The Kashmir Seismic Gap lies between the areas affected by the 1905 Kangra earthquake and the 2005 Kashmir earthquake. This region aligns with the Jhelum basin and surrounding geological structures. Researchers have examined geomorphological evidence to assess whether large-scale dextral shear and block rotation are present in the gap.
Findings indicate that such features appear to be missing at a regional scale. The absence challenges some existing models of how strain accumulates and releases along the Himalayan front. Instead, the landscape shows localized deformation patterns that do not match expectations for widespread right-lateral movement.
Geomorphological indicators such as river offsets, terrace formations, and fault scarps were mapped across the area. These features suggest that deformation may be accommodated differently than previously thought. The study emphasizes the need for updated seismic hazard assessments that account for the observed lack of large-scale rotation.
The Kashmir Seismic Gap remains a zone of interest due to its position between two major historical ruptures. Understanding the mechanics within the gap helps clarify the potential for future earthquakes. Current data point to a more complex strain distribution than simple shear models predict.
Further fieldwork and remote sensing are recommended to refine these observations. The results contribute to broader discussions on how the India-Eurasia collision zone accommodates convergence in the northwest Himalaya. This work underscores the value of detailed surface studies in regions with limited instrumental records.
