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Artykuły w czasopismach na temat „Geomorphology South Australia”

Autor: Grafiati
Data publikacji: 4 czerwca 2021
Data aktualizacji: 1 lutego 2022

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Sprawdź 24 najlepszych artykułów w czasopismach naukowych na temat „Geomorphology South Australia”.

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1

Tooth, Stephen, and Gerald C. Nanson. "The geomorphology of Australia's fluvial systems: retrospect, perspect and prospect." Progress in Physical Geography: Earth and Environment 19, no. 1 (March 1995): 35–60. http://dx.doi.org/10.1177/030913339501900103.

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This article provides a review of the study and geomorphology of Australia's fluvial systems by offering comment on the development, concerns and future of the subject. Trends in the history of fluvial landform studies in Australia are traced from the observations and comments of the early explorers and visiting scientists through to the emergence and growth of fluvial geomorphology as a study discipline. Subsequent development of the idea of a distinctive geomorphology of Australian fluvial systems that often contrast with Anglo-American observations is outlined and illustrated with particula
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2

Wakelin-King, Gresley. "Using geomorphology to assess contour furrowing in western New South Wales, Australia." Rangeland Journal 33, no. 2 (2011): 153. http://dx.doi.org/10.1071/rj10080.

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This study examines landscape rehabilitation treatments installed 20–40 years ago in the Western Catchment of NSW. Treatment outcomes were assessed using geomorphic criteria, because geomorphic processes are fundamental to ecological permanence. Contour furrowing creates artificial runoff-runon sets which intercept runoff (resistance to flow by windrows microrelief and surface roughness) and promote infiltration (artificial permeability by ripping). As originally conceived, after windrows subside, flow resistance would be afforded by surface roughness under belts of vegetation. This study show
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3

Twidale, C. Rowland. "Paul S. Hossfeld and His Contribution to Geomorphology." Historical Records of Australian Science 23, no. 2 (2012): 132. http://dx.doi.org/10.1071/hr12006.

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The received wisdom was and is that landscapes cannot be more than a few millions of years old. Nevertheless, consideration of local geology and age of sediments in adjacent basins convinced Paul S. Hossfeld that the summit surface of low relief preserved on the northern Mount Lofty Ranges of South Australia resulted from long-continued planation and that it is of Cretaceous age; that is, some 70 million years old. Hossfeld's apparently intuitive suggestion that very old landscapes exist, recorded in his graduate thesis but not further pursued by him, is the earliest known statement of this id
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Shulmeister, James, Justine Kemp, Kathryn E. Fitzsimmons, and Allen Gontz. "Constant wind regimes during the Last Glacial Maximum and early Holocene: evidence from Little Llangothlin Lagoon, New England Tablelands, eastern Australia." Climate of the Past 12, no. 7 (July 5, 2016): 1435–44. http://dx.doi.org/10.5194/cp-12-1435-2016.

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Abstract. Here we present the results of a multi-proxy investigation – integrating geomorphology, ground-penetrating radar, and luminescence dating – of a high-elevation lunette and beach berm in northern New South Wales, eastern Australia. The lunette occurs on the eastern shore of Little Llangothlin Lagoon and provides evidence for a lake high stand combined with persistent westerly winds at the Last Glacial Maximum (LGM – centring on 21.5 ka) and during the early Holocene (ca. 9 and 6 ka). The reconstructed atmospheric circulation is similar to the present-day conditions, and we infer no si
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5

Peacock, David, Gresley A. Wakelin-King, and Ben Shepherd. "Cane toads (Rhinella marina) in south-western Queensland: invasion front, spread and how Cooper Creek geomorphology could enable invasion into north-eastern South Australia." Australian Journal of Zoology 62, no. 5 (2014): 366. http://dx.doi.org/10.1071/zo14025.

