Academic literature on the topic 'Dunefield'

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Journal articles on the topic "Dunefield"

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Yang, LinHai, Tao Wang, Jie Zhou, ZhongPing Lai, and Hao Long. "OSL chronology and possible forcing mechanisms of dune evolution in the Horqin dunefield in northern China since the Last Glacial Maximum." Quaternary Research 78, no. 2 (2012): 185–96. http://dx.doi.org/10.1016/j.yqres.2012.05.002.

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AbstractThe evolution processes and forcing mechanisms of the Horqin dunefield in northern China are poorly understood. In this study, systematic OSL dating of multiple sites is used together with pollen analysis of a representative section in order to reconstruct the evolution of the dunefield since the Last Glacial Maximum (LGM). Our results show that there was extensive dune mobilization 25–10 ka, transition to stabilization 10–8 ka, considerable dune stabilization 8–3 ka, and multiple episodes of stabilization and mobilization after 3 ka. Comparison of dune evolution of the dunefields in n
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TOMAZELLI, LUIZ JOSÉ, SÉRGIO REBELLO DILLENBURG, EDUARDO GUIMARÃES BARBOZA, and MARIA LUIZA CORREA DA CAMARA ROSA. "Geomorfologia e Potencial de Preservação dos Campos de Dunas Transgressivos de Cidreira e Itapeva, Litoral Norte do Rio Grande do Sul, Brasil." Pesquisas em Geociências 35, no. 2 (2008): 47. http://dx.doi.org/10.22456/1807-9806.17936.

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The association of several favorable factors (high supply of fine sand to the beach, appropriate wind regime, lowland topography) has resulted in the development of a wide transgressive dunefield that stands out as a fundamental element in the coastal landscape of Rio Grande do Sul, southern Brazil. Along the northern littoral of the state, most of this original ecosystem has been destroyed or highly modified in the last decades, mainly due to the intense urbanization that has been settled in the area. However, some remaining segments of the original eolian field can still be found and, due to
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Hesp, Patrick A., Sergio R. Dillenburg, Eduardo G. Barboza, et al. "Beach ridges, foredunes or transgressive dunefields? Definitions and an examination of the Torres to Tramandaí barrier system, Southern Brazil." Anais da Academia Brasileira de Ciências 77, no. 3 (2005): 493–508. http://dx.doi.org/10.1590/s0001-37652005000300010.

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Many prograded barriers and some dunefields in theworld have been termed 'beach ridge' plains, but the actual genesis of the 'ridges' is often unknown. Use of the terms, berms, beach ridges and foredunes is also confusing in the literature because their definitions are highly variable and are commonly used interchangeably. Thus, the formation and definition of sand berms, beach ridges and foredunes is briefly reviewed. Beach ridges are re-defined as entirely wave formed deposits which are most commonly formed during high wave conditions and/or elevated water levels (e.g. storm surges). Foredun
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Buckley, R. C., W. Chen, Y. Liu, and Z. Zhu. "Characteristics of the Tengger dunefield, north-central China, and comparison with the central Australian dunefields." Journal of Arid Environments 10, no. 2 (1986): 97–101. http://dx.doi.org/10.1016/s0140-1963(18)31250-3.

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MARTINHO, CAROLINE T., and PAULO C. F. GIANNINI. "Morphology of the Ibiraqüera dunefield, SC." Anais da Academia Brasileira de Ciências 74, no. 3 (2002): 545. http://dx.doi.org/10.1590/s0001-37652002000300026.

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Worman, F. Scott, Alexander Kurota, and Patrick Hogan. "Dunefield geoarchaeology at White Sands National Monument, New Mexico, USA: Site formation, resource use, and dunefield dynamics." Geoarchaeology 34, no. 1 (2018): 42–61. http://dx.doi.org/10.1002/gea.21710.

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Enright, N. J., and M. J. Anderson. "Recent evolution of the Mangawhai Spit dunefield." Journal of the Royal Society of New Zealand 18, no. 4 (1988): 359–67. http://dx.doi.org/10.1080/03036758.1988.10426462.

