Relevant bibliographies by topics / Western New South Wales

Academic literature on the topic 'Western New South Wales'

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Published: 4 June 2021
Last updated: 31 January 2023

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Journal articles on the topic "Western New South Wales"

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Cherbury, Chas P. "Rain-making in Western New South Wales." Mankind 1, no. 6 (February 10, 2009): 138. http://dx.doi.org/10.1111/j.1835-9310.1932.tb00027.x.

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Holdsworth, Rhiannon L., Elizabeth Downie, Matthew J. Georgiades, Ross Bradbury, Julian Druce, and James Collett. "Lymphocytic choriomeningitis virus in western New South Wales." Medical Journal of Australia 216, no. 2 (January 6, 2022): 71–72. http://dx.doi.org/10.5694/mja2.51383.

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Green, DR. "Rangeland restoration projects in western New South Wales." Rangeland Journal 11, no. 2 (1989): 110. http://dx.doi.org/10.1071/rj9890110.

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The semi-arid to arid Western Division of New South Wales has suffered significant levels of land degradation due to overstocking by domestic animals and rabbits. Three major forms of land degradation are identified, soil erosion, woody weed growth and pasture quality decline. Restoration techniques developed and applied by the New South Wales Soil Conservation Service are presented and discussed. The successful techniques presented are contour furrowing and waterponding for sheet eroded or scalded areas, fire and blade ploughing for woody weed control and grazing management to reverse pasture decline. The lack of knowledge on pasture species responses to grazing management stimuli is highlighted.
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Webster, Rick, Chris Belcher, and David Leslie. "A survey for threatened fauna in south-western New South Wales." Australian Zoologist 32, no. 2 (February 2003): 214–28. http://dx.doi.org/10.7882/az.2003.003.

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Jago, James B., and Mark D. Pharaoh. "Pre-Antarctic Mawson in South Australia and western New South Wales." Transactions of the Royal Society of South Australia 140, no. 1 (January 2, 2016): 107–28. http://dx.doi.org/10.1080/03721426.2016.1149323.

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Oliver, Damon. "Future of the fauna of western New South Wales." Pacific Conservation Biology 3, no. 1 (1997): 78. http://dx.doi.org/10.1071/pc970078.

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This attractively presented and enlightening collection of 22 chapters written by biologists, government land managers and a pastoralist, was derived from a 1991 symposium of the same name organized by the Royal Zoological Society of New South Wales. A third of the book deals with pre- and post-European land management practices that have drastically modified the western region of New South Wales. Another third is dedicated to the impact of these practices on habitat modification and the major vertebrate fauna groups, and for some of the invertebrates. Most of the chapters regarding the biology and ecology of the region paint a bleak picture of the negative impact on its faunal components. By presenting information in this manner, however, it is hoped that the problems will be actively addressed to ensure the future survival of native fauna. The chapters written by government land managers of National Parks, CALM and Landcare read more optimistically, and provide positive solutions to some of these problems. From reading these chapters, I now have a much better appreciation of the principles of reserve design and also how the Landcare network plays a vital role in the off-reserve conservation effort on farms.
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Jarmen, Peter, Daniel Lunney, Suzanne Hand, Philip Reed, and David Butcher. "Future of the Fauna of Western New South Wales." Journal of Animal Ecology 65, no. 4 (July 1996): 533. http://dx.doi.org/10.2307/5792.

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Webb, J. A. "Discussion: Proterozoic palaeokarst at Torrowangee, western New South Wales?" Australian Journal of Earth Sciences 33, no. 3 (September 1986): 365–66. http://dx.doi.org/10.1080/08120098608729372.

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Balme, Jane. "30,000 years of fishery in western New South Wales." Archaeology in Oceania 30, no. 1 (April 1995): 1–21. http://dx.doi.org/10.1002/j.1834-4453.1995.tb00324.x.

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Grant, T. R., P. C. Gehrke, J. H. Harris, and S. Hartley. "Distribution of the Platypus (Ornithorhynchus anatinus) in New South Wales: Results of The 1994-96 New South Wales Rivers Survey." Australian Mammalogy 21, no. 2 (1999): 177. http://dx.doi.org/10.1071/am00177.

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Data from the New South Wales Rivers Survey on the occurrence of platypuses have provided the most recent and comprehensive record of platypus distribution in the State. The species was most commonly reported from the montane and coastal regions, being less common on the western slopes and uncommon in the rivers of the western lowlands. The observations confirmed those from earlier community-based surveys. In contrast to the distribution of native fish species, there appears to have been little change in the overall state-wide distribution of the platypus in response to degrading processes in the rivers of New South Wales, although nothing is known of the stability of their population numbers.
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Dissertations / Theses on the topic "Western New South Wales"

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Elliott, Malcolm Gordon. "Grass tetany of cattle in New South Wales /." View thesis View thesis, 2000. http://library.uws.edu.au/adt-NUWS/public/adt-NUWS20030424.150628/index.html.

