Author(s)

Deshraj Trivedi, Koravangatt Devi, Ilya Buynevich, P. Srinivasan, K. Ravisankar, Vipul Silwal, D. Sengupta, Rajesh R. Nair

Indian Institute of Technology.
Structural Engineering Research Centre.
Temple University.

The coastal dunes located near the Ashirmata region, south of Mandvi beach lies near the straight coast have been stud-ied by making use of sedimentological information and Ground Penetrating Radar (GPR) data. Sedimentological analy-sis reveals the NNW-SSE trending longitudinal dunes consists of well sorted fine sands with unimodal distribution pos-sibly formed by constant wind gust and also the point out to the origin of sediments from single source; mostly the sediments derived from Indus delta transported to beach by long shore drift and tidal waves, carried inland by local on-shore winds. The radargram confirms, the homogenous sand layers with paleosols at shallow depth slip faces are proba-bly formed due to extreme storm activity of Recent.

Coastal Dune; Ashirmata Region; Sedimentogical Analysis; Ground Penetrating Radar; Paleosol

D. Trivedi, K. Devi, I. Buynevich, P. Srinivasan, K. Ravisankar, V. Silwal, D. Sengupta and R. Nair, "Interpretation of Dune Genesis from Sedimentogical Data and Ground Penetrating Radar (GPR) Signatures: A Case Study from Ashirmata Dune Field, Mandvi Beach, Gujarat, India," International Journal of Geosciences, Vol. 3 No. 4, 2012, pp. 772-779. doi: 10.4236/ijg.2012.34078.