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Pell, S. D., A. R. Chivas, and I. S. Williams. "The Mallee Dunefield: development and sand provenance." Journal of Arid Environments 48, no. 2 (2001): 149–70. http://dx.doi.org/10.1006/jare.2000.0751.

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Stewart, Brian. "Charring patterns on reconstructed ceramics from Dunefield Midden." Before Farming 2005, no. 1 (2005): 1–18. http://dx.doi.org/10.3828/bfarm.2005.1.1.

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Buckley, Ralf, Andrew Gubb, and Robert Wasson. "Parallel dunefield ecosystems: predicted soil nitrogen gradient tested." Journal of Arid Environments 12, no. 2 (1987): 105–10. http://dx.doi.org/10.1016/s0140-1963(18)31180-7.

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Dissertations / Theses on the topic "Dunefield"

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Reeler, Claire. "Spatial patterns and behaviour at Dunefield Midden." Master's thesis, University of Cape Town, 1992. http://hdl.handle.net/11427/21975.

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An analysis of the spatial patterning present in the arrangement of material and features at the site of Dunefield Midden, is presented in this thesis. All items from the site are analysed, except the remains of large fauna. The site of Dunefield Midden is situated about two kilometres north of Eland's Bay on the Cape West coast, South Africa. Radiocarbon dates indicate that the site was occupied about 670 years B.P. The nature of the food remains and artefacts from this site suggests a single occupation, for a limited period, by a group of hunter-gatherers. Features from the site examined in
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McConnachie, Lauren Bernyse. "Morphology, patterns and processes in the Oyster Bay headland bypass dunefield, South Africa." Thesis, Rhodes University, 2013. http://hdl.handle.net/10962/d1001904.

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Studies of the dunefield systems crossing the Cape St. Francis headland in the Eastern Cape have focused on the role that wind plays in sediment transfer in coastal dunefield systems, with limited consideration of the role of water. The aim of this study was to improve understanding of the morphology, processes and patterns within the Oyster Bay HBD system, focussing particularly on surface water and groundwater interactions and the role of surface water in sediment transfer across the dunefield system. An extensive field survey was conducted, to collect related data, complimented by spatial a
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Elkington, Lauren. "Morphology, patterns and processes in the Oyster Bay headland bypass dunefield, South Africa." Thesis, Rhodes University, 2013. http://hdl.handle.net/10962/5879.

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Studies of the dunefield systems crossing the Cape St. Francis headland in the Eastern Cape have focused on the role that wind plays in sediment transfer in coastal dunefield systems, with limited consideration of the role of water. The aim of this study was to improve understanding of the morphology, processes and patterns within the Oyster Bay HBD system, focussing particularly on surface water and groundwater interactions and the role of surface water in sediment transfer across the dunefield system. An extensive field survey was conducted, to collect related data, complimented by spatial a
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Tonner, Tobias W. W. "A spatial database for the Later Stone Age site 'Dunefield Midden', (Western Cape, South Africa)." Master's thesis, University of Cape Town, 2003. http://hdl.handle.net/11427/4183.

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Portela, Samuel Victor da Silva. "Relation Society and Environmental Protection: Study in the Surrounding Area of Environmental Protection Dunefield Paracuru - EC." Universidade Federal do CearÃ, 2009. http://www.teses.ufc.br/tde_busca/arquivo.php?codArquivo=9219.

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Conselho Nacional de Desenvolvimento CientÃfico e TecnolÃgico<br>The Environmental Protection Area (APA) of the Field of Dunes is the largest Conservation Unit (UC) of the City of Paracuru. Comprising for 3909.60 hectares the APA has the environmental characteristics of the dunes that make up an ecosystem of ecological balance naturally fragile and in constant state of risk in relation to human intervention, but with a great ecological value and tourism. This area has a fundamental importance for the city, it is situated near the center of the municipal office and is in the process of increasi
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Leoncini, Carlotta. "Stratigraphic study and analysis of the barchan dunefield of the Laguna coastal zone in Santa Catarina, Brazil." Bachelor's thesis, Alma Mater Studiorum - Università di Bologna, 2014. http://amslaurea.unibo.it/7948/.