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Fanning, Patricia C. "Beyond the divide: a new geoarchaeology of Aboriginal stone artefact scatters in Western NSW, Australia." Australia : Macquarie University, 2002. http://hdl.handle.net/1959.14/45010.

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Thesis (PhD)--Macquarie University, Division of Environmental & Life Sciences, Graduate School of the Environment, 2002.
Includes bibliographical references: p. 228-232.
Geomorphology, archaeology and geoarchaeology: introduction and background -- Surface stone artefact scatters: why can we see them? -- Geomorphic controls on spatial patterning of the surface stone artefact record -- A temporal framework for interpreting surface artefact scatters in Western NSW -- Synthesis: stone artefact scatters in a dynamic landscape.
Surface scatters of stone artefacts are the most ubiquitous feature of the Australian Aboriginal archaeological record, yet the most underutilized by archaeologists in developing models of Aboriginal prehistory. Among the many reasons for this are the lack of understanding of geomorphic processes that have exposed them, and the lack of a suitable chronological framework for investigating Aboriginal 'use of place'. This thesis addresses both of these issues. -- In arid western NSW, erosion and deposition accelerated as a result of the introduction of sheep grazing in the mid 1800s has resulted in exposure of artefact scatters in some areas, burial in others, and complete removal in those parts of the landscape subject to concentrated flood flows. The result is a patchwork of artefact scatters exhibiting various degrees of preservation, exposure and visibility. My research at Stud Creek, in Sturt National Park in far western NSW, develops artefact and landscape survey protocols to accommodate this dynamic geomorphic setting. A sampling strategy stratified on the basis of landscape morphodynamics is presented that allows archaeologists to target areas of maximum artefact exposure and minimum post-discard disturbance. Differential artefact visibility at the time of the survey is accommodated by incorporating measures of surface cover which quantify the effects of various ephemeral environmental processes, such as deposition of sediments, vegetation growth, and bioturbation, on artefact count. -- While surface stone artefact scatters lack the stratigraphy usually considered necessary for establishing the timing of Aboriginal occupation, a combination of radiocarbon determinations on associated heat-retainer ovens, and stratigraphic analysis and dating of the valley fills which underlie the scatters, allows a two-stage chronology for huntergatherer activity to be developed. In the Stud Creek study area, dating of the valley fill by OSL established a maximum age of 2,040±100 y for surface artefact scatters. The heatretainer ovens ranged in age from 1630±30 y BP to 220±55 y BP. Bayesian statistical analysis of the sample of 28 radiocarbon determinations supported the notion, already established from analysis of the artefacts, that the Stud Creek valley was occupied intermittently for short durations over a relatively long period of time, rather than intensively occupied at any one time. Furthermore, a gap in oven building between about 800 and 1100 years ago was evident. Environmental explanations for this gap are explored, but the paiaeoenvironmental record for this part of the Australian arid zone is too sparse and too coarse to provide explanations of human behaviour on time scales of just a few hundred years. -- Having established a model for Stud Creek of episodic landscape change throughout the late Pleistocene and Holocene, right up to European contact, its veracity was evaluated in a pilot study at another location within the region. The length of the archaeological record preserved in three geomorphically distinct locations at Fowlers Gap, 250 km south of Stud Creek, is a function of geomorphic dynamics, with a record of a few hundred years from sites located on channel margins and low terraces, and the longest record thus far of around 5,000 years from high terrace surfaces more remote from active channel incision. But even here, the record is not continuous, and like Stud Creek, the gaps are interpreted to indicate that Aboriginal people moved into and out of these places intermittently throughout the mid to late Holocene. -- I conclude that episodic nonequilibrium characterizes the geomorphic history of these arid landscapes, with impacts on the preservation of the archaeological record. Dating of both archaeological and landform features shows that the landscape, and the archaeological record it preserves, are both spatially and temporally disjointed. Models of Aboriginal hunter-gatherer behaviour and settlement patterns must take account of these discontinuities in an archaeological record that is controlled by geomorphic activity. -- I propose a new geoarchaeological framework for landscape-based studies of surface artefact scatters that incorporates geomorphic analysis and dating of landscapes, as well as tool typology, into the interpretation of spatial and temporal patterns of Aboriginal huntergatherer 'use of place'.
Mode of access: World Wide Web.
vii, 232 p. ill., maps
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Holzapfel, Michael, and n/a. "Regolith-landform mapping and dryland salinity investigaton: Booberoi-Quandialla Transect, Western New South Wales." University of Canberra. Resource, Environmental & Heritage Sciences, 2004. http://erl.canberra.edu.au./public/adt-AUC20060519.144945.

