Academic literature on the topic 'New South Wales coast'

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Journal articles on the topic "New South Wales coast"

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Bryant, E. A., and R. W. Young. "Bedrock-Sculpturing by Tsunami, South Coast New South Wales, Australia." Journal of Geology 104, no. 5 (September 1996): 565–82. http://dx.doi.org/10.1086/629852.

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Vale, TG, IW Carter, KA McPhie, GS James, and MJ Cloonan. "HUMAN ARBOVIRUS INFECTIONS ALONG THE SOUTH COAST OF NEW SOUTH WALES." Australian Journal of Experimental Biology and Medical Science 64, no. 3 (June 1986): 307–9. http://dx.doi.org/10.1038/icb.1986.32.

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LOWRY, J. K. "Talitrid amphipods from ocean beaches along the New South Wales coast of Australia (Amphipoda, Talitridae)." Zootaxa 3575, no. 1 (December 7, 2012): 1. http://dx.doi.org/10.11646/zootaxa.3575.1.1.

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The sand-hopper Bellorchestia mariae sp. nov. is described from Honeymoon Bay on the north coast of Jervis Bay, NewSouth Wales, Australia. It is the sister species of B. richardsoni Serejo & Lowry, 2008 and appears to have a limited dis-tribution from about Narrawallee in the south to northern Jervis Bay. The distribution of B. richardsoni Serejo & Lowry,2008 is extended from Point Ricardo, Victoria, northwards to Ulladulla on the New South Wales coast. A new synonymyis proposed for the sand-hopper Notorchestia quadrimana (Dana, 1852) which includes N. novaehollandiae (1899) andN. lobata Serejo & Lowry, 2008. It is considered to be a wide-ranging species from Shark Bay in Western Australia aroundthe south coast to at least Maitland Bay in central New South Wales. The beach-hopper Orchestia dispar Dana, 1852 isdescribed from Valla Beach in northern New South Wales and moved to the new genus Vallorchestia. This is the first re-cord of V. dispar since its original description 160 years ago. The beach-hopper Platorchestia smithi sp. nov. is describedfrom Brooms Head, New South Wales, Australia. It is common on ocean beaches from Bendalong in the south to Ballina in northern New South Wales. South of Bendalong beach-hoppers on ocean beaches appear to be absent.
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Young, R. W., E. A. Bryant, and D. M. Price. "Last interglacial sea levels on the south coast of New South Wales." Australian Geographer 24, no. 2 (November 1993): 72–75. http://dx.doi.org/10.1080/00049189308703090.

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Kodela, Phillip, and Terry Tame. "Acacia pedina (Fabaceae: Mimosoideae), a new species from the South Coast, New South Wales." Telopea 8, no. 3 (December 16, 1999): 305–9. http://dx.doi.org/10.7751/telopea19995418.

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Dunstone, R. L., and G. C. Young. "New Devonian plant fossil occurrences on the New South Wales South Coast: geological implications." Australian Journal of Earth Sciences 66, no. 1 (January 2, 2019): 57–70. http://dx.doi.org/10.1080/08120099.2018.1533495.

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Enright, W. J. "A Dilly Bag from the North Coast of New South Wales." Mankind 1, no. 6 (February 10, 2009): 137–38. http://dx.doi.org/10.1111/j.1835-9310.1932.tb00026.x.

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Murphy, Peter A. "Development of strata units in New South Wales North Coast resorts." Australian Geographer 16, no. 4 (November 1985): 272–79. http://dx.doi.org/10.1080/00049188508702883.

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Parer, I., and T. Korn. "Seasonal Incidence of Myxomatosis in New-South-Wales." Wildlife Research 16, no. 5 (1989): 563. http://dx.doi.org/10.1071/wr9890563.

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We analysed monthly records of the presence or absence of myxomatosis in the 59 Pasture Protection Board Districts of New South Wales for 1959-64 and 1980-86. These periods respectively precede and follow the introduction of the European rabbit flea, Spilopsyllus cuniculi (Dale), into New South Wales. Throughout New South Wales during the two periods, myxomatosis was reported more frequently in summer than in winter. The seasonal trend was more pronounced on the western and central plains than on the slopes, tablelands or coastal regions. The incidence of myxomatosis was positively related to rainfall on the western and central plains and slopes, but not on the tablelands and coast. After the introduction of the rabbit flea, the reported incidence of myxomatosis increased more on the tablelands than in the other regions.
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Smith, John V. "Textures recording transient porosity in synkinematic quartz veins, South Coast, New South Wales, Australia." Journal of Structural Geology 27, no. 2 (February 2005): 357–70. http://dx.doi.org/10.1016/j.jsg.2004.09.003.

