Interpretation of Dune Genesis from Sedimentogical Data and Ground Penetrating Radar (GPR) Signatures: A Case Study from Ashirmata Dune Field, Mandvi Beach, Gujarat, India

Abstract

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.

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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.

Conflicts of Interest

The authors declare no conflicts of interest.

References

[1] W. Ritchie and S. Penland, “Aeolian Sand Bodies of the South Lousiana Coast,” Coastal Morphology and Research, John Wiley, Chichester, 1990, pp. 105-127.
[2] A. McLachlan, “Dissipative Beaches and Macrofauna Communities on Exposed Intertidal Sands,” Journal of Coastal Research, Vol. 6, 1990, pp. 57-71.
[3] R. A. Bagnold, “The Physics of Blown Sand and Desert Dunes London: Methuen,” Progress in Physical Geography, Vol. 18, No. 1, 1994, pp. 91-96. doi:10.1177/030913339401800105
[4] I. Livingstone and A. Warren, “Aeolian Geomorphology: An Introduction,” Longman, Essex, 1996, p. 221.
[5] R. A. Davis Jr. and D. M. FitzGerald, “Beaches and Coasts,” Blackwell Science Ltd., Oxford, 2004, p. 419.
[6] J. A. Jimenez, L. P. Maia, J. Serra and J. Morais, “Aeolian Dune Migration along the Ceara Coat, North-East- ern Brazil,” Sedimentology, Vol. 46, 1999, pp. 689-701. doi:10.1046/j.1365-3091.1999.00240.x
[7] N. Levin, H. Tsoar, H. J. Herrmann, V. Claudino-Sales and L. P. Maia, “Modelling the Formation of Arcuate Vegetated Dune Ridges Behind Barchans Dunes in NE Brazil,” Sedimentology, Vol. 56, 2009, pp. 1623-1641. doi:10.1111/j.1365-3091.2009.01048.x
[8] B. Greenwood, “Spatial Variability of Texture over a Beach-Dune Complex, North Devon,” Sedimentary Geology, Vol. 21, No. 1, 1978, pp. 21-44. doi:10.1016/0037-0738(78)90032-5
[9] K. Pye, “Morphological Development of Coastal Dunes in Humid Tropical Environment, Cape Bedford and Cape Flattery, North Queensland,” Geographiska Annaler, Vol. A64, 1982, pp. 212-227.
[10] Vincent, “Differentiation of Modern Beach and Coastal Dune Sands—A Logistic Regression Approach Using the Parameters of the Hyperbolic Function,” Sedimentary Geology, Vol. 49, No. 3-4, 1986, pp. 167-176. doi:10.1016/0037-0738(86)90036-9
[11] D. M. McCann, P. D. Jackson and P. J. Fenning, “Comparison of the Seismic and Ground Probing Radar Methods in Geological Surveying,” Proceedings of the Institute of Electrical Engineers, Vol. 135, No. 4, 1988, pp. 380-390.
[12] K. F. Nordstrom, N. Psuty and R. W. G. Carter, “Coastal Dunes form and Process,” Wiley, Chichester, 1986, p. 392.
[13] J. L. Davis and A. P. Annan, “Ground-Penetrating Radar for High Resolution Mapping of Soil and Rock Stratigraphy,” Geophysical Prospecting, Vol. 37, No. 5, 1989, pp. 531-551. doi:10.1111/j.1365-2478.1989.tb02221.x
[14] R. L. Gawthorpe, R. E. Ll Collier, J. Alexander, J. S. Bridges and M. R. Leeder, “Ground Penetrating Radar: Application to Sand Body Geometry and Heterogeneity Studies,” In: C. P. North and D. J. Prosser, Eds., 14 Characterization of Fluvial and Aeloian Reservoirs, Geological Society Special Publication No. 73, The Geological Society, London, 1993, pp. 421-432.