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Landholders in the Booberoi to Quandialla (B-Q) Transect area, located in central west NSW, have been concerned about an emerging dryland salinity problem since the late 1990�s (Wooldridge 2002, pers. comm. Muller 2002, pers. comm.) with borehole information and electromagnetic induction investigations supporting anecdotal observations. The presence of indicator vegetation, waterlogging of soils and salinisation of land are becoming increasingly prevalent, with two well-documented sites including �Strathairlie� near Quandialla, and �Back Creek� near West Wyalong. The B-Q Transect area lies within the Bland Creek Catchment, a broad open plain of subdued topography and restricted drainage receiving sediments from elevated rises located to the west, south and east. Significant deposits of transported alluvial materials have in-filled the catchment to depths in excess of 160 m and have posed a particular impediment to regional-scale mineral exploration. Stream flow across the alluvial plains and low angle alluvial fans is intermittent with most of the flow being diverted into groundwater storage or lost to evaporation. Rarely do streams flow into Lake Cowal to the north. A partial electromagnetic (EM) induction survey coupled with a long term bore and piezometer network monitoring program have been implemented by the Department of Infrastructure, Planning and Natural Resources (DIPNR � formerly Department of Land and Water Conservation) Central West NSW Salt Group. These programs allow for initial, broad-scale evaluation of the magnitude and spatial distribution of the salinity problem but fail to pinpoint remaining sites at risk as well as the mechanisms of salt emplacement. As part of an approach to assist with hazard mitigation and land management, two regolith-landform maps are being compiled using 1:20,000 scales in the Back Creek and Quandialla areas. A third, more regional regolith-landform map at 1:50,000 scale (Holzapfel & Moore 2003a, b & c) provides context for the more detailed mapping areas. The new regolith-landform maps will aid in interpretation of existing geophysical techniques, help piece together the three-dimensional characteristics of the Bland Creek catchment, aid in the development of a shallow fluid flow and palaeotopographic model and assist land managers in formulating land management units (LMU�s). The three-dimensional integration of regolith-landform mapping, electromagnetic studies, bore information and other geophysical methods is critical in determining the interaction, distribution and movement of groundwater in the Bland Creek Catchment as buried palaeochannels represent preferred fluid pathways. The distribution of these palaeochannels has implications for future dryland salinity outbreaks, the remediation of current outbreaks and mineral exploration closer to the well-known Wyalong Goldfield (Lawrie et al., 1999). The western quarter of the B-Q Transect area partially overlaps with the recently completed GILMORE Project (Lawrie et al., 2003a,b & c), a multi-disciplinary study, coordinated by Geoscience Australia (GA) and the Bureau of Rural Sciences (BRS). Regolith-landform information in addition to gamma-ray spectrometry, magnetics, airborne electromagnetics and a digital elevation model acquired by the GILMORE Project have been incorporated into regolith-landform maps over the B-Q Transect. The incorporation of these datasets has helped not only extend the usefulness of the GILMORE Project data but provide a consistent, regolith-landform coverage for the broader Bland Creek Catchment. Regolith-landform mapping has been successful in highlighting major recharge zones for local and intermediate flow systems. The mechanisms for dryland salinity at two well-known sites have also been determined. Increasing salt stores are occurring through evaporation of intermittent floodwaters sourced from floodplains, back plains and broad meandering existing creek systems and recharging partially exposed palaeochannels intersecting the surface. Due to the shallow nature of these partially exposed palaeochannels, evaporation further concentrates the salt load in the soil profile. It is unknown if mapped shallow palaeochannels further away from current drainage systems are affected by rising salt loads. Regolith-landform mapping highlights two additional risk factors common to the 1:50,000 and 1:20,000 scale B-Q Transect mapping areas including widespread waterlogging of soils and wind erosion. Due to the subdued topography, features such as gilgai, fences and roads are having an effect on drainage modification. Wind erosion was also observed to play a major role within the B-Q Transect with significant loss of topsoil creating hardened clay surfaces resistant to water infiltration and significant redistributed deposits of aeolian materials. Interpretation of regolith-landform mapping against geophysical datasets and drill hole data show considerable lateral and vertical variation of regolith units. This variation of regolith distribution with depth does not reduce the effectiveness of using regolithlandform mapping as a valued management tool. The subdued relief coupled with the complex interplay between recharge zones, discharge zones and surficial drainage networks over the B-Q Transect still requires a detailed knowledge of surface regolithlandform characteristics whilst reinforcing the need for a multidisciplinary approach to gain a 3D perspective. Catchment analysis has been performed on drainage systems within the Bland Creek Catchment and has helped explain the strong effect different catchments have had on sediment supply to the Bland Basin. Catchment analysis results have been used in basic calculations of salt loads in the Bland Creek Catchment. An estimated 18,780 Tonnes/yr of salt enter the Bland Creek catchment and as stream flow out of the Bland Creek Catchment is intermittent, salt stores are increasing in the upper margins of the soil profile and groundwater reserves. Reconstruction of the palaeotopography of the B-Q Transect has been made possible using a mutli-disciplinary approach incorporating information from regolith-landform mapping, drill hole information, gamma-ray spectrometry and GILMORE Project datasets. The production of large-scale regolith-landform mapping, the development of a shallow fluid flow model and reconstruction of palaeotopography builds on and contributes to knowledge of the Bland Creek Catchment allowing for detailed farmscale and paddock-scale land management decisions.
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Jayawickrema, Jacintha. "A reconstruction of the ecological history of Longneck Lagoon New South Wales, Australia /." View thesis, 2000. http://library.uws.edu.au/adt-NUWS/public/adt-NUWS20050720.135957/index.html.