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Dissertations / Theses on the topic "New South Wales coast"

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Secomb, Dorothy Margaret School of Social Science &amp Policy UNSW. "Retirement in Mobile and Manufactured Housing on the North Coast of New South Wales, Australia." Awarded by:University of New South Wales. School of Social Science and Policy, 2000. http://handle.unsw.edu.au/1959.4/17488.

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This study considers relocatable homes as an alternative housing choice for male and female retirees fifty years of age and over. Homogeneous parks and estates planned for a specific type of relocatable home are compared with those which evolved from tourist parks and retain sites for both permanent and short-term occupancy. Four relocatable home environments are considered: caravan parks, mobile homes in mixed parks, manufactured homes in mixed parks and manufactured housing estates. The differential effects of 'age', 'house type' and 'housing environment' upon 'residential satisfaction', 'sense of community within the neighbourhood', 'social integration in the community' and 'psychological adjustment' form the analytical framework of the study. Residents of 34 parks/ estates on the North Coast of New South Wales completed 778 questionnaires. Case studies, interviews, letters and written comments provided data for qualitative analysis. Approximately 94% of respondents are satisfied with their homes and housing environments. Residential satisfaction is most influenced by the interactions and perceptions of residents; psychological adjustment is influenced by a positive attitudes towards self and one's neighbours; integration in the community is affected by levels of network. Each of these relate strongly with having a sense of community in the neighbourhood. Space internal to the dwelling relates to satisfaction, adjustment and community integration. External space relates to the need for a well planned neighbourhood which affords privacy, safety and amenities. The need for meeting places for small and large groups was recurrent. The results suggest that residents of relocatable homes tend to retain affiliation with organisations joined prior to relocation. They are not reliant on their new neighbours to integrate in their community. This result is contrary to prior research which studied site built homes and traditional neighbourhoods. The present high levels of residential satisfaction would rise if it were not for the overwhelming uncertainty of tenure and unjustifiable rises in site rent. The study reviews government policy especially in relation to tenure. A relocatable home offers no more affordability than a site-built home in the same area in the long-term but it does offer a preferred retirement lifestyle.
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Wilton, Kylee Margaret, and res cand@acu edu au. "Coastal Wetland Habitat Dynamics in Selected New South Wales Estuaries." Australian Catholic University. School of Arts and Sciences, 2002. http://dlibrary.acu.edu.au/digitaltheses/public/adt-acuvp29.29082005.

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Intertidal wetland habitats in southeastern Australia have changed significantly during the past sixty years. Mangrove habitats have expanded both seawards and landwards, the latter being at the expense of saltmarsh habitats. This relatively common phenomenon is generally suggested to be an outcome of sea-level rise. Several factors potentially responsible for this change are examined, including changes in mean sealevel during the past 50 to 100 years, changes in climate, population growth, catchment landuse, and estuary type. A protocol for mapping estuarine habitats was developed and implemented, incorporating the application of geographic information systems. Spatial and temporal coastal wetland habitat changes at nine sites along the New South Wales coast are illustrated. These habitat dynamics were shown to not correlate between sites. The results demonstrate that sea-level rise in this region cannot solely account for the extent of change during the past sixty years. With the exception of one site (Careel Bay), there have been no correlations between contemporary mean sea-level rise and mangrove incursion of the saltmarsh habitats at the study sites, or with rainfall patterns, at the scale of observation in this study, which was largely decadal. The only correlations determined during this study have been between population growth and coastal wetland habitat dynamics in some sites. In spite of saltmarsh habitat loss being a regional phenomenon, local factors appear to have a profound bearing on the rates of change. Neither contemporary mean sea-level rise, rainfall patterns, estuary type, catchment landuse, catchment natural cover nor population pressure can account solely for the patterns in the spatial and temporal dynamics of the coastal wetlands of New South Wales. It seems apparent that regional factors create preconditions favourable for mangrove incursion, but that localised conditions have been responsible for the extent of these incursions from site to site. That is, despite higher sea-level and greater rainfall, the extent of change has been determined by the unique characteristics of each site. The results have important implications for current estuary management practices in the state of New South Wales. The lack of spatial and temporal trends in coastal wetland habitat dynamics point to the need for management to be conducted on a localised, rather than regional scale. Additionally, anthropogenic influences must be carefully managed, since the extent of mangrove habitat expansion into saltmarsh areas is unlikely to be a natural occurrence.
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Nunt-jaruwong, Sorawit School of Biological Earth &amp Environmental Sciences UNSW. "Engineering geology of the Patonga Claystone, Central Coast, New South Wales, with particular reference to slaking behaviour." Awarded by:University of New South Wales. School of Biological, Earth and Environmental Sciences, 2006. http://handle.unsw.edu.au/1959.4/27335.