[15] D. G. Smith and H. M. Jol, “Ground Penetrating Radar: Antenna Frequencies and Maximum Probable Depths of Penetration in Quaternary Sediments”, Journal of Applied Geophysics, Vol. 33, No. 1, 1995, pp. 93-100.
[16] A. K. Benson, “Application of Ground Penetrating Radar in Assessing Some Geological Hazards: Examples of Groundwater Contamination, Faults, Cavities,” Journal of Applied Geophysics, Vol. 33, No. 1-3, 1995, pp. 177-193.
[17] Z. Harari, “Ground-Penetrating Radar (GPR) for Imaging Strtigraphic Features and Groundwater in Sand Dunes,” Journal of Applied Geophysics, Vol. 36, No. 1, 1996, pp. 43-52. doi:10.1016/S0926-9851(96)00031-6
[18] C. Bristow, J. Pugh and T. Goodall, “Internal Structure of Aeolian Dunes in Abu Dhabi Determined Using Ground- Penetrating Radar,” Sedimentology, Vol. 43, No. 6, 1996, pp. 995-1003. doi:10.1111/j.1365-3091.1996.tb01515.x
[19] J. J. Daniels, J. Brower and F. Baumgartner, “High- Resolution GPR at Brookhaven National Laboratory to Delineate Complex Subsurface Targets,” Journal of Environmental and Engineering Geophysics, Vol. 3, No. 1, 1998, pp. 1-6. doi:10.4133/JEEG3.1.1
[20] R. L. van Dam, E. H. Van Den Berg, S. Van Heteren, C. Kasse, J. A. M. Kenter and K. Groen, “Influence of Organic Matter on Radar-Wave Reflection: Sedimentological Implications,” Journal of Sedimentary Research, Vol. 72, No. 3, 2002, pp. 341-352. doi:10.1306/092401720341
[21] G. A. Botha, C. S. Bristow, N. Porat, G. Dulle, S. J. Armitage, H. M. Roberts, B. M. Clarke, M. W. Kota and P. Schoeman, “Evidence for Dune Reactivation from GPR Profiles on the Maputuland Coastal Plain, South Africa, in Ground Penetrating Radar in Sediments,” In: C. S. Bristow and H. M. Jol, Eds., Geological Society Special Publication, Vol. 211, 2003, pp. 29-46.
[22] P. Felix-Henningsen, A. W. Kandel and N. J. Conard, “The Significance of Calcretes and Paleosols on Ancient Dunes of the Western Cape South Africa, as Stratigraphic Markers and Paleoenvironmental Indicators,” In: G. Füleky, Ed., Papers of the 1st International Conference on Archaeology and Soils, British Archaeological Reports. International Series, Vol. 1163, 2003, pp. 45-52.
[23] A. K. Singhvi and A. Kar, “The Aeolian Sedimentation Record of the Thar Desert,” Proceedings of the Indian Academy of Science (Earth Planet Sciences), Vol. 113, No. 3, 2004, pp. 371-401.
[24] S. B. Shukla, S. P. Prizomwala, V. Ukey, N. Batt and L. S. Chamyal, “Coastal Geomorphology and Tsunami Hazard Scenario along Kuchchh Coat, Western India,” Indian Journal of Geo-Marine Sciences, Vol. 39, 2010, pp. 549- 556.
[25] B. Carter and P. Wilson, “Geomorphological, Sedimentological and Pedological Influences on Coastal Dune Development in Ireland,” Journal of Coastal Research, Special Issue, 1988, pp. 27-31.
[26] V. Ramaswamy , N. B. Nagender, P. Vethamony and D. Illangovan, “Source and Dispersal of Suspended Sediment in Macro-Tidal Gulf of Kuchchh,” Marine Pollution Bulletin, Vol. 54, 2007, pp. 708-719. doi:10.1016/j.marpolbul.2007.01.026
[27] J. J. Kasper-Zubillaga and A. Carranza-Edwards, “Grain Size Discrimination between Sands of Desert and Coastal Dunes from Northwestern Mexico,” Revista Mexicana de Ciencias Geologicas, Vol. 22, 2005, pp. 383-390.