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Johnson, Andrew. "Crime, governance and numbers : a genealogy of counting crime in New South Wales /." View thesis, 2000. http://library.uws.edu.au/adt-NUWS/public/adt-NUWS20030728.132436/index.html.

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Thesis (Ph.D.) -- University of Western Sydney, 2000.
A thesis submitted in fulfilment of the requirements for the degree of PhD, Department of Critical Social Sciences, University of Western Sydney, 2000. Bibliography : leaves 196-214.
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Everett, Kristina Lyn. "Impossible realities the emergence of traditional Aboriginal cultural practices in Sydney's western suburbs /." Phd thesis, Australia : Macquarie University, 2007. http://hdl.handle.net/1959.14/84406.

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"22nd November, 2006".
Thesis (PhD)--Macquarie University, Division of Society, Culture, Media & Philosophy, Dept. of Anthropology, 2007.
Bibliography: leaves 301-330.
Introduction -- Between ourselves -- Two (or three) for the price of one -- Community -- Bits and pieces -- Space painting or painting space -- Talkin' the talk. Bunda bunya miumba (Thundering kangaroos): dancing up a storm -- Welcome to Country: talkin' the talk -- Messing with ceremony -- 'Ethnogenesis' and the emergence of 'darug custodians' -- Conclusion.
The thesis concerns an Aboriginal community, members of which inhabit the western suburbs of Sydney at the beginning of the twenty-first century. This particular group of people has emerged as a cultural group over the last twenty-five years. In other words, the community did not exist before the advent of Aboriginal land rights in Australia. It might be right to suggest that without land rights, native title and state celebrations and inclusions of Aboriginal peoples as multicufturalism, this particular urban community would not and could not exist at all. That, however, would be a simplistic analysis of a complex phenomenon. Land rights and native title provide the beginning of this story. It becomes much more interesting when the people concerned take it up themselves. -- The main foci in the thesis are the cultural forms that this particular community overtly and intentionally produce as articulations of their identity, namely public speaking, dancing, painting and ceremony. I argue that it is only through these yery deliberate collective practices of identity-making that community identity can be produced. This is because the place that the group claims as its own - Sydney - is always already inhabited by 'us' (the dominant society). Analysis of these cultural forms reveals that even if the existence of the group depends on land rights and, attempts to attract the ultimate 'authenticity' bestowed by native title, members of this group are not conforming to native title rules pertinent to what constitutes 'genuine' 'Aboriginality' for the purposes of winning land claims. Their revived traditions are pot what the state prescribes as representative of 'authentic' urban Aboriginal culture. -- The thesis analyses the ways in which urban Aboriginal peoples are makipg themselves in the era and context of native title. It considers the consequences of being themselves.
Mode of access: World Wide Web.
xii, 330, [8] leaves ill., maps
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Smith, Martin Lancaster, and martin smith@anu edu au. "Towards a Geochronology for Long-term Landscape Evolution, Northwestern New South Wales." The Australian National University. Research School of Earth Sciences, 2006. http://thesis.anu.edu.au./public/adt-ANU20061026.141414.