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The Patonga Claystone, a red bed facies in the Narrabeen Group of the Sydney Basin, is one of the most unfavorable rock units in the basin from a geotechnical point of view. This rock unit is composed of sandstone, siltstone, mudstone and claystone. One of the unfavorable characteristics is the low shear strength, which causes instability of cut slopes; another is its slaking-prone behaviour. Numerous measurements of geotechnical properties, along with extensive mineralogical and geochemical determinations, were carried out to identify cause of this slaking behaviour. Key techniques were the use of quantitative X-ray diffractometry for mineralogical analysis, and the determination of slake durability index and related properties to evaluate the slaking behaviour under both standard and more extended conditions. Standard (two cycle) slake durability test results indicate a range from low to high slake durability index values, with some mudstone samples having very low durability and some sandstones having very high slake durability indices. Jar slake test results indicate that the rock samples break rapidly and/or develop several fractures (Ij = 4) in an as-received state, but degrade to a pile of flakes or mud (Ij = 1) if the samples are oven dried before testing. The results for jar slake testing of oven-dried material are comparable, for individual samples, to those obtained from the more comprehensive slake durability tests. The mineralogy of the samples was evaluated by quantitative X-ray diffraction techniques using the Rietveld-based Siroquant processing system. Comparison to independent chemical data show a generally good level of agreement, suggesting that the mineralogical analysis results are consistent with the chemical composition of the individual rock samples. Good correlations were also obtained between clay mineralogy determined from orientedaggregate XRD analysis of the <2 micron fraction and the results from powder diffractometry and Siroquant analysis of the whole-rock samples. Evaluation of the slake durability characteristics and other geotechnical properties in relation to the quantitative mineralogy suggests that quartz and feldspar form a rigid framework in the rocks that resists the disruptive pressures that cause slaking. Expansion of the clay minerals by various processes, including the incorporation of water into the interlayer spaces of illite/smectite as well as changes in pore pressures associated with entry of water into micro-fractures in the clay matrix, are thought to produce the disruptions that cause slaking and degradation. An abundant clay matrix also reduces the strength of the rock materials, probably because of the less rigid nature of the clay minerals relative to the quartz and feldspar particles. As well as the mineralogy, the loss on ignition (LOI) and water absorption percentage were found to provide good indicators of longer-term slaking behaviour. Both properties are also related to the overall clay content. Rock samples with water absorption values of <10, 10-15 and >15% behave as highly durable, intermediate and less durable materials respectively. Rocks with LOI values of greater than 5% by weight behave as less durable rock materials, at least for the strata encompassed by the present study. The water absorption and LOI values were also used to develop a predictive model of slake durability characteristics for the different rock materials in the Patonga Claystone, providing a relatively simple basis for predicting longer-term stability in a range of geotechnical studies.
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DeMellow, Ian T. M. "Cost efficiency of NSW rail passenger services 1951/52-1991/92 : a case study in corporate strategic modelling." University of Sydney, 1996. http://hdl.handle.net/2123/2693.

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Doctor of Philosophy
During the 1990s, governments, managements and unions have been focused upon improving the cost efficiency of firms. This focus has been strongest for firms in the public sector where improved outcomes can be expected to significantly improve the Gross Domestic Products of whole economies. This case study looks at the cost efficiency of NSW rail passenger services over a 41 year period to 1991/92, long suspected (but hitherto only tentatively demonstrated) as a paradigm of cost inefficiency. The case study focuses upon the use of the total factor productivity (TFP) index, as a datum point for measuring change in productivity in four markets: suburban, internrban, country and interstate passenger services since 1951/52. From this datum, changes over the years in management, technology and other external factors can be identified and assessed. The thesis identifies management quality (the organising element in the firm) as the preeminent factor in determining productivity change, and the role that new technology plays in its impact on failures in management. We establish the linkages between management and innovation, with TFP, pricing efficiency and economic resource use efficiency, to present a rich paradigm for assessing the economic performance of any business firm. Borrowing from systems theory and other management practices such as total quality management, we disaggregated the case firm into its component systems, sub-systems and processes, for separate study in relation to impact on TFP. The database for 41 years of rail behaviour is the richest ever compiled for any railway in Australia, and with enhanced modelling, enables a systematic treatment of the performance through time of State Rail's passenger services.
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Phipps, Kathy, and n/a. "Comparative study of teachers in N.S.W. Department of Education support units (South Coast Region) and teachers in N.S.W. Department of Education special schools (South Coast Region) relating to the implementation of curriculum document for students with severe intellectual disability." University of Canberra. Education, 1993. http://erl.canberra.edu.au./public/adt-AUC20061112.124101.