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The association of several favorable factors has resulted in the development of a wide barchan dune field that stands out as a fundamental element in the coastal landscape of southern Santa Catarina state in Brazil. This original ecosystem is being destroyed and highly modified, due to urbanization. This work identifies and discusses its basic characteristics and analyzes the favorable factors for its preservation, in the foreseen of both a sustainable future and potential incomes from ecotourism. The knowledge of the geologic evolution allows to associate this transgressive Holocene dunes for
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Knight, Melanie. "Climate change in the 21st Century and the impact on continental dunefield activity : an example from the Mega-Kalahari in southern Africa." Thesis, University of Sheffield, 2003. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.401175.

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Rodrigues, Fernanda Costa Gonçalves. "Evolução dos sistemas eólicos costeiros quaternários entre Campo Bom e a foz do Rio Araranguá, SC." Universidade de São Paulo, 2017. http://www.teses.usp.br/teses/disponiveis/44/44141/tde-22082017-085425/.

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O sistema eólico quaternário do litoral sul de Santa Catarina foi dividido em inativo e ativo. O sistema inativo é composto por depósitos eólicos indiferenciados (DEI), lençol de areia e campo de dunas. O sistema ativo possui três associações de feições morfológicas: praia-duna, planície deflacionária e campo de dunas livres. Os DEI ocorrem preferencialmente associados a interflúvios alongados segundo a direção SW-NE. Formam o substrato dos demais depósitos eólicos e apresentam idades mínimas de luminescência opticamente estimulada (LOE) entre 625 ka e 134 ka. O lençol de areia corresponde a t
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Ara?jo, Ver?nica Dantas de. "Caracteriza??o geol?gica tridimensional e monitoramento de dunas no litoral oriental do Rio Grande do Norte." Universidade Federal do Rio Grande do Norte, 2006. http://repositorio.ufrn.br:8080/jspui/handle/123456789/18843.

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Made available in DSpace on 2015-03-13T17:08:40Z (GMT). No. of bitstreams: 1 VeronicaDA.pdf: 5709097 bytes, checksum: 4074580aee5ec2b7d354ddab1d446e43 (MD5) Previous issue date: 2006-05-19<br>This work presents geophysical and geological results obtained in a dunefield located in the east coast of Rio Grande do Norte State, with the aim to recognize the aeolian body depositional geometries to a future geologic modeling of the aeolian petroliferous reservoirs. The research, which was done in blowouts region situated at Nisia Floresta Municipally, included the characterization of external geom
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Guedes, Carlos Conforti Ferreira. "Cronologia e sedimentologia dos depósitos eólicos quaternários da Costa Leste maranhense." Universidade de São Paulo, 2012. http://www.teses.usp.br/teses/disponiveis/44/44141/tde-17072013-161939/.

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Idades por luminescência opticamente estimulada foram obtidas nos depósitos eólicos do litoral leste maranhense. As datações permitiram reconhecer ao menos quatro gerações de dunas eólicas, incluindo a atual. As duas gerações mais antigas (G1/G0: idades LOE de 258,9±24,6 a 88,0±8,6 ka A.P.) não são distinguíveis por critérios de campo, somente por dados geocronológicos. A geração eólica 2 corresponde a feições eólicas estabilizadas pela vegetação que ocorrem a até 135 km da linha de costa atual. As idades LOE-SAR de estabilização obtidas para essas feições eólicas compreendem um int
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Books on the topic "Dunefield"

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K, Illenberger W., Kerley G. I. H, McGwynne Lesley, University of Port Elizabeth. Institute for Coastal Research., and Cape of Good Hope (South Africa). Cape Nature Conservation., eds. Management and conservation of the Alexandria coastal dunefield: Proceedings of a workshop held by the Institute for Coastal Research and Cape Nature Conservation at the Sundays River Mouth Research Station on 9 June 1993. Institute for Coastal Research, University of Port Elizabeth, 1993.