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The invasion of northern Australia by the poisonous cane toad is well recognised, as is its devastating impacts on numerous local native species. However, there is little recognition that the toads are spreading into south-western Queensland. Utilising local knowledge, a limited survey was undertaken within the Cooper Creek catchment to locate the invasion front. Dispersal during 2010–11 floods has established cane toads as far south as Jundah. Integrating this information with landform mapping indicates that cane toad invasion can continue south-west down the Cooper Creek. Though arid, Cooper
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6

Wheeler, M. A., and M. Byrne. "Congruence between phylogeographic patterns in cpDNA variation in Eucalyptus marginata (Myrtaceae) and geomorphology of the Darling Plateau, south-west of Western Australia." Australian Journal of Botany 54, no. 1 (2006): 17. http://dx.doi.org/10.1071/bt05086.

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Phylogeographic patterns in the cp genome of Eucalyptus marginata Don ex Sm., a species common in the mesic region of south-western Australia, were investigated by using RFLP analysis. The chloroplast diversity was structured into two geographically distinct lineages and nested clade analysis inferred historical fragmentation as the major influence on the phylogeographic pattern. The lineages were separated along the geomorphological boundary of the Darling Scarp, which separates the Coastal Plain from the Darling Plateau. The divergence between the lineages is consistent with uplifting of the
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7

Boon, Paul I. "Are mangroves in Victoria (south-eastern Australia) already responding to climate change?" Marine and Freshwater Research 68, no. 12 (2017): 2366. http://dx.doi.org/10.1071/mf17015.

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The distribution and productivity of mangroves is directly affected by a wide range of climatic drivers, including temperature, frost, rainfall, evaporation and storm activity, which, in turn, influence a suite of secondary drivers, including changes in freshwater run-off and sediment supply, groundwater dynamics and inter-species competitiveness. The highest-latitude expression of mangroves globally is at Millers Landing, Victoria (38°45′S), and because the vigour and productivity of mangroves across much of Victoria is thought to be limited by low winter temperatures and the incidence and se
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8

Timms, Brian V., and Caleb Rankin. "The geomorphology of gnammas (weathering pits) of northwestern Eyre Peninsula, South Australia: typology, influence of haloclasty and origins." Transactions of the Royal Society of South Australia 140, no. 1 (December 14, 2015): 28–45. http://dx.doi.org/10.1080/03721426.2015.1115459.

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9

Murphy, Brian, and David Duncan. "Interaction of time sequences and geomorphology in the soils of the Lower Macquarie River plain in south eastern Australia." Quaternary International 365 (April 2015): 60–73. http://dx.doi.org/10.1016/j.quaint.2015.01.044.

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10

Holdaway, SJ, PC Fanning, and DC Witter. "Prehistoric aboriginal occupation of the rangelands: Interpreting the surface archaeological record of far western New South Wales, Australia." Rangeland Journal 22, no. 1 (2000): 44. http://dx.doi.org/10.1071/rj0000044.

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Recent erosion in arid regions of western NSW has exposed large areas that are scattered with stone artefacts manufactured by Aboriginal people in prehistory. These exposures offer an opportunity for archaeologists to study the artefacts abandoned by Aboriginal people through time and to compare those artefacts that accumulate in different parts of the landscape. To reconstruct the nature of prehistoric behaviour in the rangelands, two approaches are needed. First, the geomorphological context of the artefacts needs to be considered since exposure of the artefacts is a function of landscape hi
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11

Brainwood, M., Shelley Burgin, and M. Byrne. "The role of geomorphology in substratum patch selection by freshwater mussels in the Hawkesbury-Nepean River (New South Wales) Australia." Aquatic Conservation: Marine and Freshwater Ecosystems 18, no. 7 (November 2008): 1285–301. http://dx.doi.org/10.1002/aqc.949.

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12

W. Wardell-Johnson, Grant, Ben E. Lawson, and Robert H. Coutts. "Are regional ecosystems compatible with floristic heterogeneity? A case study from Toohey Forest, south-east Queensland, Australia." Pacific Conservation Biology 13, no. 1 (2007): 47. http://dx.doi.org/10.1071/pc070047.

