Series of Mild Earthquakes Jolt Dharamsala Region; No Damage Reported

Dharamsala, June 6, 2026: A series of earthquakes, including a significant tremor measuring 4.9 on the Richter scale, shook the Dharamsala region on the night of June 5, causing panic among residents and prompting many to rush out of their homes.
The strongest earthquake occurred at 10:04 PM on June 5. Its epicenter was located approximately 41 kilometers from Dharamsala, between Dhar Ghadoi and R.F. Kugti in the Dhauladhar ranges along the Kangra–Chamba border. The quake originated at a depth of 22.5 kilometres beneath the Earth's surface.
Although the tremor was brief, it was widely felt across Dharamshala and surrounding areas. Residents reported strong shaking, but no loss of life or major property damage has been reported so far.
The seismic activity began earlier in the day. At 8:52 AM, a mild earthquake measuring 2.3 magnitude was recorded near Minkiani Pass in the Dhauladhar ranges, about 16 kilometres from Dharamsala. While the tremor was too weak to be felt by most people, it marked the beginning of a day of heightened seismic activity.
Following the 4.9-magnitude quake, two additional tremors were recorded later in the night. A 2.8-magnitude earthquake struck at 11:03 PM near Dhar Gharoh, about 18 kilometres from Dharamsala, followed by another tremor of 3.0 magnitude at 11:52 PM near R.F. Hilang, approximately 23 kilometres from the town.
Kangra district, with Dharamshala as its headquarters, falls under Seismic Zone V, the highest earthquake-risk category in India. Earthquakes of magnitude 3 to 4 are generally considered minor and rarely cause structural damage, although they are often felt by residents.
Seismologists note that frequent small earthquakes in the young Himalayan mountain system may act as "natural stress relievers" along geological fault lines, helping release accumulated tectonic pressure. However, experts caution that such activity does not eliminate the possibility of a major earthquake in the future.
The recent tremors have revived memories of the devastating Kangra Earthquake of April 4, 1905, one of the deadliest earthquakes in Indian history. Measuring approximately 7.8 magnitude, the disaster claimed more than 20,000 lives and destroyed over 100,000 buildings across the region.
Several historic landmarks, including Kangra Fort, Brajeshwari Temple, and St. John in the Wilderness Church, suffered extensive damage. The earthquake was felt across a vast area stretching from Amritsar and Lahore to Dehradun.
The Himalayas are among the youngest and most tectonically active mountain ranges in the world. They were formed around 50 million years ago when the Indian Plate collided with the Eurasian Plate. This collision continues today, with the mountains still rising at an average rate of nearly one centimetre per year.
The ongoing movement of these massive tectonic plates generates enormous geological stress beneath the region, making the Himalayas highly susceptible to earthquakes. While erosion from rivers, glaciers, and weathering continually reshapes the mountains, tectonic forces remain active beneath the surface.
The latest series of tremors serves as a reminder that Dharamsala and the Kangra Valley remain among India's most earthquake-sensitive regions, underscoring the need for continuous preparedness, resilient infrastructure, and public awareness.