Bhuj, well known for the deadly 2001 earthquake, is still extremely seismic due to its placement on a tectonic plate boundary, rendering it susceptible to regular and severe earthquakes.
Darbhanga is located in seismic zone IV and sees frequent earthquakes due to its proximity to the Himalayan foothills, leaving it susceptible to substantial seismic activity.
Guwahati, located in a seismically active zone, is at high danger of earthquakes due to tectonic plate movements in the Northeast, demanding stringent building rules and emergency preparedness.
This capital city is located in a high seismic zone with a history of significant earthquakes caused by the complicated tectonics of the Indo-Myanmar border region.
Jorhat, located in one of India's most earthquake-prone locations, is constantly subjected to seismic activity as a result of Northeast India's active tectonic processes.
Mandi, located in the Himalayas, is prone to earthquakes because to the continuous collision of the Indian and Eurasian tectonic plates, resulting in regular seismic disturbances.
Port Blair, located near the tectonically active boundary of the Indian and Burmese plates, is prone to regular earthquakes and tsunamis.
Sadiya, as part of the seismically active Northeast, is vulnerable to earthquakes caused by geological forces along the Indo-Burmese arc, necessitating effective disaster management techniques.
Srinagar, located in the highly seismic Himalayan region, is subject to earthquakes caused by continuous tectonic activity between the Indian and Eurasian plates.
The capital city is located in active seismic zone IV, which poses a moderate to high earthquake danger from the nearby Himalayan seismic belt, highlighting the necessity for strict building standards.