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  • The distribution of Vibrio Parahaemolyticus, yeasts and yeast-like fungi, especially Candida Albicans in various environments of the Great South Bay of Long Island, New York in Pollution and water resources. Pollution, coastal biology and water
  • Agent pathogène ; Candida albicans ; Eau de mer ; Etats-Unis ; Great South Bay ; Géographie humaine ; Littoral ; Long Island ; New York ; Pollution ; Pollution organique ; Variation saisonnière ; Vibrio parahaemolyticus
  • Size variation in the rock hyrax (Procavia capensis) and late Quaternary climatic change in South Africa
  • Archeological site ; Biogeography ; Climatic variation ; Grassland ; Habitat ; Mammal ; Palaeo-ecology ; Palaeoclimatology ; Precipitation ; Quaternary ; South Africa
  • The average adult size of the rock hyrax varies greatly across South Africa. Regression analysis suggests that mean hyrax size is more closely linked to precipitation than to temperature, probably because precipitation has a much greater impact
  • on preferred hyrax food plants. In conjunction with other indicators of past climate, hyrax size variation can be used to reconstruct precipitation history near deeply stratified South African late Quaternary sites, including Elands Bay Cave, Die Kelders Cave 1
  • , and Nelson Bay Cave.
  • The political geography of an exclave : Walvis Bay
  • Afrique du Sud ; Enclave ; Géographie de l'Afrique ; Géographie politique ; Namibie ; Relations internationales ; Walvis Bay
  • An examination of the origins, development and problems of the South African Walvis Bay exclave and its relations with Namibia. - (AJC)
  • Sedimentology, isotopes and palynology of late Holocene cores from Lake Sibaya and the Kosi Bay system (KwaZulu-Natal, South Africa)
  • Coastal plain ; Holocene ; Isotope analysis ; KwaZulu-Natal ; Lacustrine sediment ; Lake ; Palaeo-ecology ; Palaeogeography ; Palynology ; Pollen analysis ; South Africa ; Vegetation dynamics
  • . Sedimentation rates are higher in the dated Sibaya core than the Kosi core. The pollen assemblages reflect changes from greater forest abundances to great savanna grassland abundances. The relative proportion of carbon in the samples decreases during the same
  • Grandiose plans, but insignifiant outcomes : the development of colonial ports at Twofold Bay, New South Wales
  • Australie ; Colonisation ; Géographie historique ; Localisation ; New South Wales ; Port ; Siècle 19 ; Transport
  • Australia ; Colonization ; Harbour ; Historical geography ; Location ; New South Wales ; Nineteenth Century ; Transport
  • The paper examines the period between 1820 and 1920 to explain why the ports of Twofold Bay-Boydtown and Eden never sustained their challenge to Sydney's economic hegemony. These small ports provide an interesting insight into the economic
  • marginalisation of localities by the process of colonisation. Twofold Bay is examined within Rimmer's spatial model of port development. Uneven port development is examined as the geographical expression of several colonisation processes.
  • Windflow modelling in the Saldanha Bay area
  • Coastal environment ; Eolian features ; Model ; South Africa ; Wind
  • Three boundary layer models are applied to a wind energy siting investigation in the Saldanha Bay area. The different models were then tested and results compared. Favourable results were obtained for further development of the models. - (AJC)
  • Strategic territory and territorial strategy: the geopolitics of Walvis Bay's reintegration into Namibia
  • Administration ; Colonisation ; Conflit ; Enclavement ; Géographie politique ; Géopolitique ; Histoire ; Namibie ; Walvis Bay
  • struggle waged by Namibians against South African occupation. The paper charts the history of Walvis Bay's colonization and the conflicting claims of sovereignty. The principal focus is he process of bilateral negotiation and changes to the status following
  • Discussion of the focus and concerns of critical geopolitical analysis, with reference to the contested enclave of Walvis Bay. The eventual reintegration of Walvis Bay into Namibia in 1994 represents the final episode in a long and bitter liberation
  • New constraints on the evolution of Carolina Bays from ground-penetrating radar
  • Aeolian features ; Archaeology ; Bay ; Coastal environment ; Coastal plain ; Dune ; Geophysics ; Holocene ; Humid environment ; Lacustrine sediment ; Sediment transport ; South Carolina ; Stratigraphy ; United States of America
  • Archéologie ; Baie ; Dune ; Eolien ; Etats-Unis ; Géophysique ; Holocène ; Littoral ; Milieu humide ; Plaine côtière ; South Carolina ; Stratigraphie ; Sédiment lacustre ; Transport sédimentaire
  • Ground-penetrating radar (GPR) data for the Savannah River Site (SRS) in the Upper Coastal Plain of South Carolina, combined with geological, archaeological, and ecological data place new constraints on the evolution of Carolina Bays. Extant SRS bay
  • morphology formed mainly during the Holocene and did not involve migration of bays across the landscape. The results are interpreted to develop a model of bay evolution subsequent to the formation of the initial depression.