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The study area extends from west of the Great Divide to the Broken Hill and Tibooburra regions of far western New South Wales, encompassing several important mining districts that not only include the famous Broken Hill lodes (Pb-Zn-Ag), but also Parkes (Cu-Au), Peak Hill (Au), Cobar (Cu-Au-Zn) and White Cliffs (opal). The area is generally semi-arid to arid undulating to flat terrain covered by sparse vegetation. ¶ During the Cretaceous, an extensive sea retreated across vast plains, with rivers draining from the south and east. After the uplift of the Great Divide associated with opening of the Tasman Sea in the Late Cretaceous, drainage swung to the west, cutting across the Darling River Lineament. The Murray-Darling Basin depression developed as a depocentre during the Paleogene. Climates also underwent dramatic change during the Cenozoic, from warm-humid to cooler, more seasonal climates, to the arid conditions prevalent today. Up until now, there has been very little temporal constraint on the development of this landscape over this time period. This study seeks to address the timing of various weathering and landscape evolution events in northwestern New South Wales. ¶ The application of various regolith dating methods was undertaken. Palaeomagnetic dating, clay δ18O dating, (U+Th)/He and U-Pb dating were all investigated. Palaeomagnetic and clay dating methods have been well established in Australian regolith studies for the last 30 years. More recently, (U+Th)/He dating has been successfully trialled both overseas and in Australia. U-Pb dating of regolith materials has not been undertaken. Each method dates different regolith forming processes and materials. Palaeomagnetic and clay dating were both successfully carried out for sites across northwestern New South Wales, providing a multi-technique approach to resolving the timing of weathering events. Although (U+Th)/He dating was unsuccessful, there is scope for further refinement of the technique, and its application to regolith dating. U-Pb dating was also unsuccessfully applied to late-stage anatase, which is a cement in many Australian silcretes. ¶ Results from this study indicate that the landscape evolution and weathering history of northwestern New South Wales dates back at least 60 million years, probably 100 million years, and perhaps even as far back as 180 million years. The results imply that northwestern New South Wales was continuously sub-aerially exposed for the last 100 Ma, indicating that marine sedimentation in the Murray-Darling and Eromanga-Surat Basins was separated by this exposed region. The ages also provide further evidence for episodic deep chemical weathering under certain climatic conditions across the region, and add to the data from across Australia for similar events. In particular, the palaeomagnetic ages, which cluster at ~60 ± 10 Ma and 15 ± 10 Ma, are recorded in other palaeomagnetic dating studies of Australian regolith. The clay ages are more continuous across the field area, but show older clays in the Eromanga Basin sediments at White Cliffs and Lightning Ridge, Eocene clays in the Cobar region, and Oligocene – Miocene clays in the Broken Hill region, indicating progressively younger clay formation from east to west across northwestern New South Wales, in broad agreement with previously published clay weathering ages from around Australia. ¶ These weathering ages can be reconciled with reconstructions of Australian climates from previously published work, which show a cooling trend over the last 40 Ma, following an extended period of high mean annual temperatures in the Paleocene and Eocene. In conjunction with this cooling, total precipitation decreased, and rainfall became more seasonal. The weathering ages fall within periods of wetness (clay formation), the onset of seasonal climate (clay formation and palaeomagnetic weathering ages) and the initiation of aridity in the late Miocene (palaeomagnetic weathering ages). ¶ This study provides initial weathering ages for northwestern New South Wales, and, a broad geochronology for the development of the landscape of the region. Building on the results of this study, there is much scope for further geochronological work in the region.
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Hardiman, Nigel John. "Visitor impact management in canyons of the Blue Mountains, New South Wales /." View thesis, 2003. http://library.uws.edu.au/adt-NUWS/public/adt-NUWS20030708.115013/index.html.

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Thesis (Ph.D.) -- University of Western Sydney, 2003.
"Submitted in fulfilment of the requirements for the degree of Doctor of Philosophy, Centre for Integrated Catchment Management, University of Western Sydney, April 2003" Bibliography : leaves 338-356.
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Darbas, Toni School of Science &amp Technology Studies UNSW. "Democracy, consultation and socio-environmental degradation : diagnostic insights from the Western Sydney/Hawkesbury-Nepean region." Awarded by:University of New South Wales. School of Science and Technology Studies, 2002. http://handle.unsw.edu.au/1959.4/19281.

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The use of community consultation to address socio-environmental degradation is entwined with contested democratic principles polarising views of its role. I frame this problem by examining three democratic paradigms faced with two contemporary problems. The deliberative argument that preferences require enrichment with debate mediates between the liberal-aggregative view that preferences are individual, private and amenable to aggregation and the view that participation in public life is foundational. Viewing consultation as deliberative reconciles the liberal-aggregative view of consultation as the illegitimate elevation of unrepresentative minority groups with the participationist view that consultation constitutes a step towards participatory democracy. Theorists of social reflexivity, however, point to an elided politics of knowledge challenging technoscience's exemption from politically garnered consent. Also neglected by much democratic theory is how functional differentiation renders self-referential legal, political, technoscientific and administrative domains increasingly unaccountable. I employ Habermas' procedural theory that public spheres allow social irritations into the political domain where they can be encoded into laws capable of systemic interjection in response, along with a dialogic extension accommodating the politics of knowledge. I then use this procedural-dialogic deliberative understanding of democracy to elucidate the context and outcomes of the NSW State's consultative strategy. The NSW state, institutionally compelled to underwrite economic growth, implicating itself in that growth's socio-environmental side effects provoking widespread contestation. The resulting Environmental Planning and Assessment Act (1979) and its adjunctive consultative provisions helped highlight the socio-environmental degradation of the Hawkesbury Nepean River Catchment via Western Sydney's urban sprawl, politicising the region. The convenement of a consultative forum to oversee a contaminated site audit within the region facilitated incisive lay critique of the technoscientific underpinnings of administrative underwriting of socio-environmental degradation. The discomforted NSW State tightened environmental policy, gutted the EP&A Act's consultative provisions and removed regional dialogic forums and institutions. I conclude that the socio-economic accord equating economic growth with social progress is both entrenched and besieged, destabilising the political/administrative/technoscientific regime built upon it. This withdrawal of avenues for critique risks deeper estrangement between reflexive society and the NSW State generative of electoral volatility.
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McGovern, Alyce M. "Policing media controlling representations of the New South Wales Police Force /." View thesis, 2008. http://handle.uws.edu.au:8081/1959.7/43816.

