountain-building collisions on the planet. Walking through that history in order is the fastest way to understand why the live tracker looks the way it does.

Historical estimates for pre-instrumental events, especially 1255 and 1833, vary depending on the source and the method used to reconstruct them, since no seismograph existed to record them directly. Where sources disagree, this article says so rather than presenting a single number as precise. Nepal's chronicles also describe several other medieval-era earthquakes whose magnitudes are too uncertain to compare meaningfully against modern instrumental readings, so this timeline is a selection built to tell a coherent story rather than a complete catalogue.

1255: The Earliest Well-Documented Catastrophe

The earliest earthquake in Nepal's written record that historians treat as reliably documented struck the Kathmandu Valley in 1255. Chronicles describe it as catastrophic enough to kill a significant share of the valley's population, and among the dead was the reigning king, Abhaya Malla, making it one of the few earthquakes anywhere in South Asia to have directly ended a monarch's reign. Modern estimates place its size somewhere in the large-magnitude range, but because it predates any instrumental recording by roughly seven centuries, treat any specific magnitude figure for 1255 as an informed estimate rather than a measurement.

1833: A Major Himalayan Earthquake Nepal Had Nearly Forgotten

Nearly six centuries later, in August 1833, another major earthquake struck the Kathmandu Valley and the wider Himalayan region. Contemporary accounts describe extensive damage to temples and traditional brick buildings, though, as with 1255, published casualty and magnitude figures vary between sources, and modern seismologists have revisited the event's likely rupture zone using the kind of historical and geological evidence available for pre-instrumental earthquakes. What matters for a reader today is less the exact number and more the pattern: this was Nepal's second confirmed catastrophic Kathmandu Valley earthquake in under six hundred years, evidence that the valley's vulnerability is not a modern discovery.

1934: The Nepal-Bihar Earthquake

The January 15, 1934 earthquake remains the largest instrumentally recorded event in Nepal's history, at magnitude 8.0, with an epicentre in eastern Nepal near the Bihar border. It struck in the middle of the afternoon, which meant many people were outside rather than indoors, reducing casualties compared with a night-time event of the same size. Even so, the old brick-and-timber architecture of Kathmandu, Bhaktapur and Patan was devastated, with entire historic quarters reduced to rubble. Estimates commonly cited for total deaths across Nepal and Bihar combined run to roughly 10,700, though, as with many earthquakes from this era, published figures vary by source and Nepal's own share of that total is generally estimated rather than independently confirmed to the same precision as a modern instrumentally-verified disaster. The earthquake caused severe liquefaction across the Terai plains and heavily damaged Kathmandu's historic core, and it would be 81 years before Nepal experienced destruction on a comparable scale again.

1980 and 1988: Nepal's Vulnerability Was Never Only About Kathmandu

The July 1980 Bajhang earthquake, magnitude 6.5, struck Nepal's remote far west, killing roughly 200 people and destroying more than 13,000 homes in a region where road access and emergency services were, and largely remain, limited. Eight years later, the August 1988 Udayapur earthquake, magnitude 6.9, struck eastern Nepal at night, the most dangerous time for a building-collapse disaster, killing roughly a thousand people across Nepal and Bihar combined and triggering landslides across the Mahabharat hills. Udayapur in particular exposed how vulnerable ordinary rural construction across Nepal's eastern hills was, and it directly shaped the early work of the National Society for Earthquake Technology-Nepal, the organisation that has led much of Nepal's earthquake-safety education since.

2011: A Reminder That Distance Does Not Guarantee Safety

The September 2011 earthquake centred near the Nepal-Sikkim border, magnitude 6.9, killed a small number of people in Kathmandu itself, more than a hundred kilometres from the epicentre, when a wall collapsed, while causing more significant damage closer to the border in eastern Nepal. It is a useful, relatively recent example of the distance and intensity relationship described earlier in this guide: proximity to an epicenter is not the only thing that determines whether you are at risk.

The 2015 Gorkha Earthquake: The Earthquake That Changed Nepal

No single event shapes how modern Nepal thinks about earthquakes the way April 25, 2015 does. At 11:56 in the morning, a magnitude 7.8 earthquake ruptured the Main Himalayan Thrust with an epicentre in Gorkha district, roughly 80 kilometres northwest of Kathmandu. The shaking lasted under a minute but affected an enormous area: Kathmandu Valley, Gorkha, Sindhupalchok, Dhading, Rasuwa and dozens of other districts across central Nepal.

The human and physical toll was immense. Close to 8,964 people were killed and more than 21,000 injured. More than 600,000 families were left homeless, and economic damage was estimated at around 7 billion US dollars, close to a third of Nepal's annual GDP at the time. Fourteen UNESCO World Heritage sites in the Kathmandu Valley were damaged or destroyed, including the complete collapse of the historic Dharahara tower. Schools, hospitals and rural homes across the affected districts were damaged or destroyed on a scale Nepal had not experienced since 1934. The earthquake also triggered widespread landslides in the mountains, including an avalanche that struck Langtang village, and disrupted the trekking season across several major routes.

