SRINAGAR — For decades, earthquakes in Kashmir have arrived as sudden disasters and then faded into memory. Buildings were rebuilt, roads reopened, and daily life resumed. Yet beneath the Valley’s towns, orchards, and wetlands, the geological forces that produced some of the Himalaya’s most destructive earthquakes have never stopped moving.
Two peer-reviewed scientific studies published in 2026 have renewed warnings that Kashmir remains one of the most vulnerable earthquake regions in South Asia. Their message is not that a major earthquake is imminent, nor that scientists know when one will occur. Rather, the studies argue that several risk factors — active faults, accumulated tectonic strain, vulnerable soils, dense urbanisation, and weak construction practices — continue to converge in ways that could amplify the impact of a future high-magnitude earthquake.
The concern comes at a time when Jammu and Kashmir has been placed in the newly notified Seismic Zone VI classification under IS 1893 (Part 1):2025, the highest seismic-risk category in India’s revised earthquake-zoning framework, reflecting official recognition of the region’s exposure to strong ground shaking.
A Valley Built on a Collision
The Kashmir Valley exists because of one of the most powerful geological processes on Earth: the ongoing collision between the Indian and Eurasian tectonic plates.
That collision, which began tens of millions of years ago and continues today, created the Himalaya. However, the mountains are not static. The Indian plate continues pushing northward, compressing the crust and generating enormous amounts of strain energy.
According to the review paper by Waseem Qader, Irfan Maqbool Bhat, and Mehran Qurashi, published in the Proceedings of the Indian National Science Academy, Kashmir sits amid a complex network of active tectonic structures, including the Himalayan Frontal Thrust, Main Boundary Thrust, Main Central Thrust, Main Mantle Thrust, Kishtwar Fault, and Balapur Fault. These structures accommodate the ongoing plate collision and are capable of generating large earthquakes.
The authors describe Kashmir as part of a significant “seismic gap” — a segment of the Himalayan arc where strain appears to have accumulated over long periods without being fully released through major earthquakes. In seismology, such gaps are closely monitored because they may indicate areas where stress continues to build. However, scientists caution that a seismic gap does not reveal when an earthquake will occur.
What the New Research Says
The January 2026 review synthesised geological, geophysical, seismological, and geodetic evidence from decades of research. Its central conclusion was stark: Kashmir’s seismic hazard is not driven by a single fault or isolated threat but by the interaction of multiple geological and societal vulnerabilities.
A second study, published in February 2026 in Physics and Chemistry of the Earth by geoscientist Ayaz Mohmood Dar, reached similar conclusions using a different approach. Dar analysed historical earthquake records, United States Geological Survey data, and geophysical surveys of the Kashmir Basin. The research identified approximately 1,000 earthquakes of magnitude 3 or greater since 1905, including nearly 150 events exceeding magnitude 5. Clusters of seismic activity were found along the north-northwest and south-southeast extensions of the basin.
Dar’s study concluded that the possibility of a future large-magnitude earthquake in Kashmir cannot be ruled out and called for greater emphasis on risk-based engineering and seismic hazard assessment.
The Balapur Fault and Hidden Structures Beneath the Valley
One of the more significant aspects of the 2026 research concerns the Balapur Fault, a geological structure running beneath parts of the Kashmir Basin.
Using Total Magnetic Intensity (TMI) surveys, Dar identified magnetic anomalies and low-magnetic zones associated with fault-related activity. These findings build upon earlier geophysical studies suggesting that the Balapur Fault extends for roughly 100 kilometres across parts of the Valley and may be linked to a broader system of subsurface fractures.
Scientists are careful not to claim that any particular fault will generate the next major earthquake. What the magnetic data reveal instead is that active geological structures continue to exist beneath the Valley and remain relevant to future hazard assessments.
The Threat Beneath the Ground
Earthquake risk in Kashmir is not solely about faults. It is also about what lies above them.