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The recognition and effective portrayal of floristic heterogeneity is a complex issue for land classification. This study in Toohey Forest, south-east Queensland, examines the effects of mapping scale and environmental variables on a floristically heterogeneous area. Current Version 4.1 regional ecosystem mapping at 1: 1 00 000 scale maps Toohey Forest as a single regional ecosystem unit "12.11.5", described as an "open forest complex with Corymbia citriodora, Eucalyptus siderophloia, E. major on metamorphics ± interbedded volcanics". Plant taxa data from 50, 20 x 20 m sites comprising 247 nat
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13

Mayer, Wolf. "William Noel Benson (1885-1957): Insights into the Life and Work of an Eminent Geologist." Earth Sciences History 32, no. 1 (January 1, 2013): 55–85. http://dx.doi.org/10.17704/eshi.32.1.787u2x34ln22hg31.

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William Noel Benson was one of the most renowned geologists in Australia and New Zealand during the first half of the twentieth century. He studied geology at the Universities of Sydney and Cambridge and occupied the Chair of Geology at the University of Otago with great distinction for thirty-three years. His research work extended across the greater part of the geological spectrum and gained him world-wide recognition and a reputation as a scholar in the classical mode. His name is today most closely associated with his pioneering work on the composition, origin and tectonic setting of the m
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14

TIMMS, Brian, and Jane COOPER. "Seagull Lake, Western Eyre Peninsula, South Australia: A Saline Lake to Benefit from Climate Change? I. Geomorphology, Invertebrates, Birds and the Future." Acta Geologica Sinica - English Edition 88, s1 (December 2014): 101–2. http://dx.doi.org/10.1111/1755-6724.12266_23.

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15

Fitzsimons, Sean J., and Eric A. Colhoun. "Pleistocene glaciation of the King Valley, Western Tasmania, Australia." Quaternary Research 36, no. 2 (September 1991): 135–56. http://dx.doi.org/10.1016/0033-5894(91)90022-w.

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AbstractAnalysis of the geomorphology, geology, and palynology of deposits in the King Valley permits the identification of four glaciations and two interglaciations and has led to a revision of the Pleistocene stratigraphy of the West Coast Range. The oldest late-Cenozoic deposits in the valley appear to predate glaciation, contain extinct pollen types, and are probably of late-Tertiary age. Overlying deposits of the Linda Glaciation show intense chemical weathering and have a reversed detrital remanent magnetization indicating deposition before 730,000 yr B.P. The highly weathered tills are
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16

Smith, Cathy. "Tin City: Nomadic occupation, colonization and resistance in the sand dunes of Stockton Bight, Australia." Design Ecologies 9, no. 1 (June 1, 2020): 93–109. http://dx.doi.org/10.1386/des_00006_1.

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This article explores nomadic site occupation as a form of planetary colonization involving both human and non-human agents. Conventional understandings of temporary occupation are often humancentric with little attention paid to the disruption of extant site ecologies and processes. The latter are particularly pressing concerns in nomadic settlements located in precarious landscapes. Taking the latter as its focus, this article engages the earth as an agent resisting its own colonization in the Australian-licensed squatter settlement known colloquially as Tin City. Located within the largest
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17

Vyšná, V., F. Dyer, W. Maher, and R. Norris. "Organic carbon reservoirs in five small rivers across a land-use gradient." Marine and Freshwater Research 66, no. 3 (2015): 233. http://dx.doi.org/10.1071/mf13142.

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Organic carbon (OC) inputs, stores and processing underpin river functioning. We examined patterns in OC reservoirs (total organic carbon, TOC), suspended OC, drifting coarse particulate OC (drift OC), organic debris and the biomass of in-stream primary producers in five geographically proximate small rivers in south-eastern Australia during base-flow conditions. Despite differences in the extent of land-use conversion (native forest-to-pasture) and geomorphology among all sites, we found greater within-river than ‘within-land-use’ similarities in OC reservoirs. Our predictions regarding the r
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18

Twidale, Charles Rowland. "Evolution of an ancient cratonic upland, the Gawler Ranges of inland South Australia." Géomorphologie : relief, processus, environnement 26, no. 1 (May 1, 2020): 35–54. http://dx.doi.org/10.4000/geomorphologie.14036.