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Allen, Nicholas, Nick Groom, and Jos Smith. Introduction. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780198795155.003.0001.

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In 1967, Benoît Mandelbrot suggested a mathematical conundrum that involved answering the seemingly straightforward question, ‘How long is the coast of Britain?’1 The answer is surprisingly elusive and dependent on the scale at which one is looking. Increasing the scale unearths greater detail, time and time again, and so the answer grows the closer one looks. The problem is that any measure, at however small a scale, is forced to simplify complex ambiguities that might otherwise reveal further intricacies of their own. This was an entry-point to Mandlebrot’s writings on fractal geometry, but
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Book chapters on the topic "Dunefield"

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Lancaster, Nicholas. "Dunefields of the Southwest Deserts." In Dunes of the World. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-40498-7_9.

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Pye, Kenneth, and Haim Tsoar. "The formation of sand seas and dunefields." In Aeolian sand and sand dunes. Springer Netherlands, 1990. http://dx.doi.org/10.1007/978-94-011-5986-9_5.

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Hesp, Patrick A., and Michael J. Hilton. "Restoration of Foredunes and Transgressive Dunefields: Case Studies from New Zealand." In Restoration of Coastal Dunes. Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-33445-0_5.

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"Lesser dunefields of Arabia." In Arabian Deserts. Springer Netherlands, 2006. http://dx.doi.org/10.1007/1-4020-3970-0_8.

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Lancaster, Nicholas. "Sand Seas and Dunefields." In Reference Module in Earth Systems and Environmental Sciences. Elsevier, 2021. http://dx.doi.org/10.1016/b978-0-12-818234-5.00127-9.

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Conference papers on the topic "Dunefield"

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Valdemoro, Herminia I., José A. Jiménez, Ignacio Alonso, Paloma Lorente, and Manuel Rodríguez-Herrerías. "Coastal Dunefield Evolution in Conditions of Limited Sediment Availability: Natural and Anthropogenic Controls on the Corralejo Dunes." In Sixth International Symposium on Coastal Engineering and Science of Coastal Sediment Process. American Society of Civil Engineers, 2007. http://dx.doi.org/10.1061/40926(239)99.

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Ellerton, Daniel, James Shulmeister, Tammy M. Rittenour, et al. "OSL AGES AND FORMATION MECHANISMS OF A MAJOR COASTAL DUNEFIELD, THE COOLOOLA SAND MASS, SOUTHEASTERN QUEENSLAND, AUSTRALIA." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-299369.

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WERNER PINTO, MAIARA, RICARDO MEIRELES, ANDREW COOPER, and ANTONIO HENRIQUE DA FONTOURA KLEIN. "SANTINHO/INGLESES TRANSGRESSIVE DUNEFIELD SYSTEM — SANTA CATARINA ISLAND (BRAZIL): TEMPORAL VARIABILITY IN VEGETATION, MANMADE STRUCTURES AND DUNE MIGRATION." In Coastal Sediments 2015. WORLD SCIENTIFIC, 2015. http://dx.doi.org/10.1142/9789814689977_0085.

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Araujo, V. D., Y. A. Reyes-Pérez, R. C. Freire, et al. "Monitoring methods of dunefield susceptible to human activities in the Nísia Floresta area, eastern coast of the State of Rio Grande do Norte, Brazil." In COASTAL ENVIRONMENT 2006. WIT Press, 2006. http://dx.doi.org/10.2495/cenv060371.

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DA SILVA, GRAZIELA MIOT, and PATRICK HESP. "DEVELOPMENT OF COASTAL HOLOCENE TRANSGRESSIVE DUNEFIELDS: EXAMPLES FROM SOUTH AUSTRALIA." In International Conference on Coastal Sediments 2019. WORLD SCIENTIFIC, 2019. http://dx.doi.org/10.1142/9789811204487_0107.

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Shulmeister, James, Daniel Ellerton, Kevin Welsh, et al. "THE SANDS OF TIME. MAPPING FRASER ISLAND; ONE OF THE OLDEST COASTAL DUNEFIELDS IN THE WORLD." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-298833.

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