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  • 1
    Publication Date: 2021-05-19
    Description: During the Quaternary the volume of the world’s oceans fluctuated, with sea level falls as the water has been incorporated into polar and high latitude ice sheets, and sea level rise as these have subsequently melted. Sea-level lowstands were therefore related to the Pleistocene glaciations, while high-stands correlate with interglacials. In general the climate variations in Africa shows a simple relation: Cold or cool climates are associated with dry episodes and warm climates are associated with wet episodes. This applies to the major Milankovich driven glacials and interglacials, as well as to short-lived intervals related to sun spot activities. The reconstruction of palaeoshorelines in the Maputo Bay, and the climate around the Maputo Bay is based on bathymetric maps. At about 18,000 yr BP (-130 meters sea level) the Maputo Bay was located in an inland position. As the sea level rose to about 20 m below present around 9000 - 10000 years BP, a barrier island complex developed in the northern coast, which is well defined by 20 m contour palaeoshoreline. The Maputo Bay is only formed around 8000 – 9000 years BP (when the sea level was 10 to 12 m below the present, and it was a long lasting still stand sea level. A huge island was protecting the bay from the sea. Tidal inlet and its associated ebb delta were separating the island from the peninsula in the south and were connecting the lagoon into the sea. The complete picture of Maputo Bay patterns with its modern sedimentary environments including Inhaca Island may have evolved when the sea level has stood close to its present level around 7000 – 5000 years BP, after which the Maputo Bay became more or less stable. Coral reefs may have also developed during this period. Submarine modifications of the topography during and after the sea-level rise make it difficult to make safe interpretations of the coastal palaeomorphology. However, we believe that many of the present major submarine bottom forms, which are seen on the maps today, are related to coastal processes during the sea-level rise, and were preserved when they were flooded during the Holocene transgression.
    Keywords: Geology
    Repository Name: AquaDocs
    Type: Preprint
    Format: 266193 bytes
    Format: application/pdf
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  • 2
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    Geological Society of America
    Publication Date: 2021-05-19
    Description: The coastal region of Maputaland-Mozambique is characterised by an extensive lowlying coastal plain, which rises to a height of more than 100 metres in some places and attain a width of 2 kilometres. Maputaland in Mozambique extends from Ponta de Ouro, which borders South Africa to Cabo Santa Maria stretching for a distance over 100 kilometres, and encloses several swamps and coastal lakes such as Satine, Piti, Munde and Nela running in north south direction. The main objective of this study was to access the different categories of dune morphology in Maputaland- Mozambique by using aerial photographs, satellite images and field checking. Two major distinct dune systems on the Maputaland coastal morphology were mapped: (1) vegetated dunes form a coastal dune system, which face the sea, and characterised by undulating surfaces and continuous irregular crests running in north-south direction. Transfer dunes move along the foot of slope of the vegetated dunes towards north and northeast. The recent dunes can be either mobile or partial mobile and can attain a height of 5 meters. (2) Inland dunes system comprises a series of dunes including the reworked, parabolic and climbing dunes. These series of dunes often truncate on the first coastal dune system indicating different spatial and temporal events of dune formation. Weathering and reworking processes have affected these dunes, altering their typical shape and smoothing their surface giving them a hummocky aspect. The climbing dunes, running east west in most cases, separate the coastal lakes, and seem to be a result of fragmentation of previous existed large coastal lagoon by the several blowouts events as the lagoon water level fell down. These blowouts seem to follow the uppermost paleo-topographical areas of the lagoon, and the superimposed climbing dunes suggest high rates of sediment transport and deposition. The fragmentations of coastal lagoons by blowouts, which are superimposed by climbing dunes, are common modern processes along Mozambique Coastal Plain (e.g. Umbedje Lagoon in Bilene Holiday Resort located about 100 km north of Maputo).
    Description: Published
    Keywords: Coastal dunes
    Repository Name: AquaDocs
    Type: Proceedings Paper , Non-Refereed
    Format: 1332814 bytes
    Format: application/pdf
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