[28] S. P. Prizomwala, S. B. Shukla and N. Bhatt, “Geomorphic Assemblage of the Gulf of Kachchh Coast, Western India: Implications in Understanding the Pathways of Coastal Sediments,” Zeitschrift für Geomorphologie, Vol. 54, 2010, pp. 31-46. doi:10.1127/0372-8854/2010/0054-0003
[29] R. G. D. Davidson-Arnott and N. M. Pyskir, “Morphology and Formation of an Holocene Coastal Dune Field, Bruce Peninsula, Ontario,” Géographie Physique et Quaternaire, Vol. 42, No. 2, 1988, pp. 163-170. doi:10.7202/032722ar
[30] K. Nordstrom, N. Psuty and B. Carter, Eds., “Coastal Dunes: Form and Process,” Wiley, Chichester, 1988, p. 392.
[31] C. M. Marco, de M. Luna, E. J. R. Parteli, O. Durán and H. J. Herrmann, “Model for the Genesis of Coastal Dune Fields with Vegetation,” Geomorphology, Vol. 129, 2011, pp. 215-224. doi:10.1016/j.geomorph.2011.01.024
[32] A. Kar, “Morphology and Evolution of Sand Dunes in the Thar Desert as Key to Sand Control Measures,” Indian Journal of Geomorphology, Vol. 1, No. 2, 1996, pp. 177- 206.
[33] S. K. Wadhawan, “Textural Attribute of Recent Aeolian Stratigraphy in the Ghaggar Basin of Thar Desert, India,” Journal of Arid Environments, Vol. 32, 1996, pp. 59-74. doi:10.1006/jare.1996.0006
[34] M. R. Leeder,“ Sedimentology: Process and Product”, Allen and Unwin, London, 1982, p. 344.
[35] J. J. Kasper-Zubillaga and A. Carranza-Edwards, “Grain Size Discrimination between Sands of Desert and Coastal Dunes from Northwestern Mexico,” Revista Mexicana de Ciencias Geológicas, Vol. 22, 2005, pp. 383-390.
[36] R. L. Folk, “Petrology of Sedimentary Rocks,” University of Texas Publication, Austin, 1968, p. 170.
[37] A. Kar, “Origin and Transformation of Longitudinal Sand Dunes in the Indian Desert,” Zeitschrift fur Geomorphologie, Vol. 31, 1987, pp. 311-337.
[38] A. Kar, “Granulometry of Aeolian Bedforms in the Extremely Arid Jaisalmer Region of Thar Desert,” In: S. K. Tandon and B. Thakur , Eds., Recent Advances in Geomorphology, Quaternary Geology and Environmental Geosciences: Indian Case Studies, Manisha Publications, New Delhi, 2002, pp. 261-286.
[39] I. V. Buynevich, A. Bitinas and D. Pupienis, “Lithological Anomalies in a Relict Coastal Dune: Geophysical and Paleoenvironmental Markers,” Geophysical Research Letters, Vol. 34, 2007, Article ID: L09707. doi:10.1029/2007GL029767
[40] R. K. Borowka, “Problem of the Morphology of Fossil Dune Forms on the £Eba Bar,” Quaestiones Geographi- cae, Vol.2, 1975, pp. 39-51.
[41] J. Sevink, “Soil Development in the Coastal Dunes and Its Relation to Climate,” Landscape Ecology, Vol. 6, No. 1-2, 1991, pp. 49-56. doi:10.1007/BF00157744
[42] K. Pye, “Late Quaternary Development of Coastal Parabolic Megadune Complexes In Northeastern Australia, in Eolian Sediments: Ancient and Modern,” In: K. Pye and N. Lancaster, Eds., International Association of Sedimentology, Blackwell Science, Oxford, Special Publishing, Vol. 16, 1993, pp. 23-44.
[43] P. Wilson, J. D. Orford, J. Knight, S. M. Braley and A. G. Wintle, “Late-Holocene (Post-4000 Years BP) Coastal Dune Development in Northumberland, Northeast England,” Holocene, Vol. 11, No. 2, 2001, pp. 215-229. doi:10.1191/095968301667179797
