![]() ![]() This work is part of the GRID3 (Geo-Referenced Infrastructure and Demographic Data for Development) project funded by the Bill and Melinda Gates Foundation (BMGF) and the The Foreign, Commonwealth & Development Office (FCDO) (OPP1182408). Name: grid3/population_gridded Description: These data were produced by the WorldPop Research Group at the University of Southampton. Census disaggregated gridded population estimates for Senegal (2020), version 1.0. H., Abbott T., Boytinck, E., Kuepie, M., Lazar A. Census disaggregated gridded population estimates for Niger (2021), version 1.0. Bottom-up gridded population estimates for Zambia, version 1.0. Zambia: WorldPop (School of Geography and Environmental Science, University of Southampton). South Sudan 2020 gridded population estimates from census projections adjusted for displacement, version 2.0. South Sudan: Dooley CA, Jochem WC, Leasure, DR, Sorichetta A, Lazar AN and Tatem AJ. Bottom-up gridded population estimates for Nigeria, version 2.0. Nigeria: WorldPop and National Population Commission of Nigeria. Census disaggregated gridded population estimates for Mozambique (2017), version 1.1. Mozambique: Bondarenko M, Jones P, Leasure D, Lazar AN, Tatem AJ. Bayesian gridded population estimates for Ghana 2019 (GHA v2.0). WorldPop, University of Southampton, Flowminder Foundation, École de Santé Publique de Kinshasa, Bureau Central du Recensement and Institut National de la Statistique. ![]() ![]() Modelled gridded population estimates for the HautKatanga, Haut-Lomami, Ituri, Kasaï, Kasaï-Oriental, Lomami and Sud-Kivu provinces in the Democratic Republic of the Congo (2021), version 3.0. Democratic Republic of the Congo: G Boo, R Hosner, PZ Akilimali, E Darin, HR Chamberlain, WC Jochem, P Jones, R Shulungu Runika, HM Kazadi Mutombo, AN Lazar and AJ Tatem. Census based gridded population estimates for Burkina Faso (2019), version 1.0. Project partners include WorldPop at the University of Southampton, the United Nations Population Fund (UNFPA), Center for International Earth Science Information Network (CIESIN) in the Earth Institute at Columbia University, and the Flowminder Foundation.īurkina Faso: WorldPop and Institut National de la Statistique et de la Démographie du Burkina Faso. Results from this survey pinpointed the location for PIVA 10.View In: ArcGIS JavaScript ArcGIS Online Map Viewer ArcGIS Earth ArcMap View Footprint In: ArcGIS Online Map Viewer Service Description: These data were produced by the WorldPop Research Group at the University of Southampton. A ground magnetic survey about 20 km east of Pine Valley Homestead was undertaken to accurately locate the magnetic high (Fig. Note: the topographic effects of strandline features are subdued where the Quaternary Lake Bungunnia occurred. This resulted in numerous arcuate features seen throughout the Murray Basin. ( ) The Loxton-Parilla Sands were deposited in strand plain as well as barrier island forming conditions due to fluctuations in sea level and sediment supply. Deposition involved shoreface, beach and dune facies, as well as back barrier lagoon and washover fan deposits (after Roy et al., 1994). Stacking caused the elevation of the barrier island to be greater than strand plain forming barriers. ( ) Stable or rising sea levels led to the formation of stacked barriers. The majority of deposition was in shoreface, beach and dune facies (after Roy et al., 1994). barrier sands ( ) The onset of highstand deposition and sea-level retreat in the Pliocene led to progradation of theLoxton-Parilla Sands and the formation of strand plains. ![]()
0 Comments
Leave a Reply. |
AuthorWrite something about yourself. No need to be fancy, just an overview. ArchivesCategories |