Abstract
Chameis Bay is located about 115 km north of the Orange River mouth and falls within the Sperrgebiet, an area which hosts the world’s largest gem diamond deposit. Although significant quantities of diamonds have been recovered both on land and from offshore deposits in the Chameis Bay area, the marine geology of this important tract of coastline has not previously been described in the scientific literature. Here, we report the nearshore geomorphology and seismic stratigraphy offshore of Chameis Bay through analyses of bathymetrical and seismic datasets. These data have been complemented with lithogical data obtained from 70 reverse-circulation boreholes which helped to confirm and constrain the sedimentary stratigraphy of the study area. These datasets identified four major lithological units; viz. a Precambrian basement which predominates as the footwall in the nearshore regions of the study area, a Cretaceous clay unit that represents the offshore footwall lithology and two unconsolidated Cenozoic sedimentary units. The distribution of these unconsolidated sediments is strongly controlled by the ambient accommodation space which can be quantified by considering the architecture of the respective footwall units. Architectural features within the study site include two prominent wave-cut platforms, two coast-parallel sea cliffs, and a shelf-break formed at the contact between the Precambrian basement and the Cretaceous clay footwall. Accommodation space exists on the seaward of the two wave-cut platforms, which is cut into the Precambrian basement footwall and which lies below the fair-weather wave base, and at the break in slope at the contact between the two footwall units. The former accommodation space is most notable for gravel entrapment and preservation since gulley-controlled jointing and erosional depressions at lithological contacts represent ‘fixed’ trapsites from which coarse material is less likely to be remobilised. In contrast, the trapsites formed on the soft Cretaceous clay footwall are regarded as ‘mobile’ trapsites since they can be easily reconfigured by continuing erosional processes. As a result, the gravel bodies found above the Cretaceous clay are generally thin and poorly developed. The implications of these two different trapsites are briefly discussed in terms of diamond preservation potential, where anticipated diamond sources to the Chameis Bay near-shelf include the Orange River mouth as well as material that has been reworked from proximal sources. These results represent the first detailed description of the marine geology of the Chameis Subterrane thrust sheet and complement existing understanding of the Sperrgebiet’s marine geology which largely derives from study sites on the Oranjemund Subterrane where linear beaches predominate.
Graphical abstract
Similar content being viewed by others
References
Apollus L (1995) The distribution of diamonds on a Late Cainozoic gravel beach, southwestern Namibia. Dissertation, University of Glasgow
Beerbower JR (1964) Cyclothems and cyclic depositional mechanisms in alluvial plain sedimentation. Kansas State Geol Surv Bull 169(1):32–42
Bluck BJ, Ward JD, Cartwright J, Swart R (2007) The Orange River, southern Africa: an extreme example of a wave-dominated sediment dispersal system in the South Atlantic Ocean. J Geol Soc 164:341–351
Cecil CB (2003) The concept of autocyclic and allocyclic controls on sedimentation and stratigraphy, emphasizing the climate variable. In: Cecil CB, Edgar NT (eds) Climate controls on stratigraphy: SEPM Special Publication No. 77. Society for Sedimentary Geology, Tulsa, pp 13–20
Clark PU, Dyke AS, Shakun JD, Carlson AE, Clark J, Wohlfarth B, Mitrovica JX, Hostetler SW, McCabe AM (2009) The last glacial maximum. Science 325(5941):710–714
Compton J (2001) Holocene sea-level fluctuations inferred from the evolution of depositional environments of the southern Langebaan Lagoon salt marsh. South Africa the Holocene 11(4):395–405
Compton JS, Mulanisana J, McMillan IK (2002) Origin and age of phosphorite from the Last Glacial Maximum to Holocene transgressive succession off the Orange River, South Africa. Mar Geol 186:243–261
Cooper JAG, Green AN, Compton JS (2018) Sea-level change in southern Africa since the Last Glacial Maximum. Quatern Sci Rev 201:303–318
Cooper JAG, Masselink G, Coco G, Short AD, Castelle B, Rogers K, Anthony E, Green AN, Kelley JT, Pilkey OH, Jackson DWT (2020) Sandy beaches can survive sea-level rise. Nat Clim Chang 10(11):993–995
Davies JL (1964) A morphogenic approach to world shorelines. Zeitschrift Fur Geomorphologie 8:127–142
De Decker RH (1986) The geological settings of diamondiferous deposits on the inner shelf between the Orange River and Wreck Point. Thesis (unpublished), University of Cape Town, Namaqualand. M.Sc, p 258
De Wit M, Bhebhe Z, Davidson J, Haggerty SE, Hundt P, Jacob RJ, Lynn M, Marshall TR, Skinner C, Simithson K, Stiefenhofer J, Robert M, Revitt A, Spaggiari R, Ward JD (2016) Overview of diamond resources in Africa. Episodes 39(2):199–234
Dingle RV, Siesser WG, Newton AR (1983) Mesozoic and Tertiary geology of southern Africa. AA Balkema, Rotterdam
Engelbrecht L, Green AN, Cooper JAG, Hahn A, Zabel M, Mackay CF (2020) Construction and evolution of submerged deltaic bodies on the high energy SE African coastline: the interplay between relative sea level and antecedent controls. Mar Geol 424:106170
Frimmel HE (2018) The gariep belt. In: Siegesmund S, Basei MA, Oyhantçabal P, Oriolo S (eds) Geology of southwest gondwana. Springer, Cham, pp 353–386