The 2026 review highlights extensive deposits of Quaternary-age lake and river sediments across the Valley floor. These sediments, laid down over thousands of years, create conditions that may increase the likelihood of liquefaction during intense shaking. Liquefaction occurs when water-saturated soils temporarily lose their strength and behave like a liquid. Buildings can tilt, foundations can fail, and roads can deform.
Previous studies cited by the review identify parts of Srinagar, Baramulla, and Kupwara as areas with high to very high liquefaction susceptibility. The combination of loose sediments and shallow groundwater is particularly concerning because it can amplify seismic shaking while simultaneously weakening the ground supporting structures.
In practical terms, two buildings exposed to the same earthquake may experience very different outcomes depending on the ground beneath them.
The Real Vulnerability: Buildings
The strongest theme emerging from the latest research is that future earthquake losses in Kashmir will depend less on the earthquake itself and more on how society prepares for it.
The studies repeatedly point to the Valley’s built environment as a critical vulnerability.
Rapid urban growth has transformed Kashmir over recent decades. Multi-storey concrete buildings have spread across urban and semi-urban areas, often without detailed site-specific geotechnical investigations. The review notes concerns regarding shallow foundations, inconsistent enforcement of seismic design requirements, and the prevalence of non-engineered construction.
Engineering simulations referenced in the review found that substantial lateral forces can act on typical structures during strong shaking. Such forces are often what cause walls, columns, and structural connections to fail.
Professor Shakil Ahmad Romshoo, Vice-Chancellor of the Islamic University of Science and Technology and a long-time researcher of Himalayan hazards, has repeatedly argued that the greatest danger lies not in the earthquake itself but in the vulnerability of infrastructure and society.
Research co-authored by Romshoo found that nearly 98 percent of Srinagar’s buildings are masonry structures with limited seismic resistance. The vulnerability is especially acute in older neighbourhoods where narrow roads, dense construction, and limited open spaces could complicate emergency response efforts after a major earthquake.
He has also warned that many schools and hospitals remain insufficiently earthquake-resistant, raising concerns about critical infrastructure during disasters.
Traditional Architecture Offers Lessons
One notable observation from the 2026 review is that some traditional Kashmiri construction methods may hold valuable lessons for modern earthquake resilience.
Historic systems such as Taq and Dhajji Dewari employ timber-laced masonry and flexible framing techniques that have demonstrated superior performance during past earthquakes. Their ability to absorb and dissipate seismic energy contrasts with the brittle failure mechanisms often observed in poorly designed masonry structures.
Researchers do not suggest abandoning modern engineering. Rather, they argue that traditional seismic wisdom should inform contemporary building practices, especially in earthquake-prone mountain regions.
Preparedness, Not Prediction
Despite public fascination with earthquake forecasts, the scientific consensus remains unchanged: earthquakes cannot currently be predicted with sufficient accuracy regarding time, location, and magnitude.
The latest studies make no prediction about when a major earthquake might strike Kashmir. Their warnings are based on long-term geological conditions, historical seismicity, and present-day vulnerabilities.
This distinction matters.
The research does not say that a devastating earthquake is about to happen. It says that the underlying conditions that produced destructive earthquakes in the past continue to exist, while rapid urbanisation may have increased the consequences of a future event.
For scientists, the central question is not whether earthquakes will return to Kashmir. Geological history makes that virtually inevitable over long timescales. The question is whether the region’s infrastructure, institutions, and communities will be better prepared when they do.
The 2026 studies converge on a common set of recommendations: stronger enforcement of seismic building codes, retrofitting vulnerable structures, expanding hazard assessments, developing earthquake early-warning capabilities, implementing community-level awareness programmes, and conducting regular preparedness drills.
In the end, the most important lesson from the latest science may be that Kashmir’s earthquake threat is not a future problem. It is a present condition — one that exists every day beneath the Valley, whether people are thinking about it or not.
Haseena Ayoob is a regular contributor of The Chenab Times.