Seventeen days later, on May 12, 2015, while rescue and recovery work was still underway, a second major earthquake, magnitude 7.3, struck near Dolakha. It was large enough to be a significant disaster in its own right, and it killed more people in buildings that had already been weakened by the first event. Nepal recorded more than 300 aftershocks above magnitude 4 in the year that followed the mainshock, a scale of aftershock activity that shaped emergency planning for years afterward.

What Nepal Learned From 2015

The disaster did not end Nepal's engagement with earthquake risk; in many ways it began it in earnest. Reconstruction after 2015 pushed earthquake-resistant building standards into far wider use than before, including for ordinary rural homes rebuilt under national reconstruction guidelines. Public awareness of Drop, Cover and Hold On, of aftershock behaviour, and of the value of a simple household emergency plan spread far beyond the small circle of disaster-preparedness professionals who had promoted it for decades before. Community-level disaster management committees, emergency communication systems and coordinated response protocols involving the Nepal Army, Nepal Police and Nepal Red Cross were built out substantially in the years since. None of this means Nepal is now safe from a repeat event; it means the country's institutional and household-level preparedness is measurably different from what it was on April 24, 2015.

The 2023 Jajarkot Earthquake: A Modern Case Study

On November 3, 2023, a magnitude 5.7 earthquake struck Jajarkot district in Karnali Province, killing roughly 150 people and injuring hundreds more. By global standards, a magnitude 5.7 event is moderate, not great, and in a city built to modern seismic codes it would likely cause little to no loss of life. In Jajarkot and neighbouring Rukum West, among Nepal's most remote and least developed districts, traditional stone-walled homes without reinforcing mortar collapsed on residents who were mostly asleep when the earthquake struck close to midnight. Tens of thousands of homes were damaged or destroyed, and helicopters carrying rescue teams could not reach some of the worst-hit villages until daylight. Jajarkot is a compact, sobering illustration of a point this guide returns to more than once: magnitude alone does not determine how deadly an earthquake becomes. Building quality, timing, remoteness and emergency access matter just as much.

Then, Now, Next

Laid end to end, Nepal's earthquake history is less a list of disasters than a slow, ongoing lesson in how a country learns to live with unavoidable geological risk.

None of this means the risk has gone away, and this guide is not going to claim otherwise. Nepal's building stock still varies enormously between a reinforced concrete apartment in central Kathmandu and a stone house in rural Karnali, and a repeat of an event on the scale of 1934 or 2015 would still be a national catastrophe. What has changed is preparedness, not the underlying geology. That is exactly why the next sections of this guide exist: to turn Nepal's hard-earned earthquake history into something you can actually act on before the next one.

What Is an Aftershock?

An aftershock is an earthquake that follows a larger mainshock in the same general area, as the surrounding section of fault adjusts to the stress change caused by the first rupture. Aftershocks are usually, but not always, smaller than the mainshock, and they can still be strong enough on their own to damage buildings that were already weakened by the first event, as Nepal experienced directly with the May 12, 2015 Dolakha aftershock. Aftershock frequency generally decreases with time, but "generally decreases" is not the same as "always gets weaker," and a sequence can continue for days, weeks or considerably longer depending on the size of the mainshock. In rare cases, a later earthquake in a sequence turns out to be larger than the one that came before it; when that happens, seismologists reclassify the sequence, and the earlier, apparently larger event becomes a foreshock instead. This is exactly why this guide does not tell you that aftershocks always become weaker over time. That would be a reassuring oversimplification, not an accurate one.

Aftershock Safety Guide: How to Stay Safe After the First Shake

Aftershock Decision Guide

When Should You Stay Out of a Building?

Do not decide a damaged building is safe simply because the shaking has stopped. Warning signs include visible cracks in walls or columns, a wall or floor that looks even slightly out of alignment, leaning or bulging sections, a smell of gas, and exposed or damaged electrical wiring. For anything beyond obviously superficial, cosmetic damage, the right next step is an inspection by a qualified engineer or the relevant local authority, not a personal judgment call, and certainly not an AI-generated one. This guide can tell you what the warning signs look like; it cannot tell you that a specific building is safe.

Can Scientists Predict the Next Earthquake?

