Baía dos Tigres - The dynamic of the process

Authors

DOI:

https://doi.org/10.14295/bjs.v3i6.554

Keywords:

restinga, tiger bay, spawning, fishing

Abstract

Baía dos Tigres is a well-known sandbank in Angola, referred to since the 15th century when the Portuguese navigators passed there in 1488, on the voyage that allowed them to round the Cape of Good Hope, in southern Africa. It is a phenomenon of a sedimentary nature and therefore it is linked to the availability of solid flow carried by the drift current coming from the South. However, several changes in its condition have been recorded over the centuries. It has shifted from being a sandbank (restinga) and an island, this latter occurring when the isthmus that connects it to the mainland broke, becoming a restinga again when it reestablisheb itself. In March 1962, a huge storm at sea destroyed the fragile structure connecting the land to the coast and since then, precisely 60 years ago, Baía dos Tigres became an island, being separated from the coast in a way that seemed definitive. The observation and analysis of the satellite images used in this work seem to suggest that a setback is beginning to appear, since Baía dos Tigres may be starting to reconnect to the mainland. If this occurs, there is the possibility for Angola to have again a true fish hatchery where countless varieties of fishes and molluscs find unique conditions for spawning. Those partially closed conditions, with waters sufficiently oxygenated to generate excellent biological environment for spawning, are of great importance for the future of fish industry in the country. If those conditions are restored, the zone will be protected from the direct action of storms and the speed of currents, covering an area of more than 250 km2. This article makes an up-date of the situation, based on the analysis of satellite images currently available.

References

Bellin, J. N. (1754). Carte Réduite Des Costes Occidentales d’Afrique. Departement de la Marine, Paris.

Dyer, K. R., & Huntley, D. A. (1999). The Origin, Classification and Modelling of Sandbanks and Ridges. Continental Shelf Research, 19(10), 1285-1330. https://doi.org/10.1016/S0278-4343(99)00028-X DOI: https://doi.org/10.1016/S0278-4343(99)00028-X

Garzanti, E., Vermeesch, P., Andò, S., Lustrino, M., Padoan, M., & Vezzoli, G. (2014). Ultra-long distance littoral transport of orange sand and provenance of the Skeleton Coast Erg (Namibia). Marine Geology, 357, 25-36. https://doi.org/10.1016/j.margeo.2014.07.005 DOI: https://doi.org/10.1016/j.margeo.2014.07.005

General Bathymetric, Chart of the Oceans. (2024). Overview. In: What we do. Available in: https://www.gebco.net/about_us/overview/ Access in 05/12/2024.

Giresse, P., Hoang, C-T., & Kouyoumontzakis, G. (1984). Analysis of vertical movements deduced from a geochronological study of marine Pleistocene deposits, southern coast of Angola. Journal of African Earth Sciences, 2(2), 177-187. https://doi.org/10.1016/S0731-7247(84)80012-9 DOI: https://doi.org/10.1016/S0731-7247(84)80012-9

Guilcher, A., Medeiros, C. A., Esteves de Matos, J., Tomás de Oliveira., J., (1974). Les restingas (Flèches Littorales) d’Angola spécialement celles du Sud et du Centre. Finisterra, 9(18), 173-211. DOI: https://doi.org/10.18055/Finis2357

Goscombe, B., Hand, M., Gray, D., & Mawby, J. (2003). The methamorfic arquitecture of a transpressional orogen: the Kaoko Belt, Namibia. Journal of Petrology, 44(4), 679-711. https://doi.org/10.1093/petrology/44.4.679 DOI: https://doi.org/10.1093/petrology/44.4.679

Guilcher, A. (1954). Dynamique et morphologie des côtes sableuses de l'Afrique Atlantique. In: Cahiers de l'Information Géographique, Paris, France.

Jessen, O. (1951). Dünung im Atlantik und an der Westküste Afrikaas. Sonderabdruck aus Petermanns Geographische Mitteilungen, Frankfurt, 1.

Mendelsohn, J. S. (2018). Sudoeste de Angola, um retrato da terra e da vida. Ed. Printer Portuguesa, Raison, Universidade do Porto, Portugal.

Nascimento, D. B. (2012). Estratigrafia da sequência Damara, Neoproterozóico, em Damaraland, Namíbia. Dissertação de Mestrado em Geologia pela Universidade Federal do Rio de Janeiro, Brasil, 117 p.

Pereira, D. P. (1505). Esmeraldo de Situ Orbis. In: Grande Enciclopédia Portuguesa-Brasileira, Editorial Enciclopédia, Lisboa-Rio de Janeiro, 1935-1957 p.

Ribas, F., Flques, A., Van den Berg, N., & Caballeria, M. (2013). Modeling shoreline sand waves on the coasts of Namibia and Angola. International Journal of Sediment Research, 28(3), 338-348. https://doi.org/10.1016/S1001-6279(13)60044-X DOI: https://doi.org/10.1016/S1001-6279(13)60044-X

Tábua de Marés. (2024). Tábua de Marés e Solunares. Available in: https://tabuademares.com/af/angola/tombua Access in: 05/12/2024.

Zenkovich, V. P. (1967). Processes of coastal development. Oliver and Boyd, Edimburgh and London.

Downloads

Published

2024-05-13

How to Cite

Costa, C. B. da, Fonte, C., Santos, C. V.-D., & Teixeira-Pinto, A. (2024). Baía dos Tigres - The dynamic of the process. Brazilian Journal of Science, 3(6), 39–53. https://doi.org/10.14295/bjs.v3i6.554

Issue

Section

Environmental Sciences