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19

OHMORI, Hiroo, Kunihiko ENDO, Yo UESUGI, and Masuoki HORIKOSHI. "Stratigraphy and geomorphologic history of Holocene dunefield near Millicent along the southeastern coast of South Australia." Journal of Geography (Chigaku Zasshi) 96, no. 1 (1987): 1–22. http://dx.doi.org/10.5026/jgeography.96.1.

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20

Linklater, Michelle, Timothy C. Ingleton, Michael A. Kinsela, Bradley D. Morris, Katie M. Allen, Michael D. Sutherland, and David J. Hanslow. "Techniques for Classifying Seabed Morphology and Composition on a Subtropical-Temperate Continental Shelf." Geosciences 9, no. 3 (March 22, 2019): 141. http://dx.doi.org/10.3390/geosciences9030141.

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In 2017, the New South Wales (NSW) Office of Environment and Heritage (OEH) initiated a state-wide mapping program, SeaBed NSW, which systematically acquires high-resolution (2–5 m cell size) multibeam echosounder (MBES) and marine LiDAR data along more than 2000 km of the subtropical-to-temperate southeast Australian continental shelf. This program considerably expands upon existing efforts by OEH to date, which have mapped approximately 15% of NSW waters with these technologies. The delivery of high volumes of new data, together with the vast repository of existing data, highlights the need
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21

Hinschberger, Florent, Jacques André Malod, Jean Pierre Réhault, and Safri Burhanuddin. "Contribution of bathymetry and geomorphology to the geodynamics of the East Indonesian Seas." Bulletin de la Société Géologique de France 174, no. 6 (November 1, 2003): 545–60. http://dx.doi.org/10.2113/174.6.545.

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Abstract Southeastern Indonesia is located at a convergent triple junction of 3 plates : the Pacific (including the Caro-line and Philippines plates), the Australian and the Southeast Asian plates (fig. 1). The age of the different basins : the North Banda Sea (Sula Basin), the South Banda Sea (Wetar and Damar Basins) and the Weber Trough has been debated for a long time. Their great depth was a reason to interpret them as remnants of oceanic domains either of Indian or Pacific ocean affinities. It has now been demonstrated from geochronological studies that these basins have formed during the
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22

BARLETTA, RODRIGO DO CARMO, and LAURO JÚLIO CALLIARI. "Determinação da Intensidade das Tempestades que atuam no Litoral do Rio Grande do Sul, Brasil." Pesquisas em Geociências 28, no. 2 (December 31, 2001): 117. http://dx.doi.org/10.22456/1807-9806.20276.

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Waves generated by South Atlantic storms are greatly responsible for the beach and coastal erosion verified at the central coast of Rio Grande do Sul State, Brazil. These beaches are classified as intermediate, according to the morphodynamic approach suggested by the “Australian School of Coastal Geomorphology”. The storm wave regime controls the morphodynamic variability of those sandy beaches. Through the classification proposed by Dolan and Davis (1992). South Atlantic storms were classified and related to meteorological systems, considering corresponding beach responses. Out of the 3 year
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23

McBride, Randolph A., Thomas S. N. Oliver, Amy J. Dougherty, Toru Tamura, Rafael C. Carvalho, Andrew D. Short, and Colin D. Woodroffe. "The turnaround from transgression to regression of Holocene barrier systems in south‐eastern Australia: Geomorphology, geological framework and geochronology." Sedimentology, December 27, 2020. http://dx.doi.org/10.1111/sed.12812.

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24

Williams, Martin, Nicholas Nitschke, and Carly Chor. "Complex geomorphic response to late Pleistocene climatic changes in the arid Flinders Ranges of South Australia." Géomorphologie : relief, processus, environnement 12, no. 4 (December 31, 2006). http://dx.doi.org/10.4000/geomorphologie.47.

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