Green AN (2009) Sediment dynamics on the narrow, canyon-incised and current-swept shelf of the northern KwaZulu-Natal continental shelf, South Africa. Geo-Mar Lett 29:201–219
Jacob J, Ward JD, Bluck BJ, Scholz RA, Frimmel HE (2006) Some observations on the diamondiferous bedrock gully trapsites on Late Cainozoic, marine-cut platforms of the Sperrgebiet, Namibia. Ore Geol Rev 28:493–506
Jacob J (2016) Contextualized risk mitigation based on geological proxies in alluvial diamond mining using geostatistical techniques. Dissertation, University of the Witwatersrand
Kalbskopf S (1987) Bedrock gullies, their patterns, morphology and relationship to major wave-cut shelves at CDM. CDM, (PTY) LTD. Internal report
Kirkpatrick LH, Green AN (2018) Antecedent geological control on nearshore morphological development: the wave dominated, high sediment supply shoreface of southern Namibia. Mar Geol 403:34–47
Kirkpatrick LH, Green AN, Pether J (2019a) The seismic stratigraphy of the inner shelf of southern Namibia: the development of an unusual nearshore shelf stratigraphy. Mar Geol 408:18–35
Kirkpatrick LH, Jacob J, Green AN (2019b) Beaches and bedrock: how geological framework controls coastal morphology and the relative grade of a Southern Namibian diamond placer deposit. Ore Geol Rev 107:853–862
Liu JP, Milliman JD (2004) Reconsidering melt-water pulses 1A and 1B: global impacts on rapid sea-level rise. Journal of Ocean University of China 3(2):183–190
Miller WR, Ramsay PJ, Leuci R, Bosman C (2000) Geophysical interpretation of the Kerbehuk Inshore Survey Block, Namibia. Council for Geoscience, South Africa (Report No. 2000–0246, 23)
Oelofsen A (2008) Late Cainozoic shallow marine diamond placers off the Northern Sperrgebiet, Namibia. M.Sc Thesis (unpublished), University of Cape Town, 193
Pether J (2013) The Last Transgression Sequence (LTS) and Formation of the Sediment Body, Namdeb Diamond Corporation (Pty) Ltd. Midwater Campaign Internal Report, 13
Pether J (2013) Chameis Geological Observations, Namdeb Midwater Campaign 2013, Namdeb Diamond Corporation (Pty) Ltd. Midwater Campaign Internal Report, 88
Rau G (2003) The integrated use of detailed geophysical, geological and oceanographic techniques to delineate and prioritize marine diamond placer deposits on the inner shelf, west coast, Central Namibia: EPL 1950 (Hottentot Bay) – a case study. Thesis (unpublished), Rhodes University, M.Sc, p 139
Ressler T (1998) WinXAS: A program for X ray absorption spectroscopy data analysis under MS-windows. J Synchrotron Radiat 5:118
Richardson K (2007) A perspective of marine mining within De Beers. The Journal of the Southern African Institute of Mining and Metallurgy 107:393–402
Robert C, Diester-Haass L, Paturel J (2005) Clay mineral assemblages, siliciclastic input and paleoproductivity at ODP Site 1085 off Southwest Africa: a Late Miocene-Early Pliocene history of Orange river discharges and Benguela current activity, and their relation to global sea level change. Mar Geol 216:221–238
Runds MJ, Bordy EM, Pether J (2019) Late Quaternary sedimentological history of a submerged gravel barrier beach complex, southern Namibia. Geo-Mar Lett 39:469–491
Spaggiari RI (2011) Sedimentology of Plio-Pleistocene gravel barrier deposits in the Palaeo-Orange River Mouth, Namibia: depositional history and diamond mineralisation. Dissertation, Rhodes University
Spaggiari RI, Bluck BJ, Ward JD (2006) Characteristics of diamondiferous Plio-Pleistocene littoral deposits within the paleo-Orange River mouth, Namibia. Ore Geol Rev 28:475–492
Stevenson IR, McMillan IK (2004) Incised valley fill stratigraphy of the Upper Cretaceous succession, proximal to the Orange Basin, Atlantic margin of southern Africa. J Geol Soc London 161:185–208
Stevenson IR (1999) The application of high resolution geophysical techniques for seismic stratigraphic analysis at an outcrop scale: a study from the Namaqualand Continental Shelf, west coast, South Africa. Dissertation, University of Reading
Williams R (1996) King of sea diamonds: the saga of Sam Collins. W.J Flesch and Partners (Pty) Ltd, Cape Town
Acknowledgements
The authors would like to thank Namdeb Diamond Corporation (Pty) Limited, specifically C. August for enabling the project which represents the work conducted by the lead author (HF) for her B.Sc. Hons. thesis (Stellenbosch University, 2019). We gratefully acknowledge the assistance from, and fruitful discussions with J. Conradie, J. Jacob, M. Runds and L. Kirkpatrick. We further thank Professor J.A.G. Cooper, one other anonymous reviewer and editor Professor A.N. Green for their valuable comments which helped in strengthening the final submission. Financial support from DSI-NRF CIMERA (BvdH) is also acknowledged and duly appreciated.
Author information
Authors and Affiliations
Corresponding author
Additional information
Publisher’s note
Springer Nature remains neutral with regard to jurisdictional claims in published maps and institutional affiliations.
This article is part of the Topical Collection on Coastal and marine geology in Southern Africa: alluvial to abyssal and everything in between
Rights and permissions
About this article
Cite this article
Fourie, H., von der Heyden, B.P. & Strydom, K. Shelf architecture and recent sediment stratigraphy of the Chameis Bay area, southern Namibia. Geo-Mar Lett 41, 29 (2021). https://doi.org/10.1007/s00367-021-00700-z
Received:
Accepted:
Published:
DOI: https://doi.org/10.1007/s00367-021-00700-z