No, not with a precise date, time and magnitude. Scientists can monitor active fault systems, study historical rupture patterns, and estimate long-term probabilities for a given region and time window, but this is fundamentally different from predicting that a specific earthquake will occur at a specific hour. Even measuring an earthquake that has already happened is not always perfectly consistent: Nepal's own November 2023 Jajarkot earthquake was measured at magnitude 5.7 by the US Geological Survey, while Nepal's own national monitoring agency reported a somewhat higher local magnitude for the same event, a difference that reflects different measurement methods and networks rather than any error, and a useful real example of why a single "the magnitude was exactly X" headline can vary slightly between sources. Do not trust any message, however confident it sounds, that claims to know the exact date of Nepal's next major earthquake. No legitimate seismological organisation makes that claim, because the science genuinely does not support it.

Why Does Nepal Have So Many Earthquakes?

In simple terms, Nepal sits where the Indian tectonic plate is pushing into the Eurasian plate, a collision that has been building the Himalaya for tens of millions of years and has never stopped. The plates converge at a few centimetres a year, an almost imperceptible pace that nonetheless accumulates enormous strain along the fault system beneath Nepal, known as the Main Himalayan Thrust. That strain releases suddenly, as an earthquake, when a locked section of the fault finally slips. Earthquakes are not a malfunction in this system; they are how it has always worked.

This guide keeps the science brief by design. For a full breakdown of the fault system, Kathmandu Valley's specific ground conditions, and province-by-province seismic risk ratings, the Nepal Earthquake Live tracker includes a detailed tectonic and risk-analysis section for readers who want to go deeper than this guide's practical focus.

Nepal-Specific Safety Considerations

Earthquake Safety at Home

Before an Earthquake

Secure shelves, cabinets, televisions, gas cylinders and other heavy or hanging objects so they cannot fall or tip over during shaking. Prepare basic supplies in advance, including a flashlight, batteries or a power bank, first-aid supplies, water, essential medicines, copies of important documents, a whistle and sturdy shoes. Plan ahead as a household: agree on a family meeting location, a communication plan for when phone networks are congested, an evacuation route, and how you will account for children, elderly family members, or anyone with a disability who may need help.

Nepal Earthquake Emergency Kit

Make This Plan Tonight

A family earthquake plan is more useful than most people assume, and it does not take long to put together.

Nepal's national disaster hotline moved to 1234 in mid-2026, replacing the previously used 1149 number, and has since been extended to all 77 districts. If you have older material or a saved contact listing 1149, update it; 1234 is the current number as of this article's last update.

Earthquake Safety for Schools and Offices

Schools benefit most from regular, practiced evacuation drills, clear teacher responsibilities during and after shaking, an attendance and accountability system for the assembly point, and a plan for communicating with parents once children are confirmed safe. Offices should have a clear emergency plan, a designated assembly point away from the building, awareness of which stairwells to use, elevators clearly marked as off-limits during an emergency, basic fire-hazard awareness, and a way to communicate with employees once everyone is accounted for. Neither of these lists is a substitute for a structural engineer's assessment of a specific building; they cover organisational readiness, not construction safety.

What to Do If Someone Is Trapped

Staying calm and conserving energy matters more than it might seem. Signal your location using a whistle if you have one, or by tapping on a pipe or wall in a repeated, deliberate pattern rather than shouting continuously, which uses up air and energy quickly. Protect your mouth and nose from dust if possible. Avoid unnecessary movement, particularly if you suspect an injury, and call emergency services as soon as you are able to. This is safety information only; it is not a substitute for professional rescue guidance, and it does not encourage attempting a dangerous self-rescue or moving debris without proper support.

Understanding Magnitude vs Damage

It is tempting to reduce earthquake risk to a single rule, such as "magnitude 5 means minor damage." Nepal's own history shows why that shortcut fails. The 2023 Jajarkot earthquake, at a moderate magnitude 5.7, killed roughly 150 people, while many magnitude 5-plus earthquakes elsewhere in the world cause no deaths at all. The difference was not the shaking itself but everything around it: depth, distance from the nearest towns, local ground conditions, building quality, the time of night, and how quickly help could reach a remote district. Damage from any given earthquake depends on all of these factors together, not on magnitude in isolation, which is exactly why this guide has spent as much time on preparedness and building awareness as it has on the numbers themselves.

Earthquake Myths and Rumors

Frequently Asked Questions

Final Earthquake Safety Checklist

• I know the Drop, Cover and Hold On sequence and have practiced it at least once
• I know the safe spot in each room I spend time in regularly
• My household has an emergency meeting point outside
• I have a basic emergency kit prepared with water, first aid and a flashlight
• I have saved Nepal Police, Ambulance and the national disaster hotline numbers
• I know not to run outside while a building is actively shaking
• I know to expect aftershocks and not assume the first shake was the last
• I know not to re-enter a visibly damaged building
• I have bookmarked the Nepal Earthquake Live tracker to check verified data quickly
• I check information before sharing it, rather than forwarding unverified earthquake claims

Check Nepal Earthquake Activity