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Thesis (Ph.D.)--University of Western Sydney, 2008.
A thesis presented to the University of Western Sydney, College of Arts, School of Social Sciences, in fulfilment of the requirements for the degree of Doctor of Philosphy. Includes bibliographies.
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Books on the topic "Western New South Wales"

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Plants of western New South Wales. Collingwood, Vic: CSIRO Publishing, 2011.

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Muir, Sonia. Living out back: People of Western New South Wales. Orange, NSW: NSW Agriculture, 2002.

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Museum, Australian. Australian Museum's Aboriginal collections: Far Western New South Wales catalogue. Sydney: The Museum, 2001.

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David, Copsey, ed. Australia: Queensland, New South Wales, Victoria, Tasmania, South Australia, Western Australia, Northern Territory. New York: Gallery Books, 1987.

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Adventuring in Australia: New South Wales, Northern Territory, Queensland, South Australia, Tasmania, victoria, Western Australia. 2nd ed. San Francisco: Sierra Club Books, 1999.

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Condon, Dick. Out of the west: Historical perspectives on the Western Division of New South Wales. [Mildura]: Rangeland Management Action Plan, 2002.

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Credit acts handbook for Victoria, New South Wales, the Australian Capital Territory, and Western Australia. Sydney: Law Book Co., 1985.

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Wagner, Regine. The good, the bad and the invisible: Partnerships and collaborations between three sectors in central western New South Wales. [Kingswood, N.S.W: UWS, ACWA], 2003.

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Place as occupational histories: An investigation of the deflated surface archaeological record of Pine Point and Langwell Stations, Western New South Wales, Australia. Oxford, England: Archaeopress, 2008.

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Ryan, Ver Bermoes, ed. New South Wales. 4th ed. Footscray, Vic: Lonely Planet, 2004.

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Book chapters on the topic "Western New South Wales"

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Tyler, Michael J. "Frogs of western New South Wales." In Future of the Fauna of Western New South Wales, 155–60. P.O. Box 20, Mosman NSW 2088, Australia: Royal Zoological Society of New South Wales, 1994. http://dx.doi.org/10.7882/rzsnsw.1994.014.

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Briggs, S. V. "The future of waterbirds in western New South Wales." In Future of the Fauna of Western New South Wales, 149–54. P.O. Box 20, Mosman NSW 2088, Australia: Royal Zoological Society of New South Wales, 1994. http://dx.doi.org/10.7882/rzsnsw.1994.013.

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Cambell, D. "Clearing and cultivation in the Western Division." In Future of the Fauna of Western New South Wales, 201–5. P.O. Box 20, Mosman NSW 2088, Australia: Royal Zoological Society of New South Wales, 1994. http://dx.doi.org/10.7882/rzsnsw.1994.019.

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Halliger, Michael. "Reptiles on regenerating mine sites in western New South Wales." In Herpetology in Australia, 327–32. P.O. Box 20, Mosman NSW 2088, Australia: Royal Zoological Society of New South Wales, 1993. http://dx.doi.org/10.7882/rzsnsw.1993.050.

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Leitch, E. C., B. D. Webby, K. J. Mills, and P. Kolbe. "Terranes of the Wonominta block, far western New South Wales." In Terrane Accretion and Orogenic Belts, 31–37. Washington, D. C.: American Geophysical Union, 1987. http://dx.doi.org/10.1029/gd019p0031.

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Dickman, C. R. "Native mammals of western New South Wales: past neglect, future rehabilitation?" In Future of the Fauna of Western New South Wales, 81–91. P.O. Box 20, Mosman NSW 2088, Australia: Royal Zoological Society of New South Wales, 1994. http://dx.doi.org/10.7882/rzsnsw.1994.008.

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Schodde, R. "The bird fauna of western New South Wales: geography and status." In Future of the Fauna of Western New South Wales, 107–21. P.O. Box 20, Mosman NSW 2088, Australia: Royal Zoological Society of New South Wales, 1994. http://dx.doi.org/10.7882/rzsnsw.1994.011.

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Lunney, Daniel. "Review of official attitudes to western New South Wales 1901–93 with particular reference to the fauna." In Future of the Fauna of Western New South Wales, 1–26. P.O. Box 20, Mosman NSW 2088, Australia: Royal Zoological Society of New South Wales, 1994. http://dx.doi.org/10.7882/rzsnsw.1994.001.

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Strahan, R. "The dilemma of efficient agriculture practices." In Future of the Fauna of Western New South Wales, 27–29. P.O. Box 20, Mosman NSW 2088, Australia: Royal Zoological Society of New South Wales, 1994. http://dx.doi.org/10.7882/rzsnsw.1994.002.