  • Wave energy and clast transport in eastern Tasman Bay, New Zealand
  • Dynamique littorale ; Gravier ; Littoral ; Nouvelle-Zélande ; Pacifique Sud ; South Island ; Tasman Bay ; Transport sédimentaire ; Vague ; Vent
  • Coastal dynamics ; Coastal environment ; Gravel ; New Zealand ; Sediment transport ; South Island ; South Pacific Ocean ; Wave ; Wind
  • The aim of this paper is to determine whether wave energy in Tasman Bay is sufficient to initiate clast transport along the gravel platforms. In this study, wind data form Nelson airport and measured wave data from Cable Bay and Mackay Bluff
  • are used in conjunction with 2 different mathematical models of clast transport. Values calculated from each of these models are compared with the present wind and wave environment of Tasman Bay. While the mathematical models can only provide approximations
  • because of differences in bathymetry and wave morphology, they will provide a calibrated scale of clast movement along eastern Tasman Bay.
  • Permafrost distribution at Tasiujaq (Leaf Basin) on the south west coast of Ungava Bay, New Québec
  • with foredune formation, Roy with New South Wales estuaries, Marshall and Davies with facies variation in Holocene reef growth, Hopley with the Holocene high energy window on the Great Barrier Reef, Grindrod and Rhodes with Holocene sea level history
  • of Missionary Bay, N. Queensland, Pye and Bowman with episodic dune activity on the East Australian coast, Chappell and Grindrod with chenier plain formation in northern Australia, Thom with sand barriers in eastern Australia, Thompson and Bowman with subaerial
  • denudation and weathering on coastal dunes, Schwebel with Quaternary sea level variation in S.E. South Australia, and Bowden and Colhoun with Quaternary emerged shorelines in Tasmania. (ECFB).
  • Sedimentological consequences of Winter ice cover on a tidal flat environment, Great Bay, New Hampshire
  • 1970-1971 ; Estran ; Etats-Unis ; Glace flottante ; Glaciel ; Great Bay ; Géographie de l'Amérique ; Littoral ; New Hampshire ; Sédimentologie
  • River sediment supply, sedimentation and transport of the highly turbid sediment plume in Malindi Bay, Kenya
  • Bay ; Coastal current ; Coastal environment ; Kenya ; Land use ; Monsoon ; Sediment transport ; Turbidity ; Watershed
  • The current velocities, tidal elevation, salinity and suspended sediment concentrations (TSSC) were measured in stations located within Malindi Bay in the Northern region of the Kenya coast. It is established that Malindi Bay receives a high
  • terrigenous sediment load. The river freshwater supply into the bay is highly variable. Relatively low peak flows occurred in November during the North East Monsoon (NEM). The discharge of highly turbidity river water into the bay in April and May occurs
  • in a period of high intensity South East Monsoon (SEM) winds that generate strong north flowing current that transports the river sediment plume northward. The mechanism of advection of the sediment plume north or south of the estuary is mainly thought
  • to be due to the Ekman transport generated by the onshore monsoon winds. The high sediment discharge into Malindi Bay can be attributed to land use change in the Athi-Sabaki River Basin in addition to rapid population increase which has led to clearance
  • [b1] South Eastern Kenya Univ., School of Water Resources Science and Technology, Dept. of Hydrology and Water Resources Management, Kitui, Kenya
  • Upland and coastal sediment sources in a Chesapeake Bay estuary
  • Bay ; Chesapeake ; Coastal environment ; Coastal erosion ; Environment management ; Estuary ; Fluvial processes ; Human impact ; Maryland ; Palynology ; Resource management ; Sedimentation ; Sedimentology ; Stream ; United States
  • New data from the South River, Maryland and reexamination of existing literature suggest that coastal erosion may be the dominant process driving sediment inputs along the lenght of many tributary estuaries of the Chesapeake. This paper addresses
  • those issues by developing a sediment budget for the upper South River and examining resource management implications of that budget.