[44] R. L. van Dam, S. L. Nichol, P. C. Augustinus, K. E. Parnell, P. L. Hosking and R. F. McLean, “GPR Stratigraphy of a Large Active Dune on Parengarenga Sandspit, New Zealand,” Leading Edge, Vol. 22, No. 9, 2003, pp. 865-870. doi:10.1190/1.1614159
[45] K. G. Havholm, D. V. Ames, G. R. Whittecar, B. A. Wenell, S. R. Riggs, H. M. Jol, G. W. Berger and M. A. Holmes, “Stratigraphy of Backbarrier Coastal Dunes, Northern North Carolina and Southern Virginia,” Journal of Coastal Research, Vol. 20, No. 4, 2004, pp. 980-999. doi:10.2112/03503A2.1
[46] M. L. Clarke and H. M. Rendell, “Effects of Storminess, Sand Supply and the North Atlantic Oscillation on Sand Invasion and Coastal Dune Accretion in Western Portugal,” Holocene, Vol. 16, 2006, pp. 341-355. doi:10.1191/0959683606hl932rp
[47] S. K. Tandon, M. Jain and A. K. Singhvi, “Comparative Development of Mid- to Late Quaternary Fluvial and Fluvio-Aeolian Stratigraphy in the Luni, Sabarmati and Mahi river Basins of Western India,” Gondwana Geology Magazine, Vol. 4, 1999, pp. 1-16.
[48] S. K. Tandon, B. K. Sareen, M. S. Rao and A. K. Singhvi, “Aggradation History and Luminescence Chronology of Late Quaternary Semi-Arid Sequences of the Sabarmati Basin, Gujarat,” Palaeogeography, Palaeoclimatology, Palaeoecology, Vol. 128, No. 1, 1997, pp. 339-357. doi:10.1016/S0031-0182(96)00035-1
[49] A. Kar, A. K. Singhvi, S. N. Rajaguru, N. Juyal, J. V. Thomas, D. Banerjee and R. P. Dhir, “Reconstruction of Late Quaternary Environment of the Lower Luni Plains, Thar Desert, India,” Journal of Quaternary Science, Vol. 16, 2001, pp. 61-68. doi:10.1002/1099-1417(200101)16:1<61::AID-JQS562>3.0.CO;2-G
[50] N. Juyal, A. Kar, S. N. Rajaguru and A. K. Singhvi, “Luminescence Chronology of Aeolian Deposition during the Late Quaternary on the Southern Margin of Thar Desert, India,” Quaternary International, Vol. 104, 2003, pp. 87-98. doi:10.1016/S1040-6182(02)00137-4
[51] J. V. Thomas, A. Kar, A. J. Kailath, N. Juyal, S. N. Rajaguru and A. K. Singhvi, “Late Pleistocene—Holocene History of Aeolian Accumulation in the Thar Desert, India,” Zeitschrift fur Geomorphologie Supplement Band, Vol. 116, 1999, pp. 181-194.
[52] T. Naruse, “Aeolian Geomorphology of the Punjab Plains and the North Indian Desert,” Annals of Arid Zone, Vol. 24, No. 4, 1985, pp. 267-280.
[53] M. P. Patel and S. J. Desai, “Environmental Significance of Fossil Sand Dunes of North Gujarat,” Proceedings of National seminar on Recent Quaternary Studies in India, 1988, pp. 139-147.
[54] Juyal, R. Raj, D. M. Mourya, L. S. Chamyal and A. K. Singhvi, “Chronology of the Late Pleistocene Environment Changes in the Lower Mahi Basin, Western India,” Journal of Quaternary Sciences, Vol. 15, No. 5, 2000, pp 501-508. doi:10.1002/1099-1417(200007)15:5<501::AID-JQS528>3.0.CO;2-J
[55] S. A. Wolfe, D. R. Muhs, P. P. David and J. P. McGeehin, “Chronology and Geochemistry of Late Holocene Eolian Deposits in the Brandon Sand Hills, Manitoba, Canada,” Quaternary International, Vol. 67, 2000, pp. 61-74. doi:10.1016/S1040-6182(00)00009-4

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