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Pressey, R. L. "Land classifications are necessary for conservation planning but what do they tell us about fauna?" In Future of the Fauna of Western New South Wales, 31–41. P.O. Box 20, Mosman NSW 2088, Australia: Royal Zoological Society of New South Wales, 1994. http://dx.doi.org/10.7882/rzsnsw.1994.003.

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Conference papers on the topic "Western New South Wales"

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Hewson, R. D., G. R. Taylor, and L. B. Whitbourn. "Application of TIR Imagery and Spectroscopy for the Extraction of Soil Textural Information at Fowlers Gap, Western New South Wales, Australia." In IGARSS 2008 - 2008 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2008. http://dx.doi.org/10.1109/igarss.2008.4779095.

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Marfella, Giorgio. "Seeds of Concrete Progress: Grain Elevators and Technology Transfer between America and Australia." In The 38th Annual Conference of the Society of Architectural Historians Australia and New Zealand. online: SAHANZ, 2022. http://dx.doi.org/10.55939/a4000pi5hk.

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Modern concrete silos and grain elevators are a persistent source of interest and fascination for architects, industrial archaeologists, painters, photographers, and artists. The legacy of the Australian examples of the early 1900s is appreciated primarily by a popular culture that allocates value to these structures on aesthetic grounds. Several aspects of construction history associated with this early modern form of civil engineering have been less explored. In the 1920s and 1930s, concrete grain elevator stations blossomed along the railway networks of the Australian Wheat Belts, marking with their vertical presence the landscapes of many rural towns in New South Wales, Queensland, Victoria, and Western Australia. The Australian reception of this industrial building type of American origin reflects the modern nation-building aspirations of State Governments of the early 1900s. The development of fast-tracked, self-climbing methods for constructing concrete silos, a technology also imported from America, illustrates the critical role of concrete in that effort of nation-building. The rural and urban proliferation of concrete silos in Australia also helped establish a confident local concrete industry that began thriving with automatic systems of movable formwork, mastering and ultimately transferring these construction methods to multi-storey buildings after WWII. Although there is an evident link between grain elevators and the historiographical propaganda of heroic modernism, that nexus should not induce to interpret old concrete silos as a vestige of modern aesthetics. As catalysts of technical and economic development in Australia, Australian wheat silos also bear important significance due to the international technology transfer and local repercussions of their fast-tracked concrete construction methods.
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Platt, T. J. "New South Wales Incident Management System." In Ninth International Conference on Road Transport Information and Control. IEE, 1998. http://dx.doi.org/10.1049/cp:19980182.

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Senden, David van, and Douglas Lord. "Estuary Processes Investigation; New South Wales, Australia." In 27th International Conference on Coastal Engineering (ICCE). Reston, VA: American Society of Civil Engineers, 2001. http://dx.doi.org/10.1061/40549(276)288.

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Simou, Xeni. "The Old Navarino fortification (Palaiokastro) at Pylos (Greece). Adaptation to early artillery." In FORTMED2020 - Defensive Architecture of the Mediterranean. Valencia: Universitat Politàcnica de València, 2020. http://dx.doi.org/10.4995/fortmed2020.2020.11389.

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Old Navarino fortification (Palaiokastro) is located on the promontory supervising the naturally endowed Navarino-bay at the south-western foot of Peloponnese peninsula, near the contemporary city of Pylos. The cliff where it is built and where ancient relics lie, was fortified by Frankish in the thirteenth century. The fortification though knows significant alterations firstly by Serenissima Republic of Venice from the fifteenth century that aims to dominate the naval routes of Eastern Mediterranean by establishing a system of coastal fortifications and later by the Ottomans after the conquest of Venice’s possessions at Messenia in 1500. Between fifteenth and seventeenth century, apart from important modifications at the initial enceinte of the northern Upper City, the most notable transformation of Old Navarino is the construction of the new Lower fortification area at the south and the southern outwork ending up to the coastline. Especially the Lower fortification is a sample of multiple and large-scale successive alterations for the adjustment to technological advances of artillery (fortification walls reinforcement, modification of tower-bastions, early casemates, gate complex enforcements). The current essay focuses on the study of these specific elements of the early artillery period and the examination of Old Navarino’s strategic role at the time of transition before the adaptation of “bastion-front” fortification patterns, such as those experimented in the design of the fortified city of New Navarino, constructed at the opposite side of the Navarino gulf by the Ottomans (1573).
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Conway, Andrew, Michelle Blom, Lee Naish, and Vanessa Teague. "An analysis of New South Wales electronic vote counting." In ACSW 2017: Australasian Computer Science Week 2017. New York, NY, USA: ACM, 2017. http://dx.doi.org/10.1145/3014812.3014837.

