Skip to main content

Geomorphic Response of the Solani River Basin to Neotectonics: A Study from the Western Himalayan Foothills, India

  • Chapter
  • First Online:
Himalayan Neotectonics and Channel Evolution

Part of the book series: Society of Earth Scientists Series ((SESS))

Abstract

This study investigates the influence of neotectonics on the Solani River basin, using morphometric parameters, seismic signatures, and field-based study of unpaired river terraces. Morphometric parameters such as linear, areal, relief parameters, slope, aspect, stream-length (SL) index, and longitudinal river profile (LRP) suggest that the neotectonic activity triggered by the Himalayan tectonics affect the Solani River basin. Local convexity in the LRP indicates differential uplift along the associated faults. However, minor variation in knick points in LRP has been interpreted as rapid erosion due to unconsolidated to semi-consolidated nature of the sediments. The SL index of the Solani River ranges from 29.4 to 5233.2. The SL values along the river length indicates anomalies around the active fault zones. Mountain front sinuosity (Smf) adjacent to the river basin ranges from 1.04 to 1.13, suggesting tectonically active nature of the region. Unpaired terraces reported at Roorkee and Toda-Kalyanpur at the right bank of the river are evidence of neotectonics. Three unpaired terraces reported at Roorkee, have riser-height of 1, 1.5, and 3 m and tread-width of 50, 40, and 70 m. While the riser and tread could not be measured at Toda-Kalyanpur due to their deformed nature. These E-W aligned terraces present 1.5 km south of the present river course dated back to 2.5 Ka (T1) and 1.6 Ka (T2). These terraces were formed due to the river shifting in response to the uplift of the river basin along with the Ganga plain. The upliftment rate along the Himalaya in the area shows a good coherency with few of the morphotectonic signatures of the basin. Other morphometric parameters such as hypsometry, asymmetry, valley width height ratio, did not yield supporting result, probably due to the DEM error and the unconsolidated nature of the sediments.

This is a preview of subscription content, log in via an institution to check access.

Access this chapter

Chapter
USD 29.95
Price excludes VAT (USA)
  • Available as PDF
  • Read on any device
  • Instant download
  • Own it forever
eBook
USD 129.00
Price excludes VAT (USA)
  • Available as EPUB and PDF
  • Read on any device
  • Instant download
  • Own it forever
Softcover Book
USD 169.99
Price excludes VAT (USA)
  • Compact, lightweight edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info
Hardcover Book
USD 169.99
Price excludes VAT (USA)
  • Durable hardcover edition
  • Dispatched in 3 to 5 business days
  • Free shipping worldwide - see info

Tax calculation will be finalised at checkout

Purchases are for personal use only

Institutional subscriptions

References

Download references

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to Pitambar Pati .

Editor information

Editors and Affiliations

Rights and permissions

Reprints and permissions

Copyright information

© 2022 The Author(s), under exclusive license to Springer Nature Switzerland AG

About this chapter

Check for updates. Verify currency and authenticity via CrossMark

Cite this chapter

Patel, N.K., Pati, P. (2022). Geomorphic Response of the Solani River Basin to Neotectonics: A Study from the Western Himalayan Foothills, India. In: Bhattacharya, H.N., Bhattacharya, S., Das, B.C., Islam, A. (eds) Himalayan Neotectonics and Channel Evolution. Society of Earth Scientists Series. Springer, Cham. https://doi.org/10.1007/978-3-030-95435-2_4

Download citation

Publish with us

Policies and ethics