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What is the news?
According to a study, major earthquake events in the last 30,000 years resulted in spectacular changes in the landscape of the Katrol Hill Fault in the Kachchh region in Gujarat.
Seismicity in Kachchh Region
Seismicity in the Kachchh region is highly complex as it is characterized by multiple seismic sources in the form of fault lines which release continuously accumulating tectonic stresses at intervals producing earthquakes.
Real-time monitoring of earthquakes since the occurrence of 2001 Bhuj earthquake indicate that most of the faults in the region: Kachchh Mainland Fault (KMF), South Wagad Fault (SWF), Gedi Fault (GF), and Island Belt Fault (IBF) are seismically active.
However, seismic activity along faults like Katrol Hill Fault (KHF) is not apparent.
What is the study undertaken by the Geologists?
The study was undertaken to understand the seismic activity along Katrol Hill Fault (KHF) in the Kachchh region.
The study was funded mainly under the FIST Programme of the Department of Science & Technology.
| Note: Fund for Improvement of S&T Infrastructure (FIST) Programme was launched in the year 2000 to strengthen S&T infrastructure with adequate funding and associated flexibility. |
What are the key findings of the study?
Katrol Hill Fault(KHF) has produced high magnitude seismic events during the past ~30,000 years. These seismic events resulted in spectacular changes in landscape, as evidenced by the disruption and reorganization of the channel of the Gunawari River in the fault zone.
Hence, it can be a credible seismic source capable of generating surface rupture hazard in the Kachchh Basin.
What is the significance of the study?
The findings of this study necessitates a revised seismic hazard assessment and mitigation strategies in Kachchh Basin, owing to its close proximity to industrial corridors and major settlements, including Bhuj city.
Source: This post is based on the article “Spectacular landscape changes detected in Gujarat’s Kachchh region due to major earthquakes in recent geological past” published in PIB on 12th January 2022.