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Allen, Lori E., Michael C. B. Ashley, Michael G. Burton, Stuart D. Ryder, John W. V. Storey, and Yinsheng Sun. "UNSWIRF: the University of New South Wales infrared Fabry-Perot." In Astronomical Telescopes & Instrumentation, edited by Albert M. Fowler. SPIE, 1998. http://dx.doi.org/10.1117/12.317242.

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Radoll, Peter, Sebastian Fleissner, Duncan Stevenson, and Henry Gardner. "Improving ICT support for aboriginal land councils in New South Wales." In the Sixth International Conference. New York, New York, USA: ACM Press, 2013. http://dx.doi.org/10.1145/2517899.2517916.

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Zhu, Qinggaozi, Xihua Yang, and Qiang Yu. "Climate change impact on bushfire risk in New South Wales, Australia." In IGARSS 2015 - 2015 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2015. http://dx.doi.org/10.1109/igarss.2015.7326042.

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Catalan, Alex, and C. Suarez. "Geotechnical characterisation — Cadia East panel caving project, New South Wales, Australia." In Second International Symposium on Block and Sublevel Caving. Australian Centre for Geomechanics, Perth, 2010. http://dx.doi.org/10.36487/acg_rep/1002_26_catalan1.

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Reports on the topic "Western New South Wales"

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Cunningham, Stuart, Marion McCutcheon, Mark Ryan, Susan Kerrigan, Phillip McIntyre, and Greg Hearn. ‘Creative Hotspots’ in the regions: Key thematic insights and findings from across Australia. Queensland University of Technology, 2022. http://dx.doi.org/10.5204/rep.eprints.227753.

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Description The Creative Hotspots project, or as it was officially titled Australian Cultural and Creative Activity: A Population and Hotspot Analysis, was an expansive, four-year project funded by an Australian Research Council Linkage grant (LP160101724). This comprehensive national study investigated the contemporary dynamics of cultural and creative activity in largely regional and non-capital cities and towns across Australia before the outbreak of COVID-19 in March 2020. In total, the project conducted fieldwork in 17 creative and cultural hotspots across five states: Queensland, New South Wales, Victoria, Western Australia, and South Australia, examining what makes each hotspot “hot”, identifying the dynamics that underpinned their high concentrations of creative and cultural employment and activity. This White Paper outlines the project's findings and outcomes.
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Reid, Andrew. Tackling gambling harm to improve health equity in New South Wales. Centre for Health Equity Training, Research and Evaluation, 2021. http://dx.doi.org/10.53714/igoo2131.

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Kyi, D., J. Duan, A. Kirkby, and N. Stolz. Australian Lithospheric Architecture Magnetotelluric Project (AusLAMP): New South Wales: data release report. Geoscience Australia, 2020. http://dx.doi.org/10.11636/record.2020.011.

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Chisholm, Emma-Kate, Carol Simpson, and Phillip Blevin. New SHRIMP U-Pb zircon ages from the New England Orogen, New South Wales : July 2010-June 2012. Geoscience Australia, 2014. http://dx.doi.org/10.11636/record.2014.013.

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Chisholm, E. I., P. L. Blevin, and C. J. Simpson. New SHRIMP U–Pb zircon ages from the New England Orogen, New South Wales: July 2012–June 2014. Geoscience Australia, 2014. http://dx.doi.org/10.11636/record.2014.052.

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Waltenberg, K., P. L. Blevin, S. Bodorkos, and D. E. Cronin. New SHRIMP U-Pb zircon ages from the New England Orogen, New South Wales: July 2014-June 2015. Geoscience Australia and Geological Survey of New South Wales, 2015. http://dx.doi.org/10.11636/record.2015.028.

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Armistead, S. E., and G. L. Fraser. New SHRIMP U-Pb zircon ages from the Cuttaburra and F1 prospects, southern Thomson Orogen, New South Wales. Geoscience Australia, 2015. http://dx.doi.org/10.11636/record.2015.020.

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Bodorkos, S., K. F. Bull, L. M. Campbell, M. A. Eastlake, P. J. Gilmore, and S. J. Triggs. New SHRIMP U-Pb ages from the central Lachlan Orogen and New England Orogen, New South Wales: July 2014-June 2015. Geoscience Australia and Geological Survey of New South Wales, 2016. http://dx.doi.org/10.11636/record.2016.021.

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Fraser, G. L., P. J. Gilmore, J. A. Fitzherbert, S. J. Trigg, L. M. Campbell, L. Deyssing, O. D. Thomas, et al. New SHRIMP U-Pb zircon ages from the Lachlan, southern Thomson and New England orogens, New South Wales: February 2011–June 2013. Geoscience Australia, 2014. http://dx.doi.org/10.11636/record.2014.053.

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Armistead, S. E., R. G. Skirrow, G. L. Fraser, D. L. Huston, D. C. Champion, and M. D. Norman. Gold and intrusion-related Mo-W mineral systems in the southern Thomson Orogen, New South Wales. Geoscience Australia, 2017. http://dx.doi.org/10.11636/record.2017.005.

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