  • The impact of tsunami on the coastline of Jervis Bay, southeastern Australia
  • Australie ; Bloc erratique ; Catastrophe ; Datation ; Dynamique littorale ; Falaise ; Géomorphologie littorale ; Littoral ; New South Wales ; Thermoluminescence ; Tsunami
  • Australia ; Catastrophe ; Cliff ; Coastal dynamics ; Coastal environment ; Coastal geomorphology ; Dating ; Erratic boulder ; New South Wales ; Thermoluminescence ; Tsunami
  • The Jervis Bay area offers a diversity of landforms that do not fit within contemporary views of coastal evolution. Field evidence indicates that catastrophic tsunami have had a significant impact on the coast and its hinterland both within
  • Dynamics of deflation hollows in the Elands Bay area, Cape Province, South Africa
  • Observations of erosion and deposition patterns in deflation hollows in the Elands Bay area, show that they are being slowly deepened and elongated in a SSW-NNE direction as a result of sand movements generated by southerly winds. This is probably
  • Variance estimates for a dynamic eutrophication model of Saginaw Bay, Lake Huron
  • Algue ; Amérique du Nord ; Dynamique des populations ; Estimation ; Eutrophisation ; Great Lakes ; Géographie physique ; Huron, lac ; Lac ; Milieu dulçaquatique ; Modélisation ; Plancton ; Saginaw Bay ; Statistique ; Variance ; Variation saisonnière
  • Macro-historical geography and the great chartered companies: the case of the Hudson's Bay Company
  • localized rainfall within the inner core region of intense TCs. Sub-basins with intense TCs that produce extreme rainfall rate maxima include the Bay of Bengal, the South Philippine Sea, the East China Sea, the north coast of Australia, southeast Melanesia
  • . subdivide each major ocean basin, (the North Indian Ocean, the Atlantic Ocean, the Northwest Pacific Ocean, the South Pacific Ocean, the South Indian Ocean, and the East-central Pacific Ocean), into several sub-basins to survey the heterogeneity of extreme
  • , and the Northwest Atlantic. Sub-basins with a higher proportion of category 5 (CAT5) observations than category 3 (CAT3) observations tend to have a greater P25 beyond 60 km from the storm center.
  • La ville nouvelle portuaire de Richards Bay en Afrique du Sud : un destin assujetti à la métropole de Durban
  • Afrique du Sud ; Durban ; Equipement portuaire ; Espace urbain ; KwaZulu Natal ; Port ; Richards Bay ; Trafic portuaire ; Ville
  • Harbour ; Harbour facilities ; Harbour traffic ; South Africa ; Town ; Urban area
  • Les AA. se demandent si les ambitieux projets sur la ville nouvelle de Richards Bay, suppléer le port de Burban et équilibrer l'armature urbaine provinciale, ont été réalisés. En rappelant l'historique de ces deux villes portuaires et en décrivant
  • leurs paysages contemporains, les AA. montrent à quel point les objectifs initiaux ont quelque peu été surestimés. Cependant Richards Bay, par ses atouts présents et surtout futurs doit être gratifiée d'un relatif succès.