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The following research project was a comparative study of teachers in Support Units and teachers in Special Schools. They were teachers currently involved with the implementation of the 1989 NSW Department of Education Mandatory Curriculum Change for the education of students with severe intellectual disability. The purpose of the research was to present a comparative study on teachers' responses, in both educational settings, examining their understanding of the curriculum change, the concerns of individuals and the levels of curriculum usage in relation to the factors affecting implementation. The application of the Concerns-Based Adoption Model of Change (Hall and Loucks, 1987), enabled the study to focus on the various forms of the innovation, including the innovation configuration, stages of concern, and the levels of use from the two given perspectives, teachers in Support Units and teachers in Special Schools, in relation to the major factors affecting implementation. The study findings highlighted that in both educational settings, change is accomplished by individuals and is a highly personal experience, demanding adequate support by facilitators of the change through appropriate actions, in order to assist effective and successful implementation of the change.
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Miner, M. H. "The human cost of Presbyterian identity : secularisation, stress and psychological outcomes for Presbyterian ministers in N.S.W. /." [Campbelltown, N.S.W. : The Author], 1996. http://library.uws.edu.au/adt-NUWS/public/adt-NUWS20030711.103044/index.html.

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Rowling, Jill. "Cave Aragonites of New South Wales." University of Sydney. Geosciences, 2004. http://hdl.handle.net/2123/694.

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Abstract Aragonite is a minor secondary mineral in many limestone caves throughout the world. It has been claimed that it is the second-most common cave mineral after calcite (Hill & Forti 1997). Aragonite occurs as a secondary mineral in the vadose zone of some caves in New South Wales. Aragonite is unstable in fresh water and usually reverts to calcite, but it is actively depositing in some NSW caves. A review of current literature on the cave aragonite problem showed that chemical inhibitors to calcite deposition assist in the precipitation of calcium carbonate as aragonite instead of calcite. Chemical inhibitors work by physically blocking the positions on the calcite crystal lattice which would have otherwise allowed calcite to develop into a larger crystal. Often an inhibitor for calcite has no effect on the aragonite crystal lattice, thus aragonite may deposit where calcite deposition is inhibited. Another association with aragonite in some NSW caves appears to be high evaporation rates allowing calcite, aragonite and vaterite to deposit. Vaterite is another unstable polymorph of calcium carbonate, which reverts to aragonite and calcite over time. Vaterite, aragonite and calcite were found together in cave sediments in areas with low humidity in Wollondilly Cave, Wombeyan. Several factors were found to be associated with the deposition of aragonite instead of calcite speleothems in NSW caves. They included the presence of ferroan dolomite, calcite-inhibitors (in particular ions of magnesium, manganese, phosphate, sulfate and heavy metals), and both air movement and humidity. Aragonite deposits in several NSW caves were examined to determine whether the material is or is not aragonite. Substrates to the aragonite were examined, as was the nature of the bedrock. The work concentrated on Contact Cave and Wiburds Lake Cave at Jenolan, Sigma Cave, Wollondilly Cave and Cow Pit at Wombeyan and Piano Cave and Deep Hole (Cave) at Walli. Comparisons are made with other caves. The study sites are all located in Palaeozoic rocks within the Lachlan Fold Belt tectonic region. Two of the sites, Jenolan and Wombeyan, are close to the western edge of the Sydney Basin. The third site, Walli, is close to a warm spring. The physical, climatic, chemical and mineralogical influences on calcium carbonate deposition in the caves were investigated. Where cave maps were unavailable, they were prepared on site as part of the study. %At Jenolan Caves, Contact Cave and Wiburds Lake Cave were examined in detail, %and other sites were compared with these. Contact Cave is located near the eastern boundary of the Late Silurian Jenolan Caves Limestone, in an area of steeply bedded and partially dolomitised limestone very close to its eastern boundary with the Jenolan volcanics. Aragonite in Contact Cave is precipitated on the ceiling as anthodites, helictites and coatings. The substrate for the aragonite is porous, altered, dolomitised limestone which is wedged apart by aragonite crystals. Aragonite deposition in Contact Cave is associated with a concentration of calcite-inhibiting ions, mainly minerals containing ions of magnesium, manganese and to a lesser extent, phosphates. Aragonite, dolomite and rhodochrosite are being actively deposited where these minerals are present. Calcite is being deposited where minerals containing magnesium ions are not present. The inhibitors appear to be mobilised by fresh water entering the cave as seepage along the steep bedding and jointing. During winter, cold dry air pooling in the lower part of the cave may concentrate minerals by evaporation and is most likely associated with the ``popcorn line'' seen in the cave. Wiburds Lake Cave is located near the western boundary of the Jenolan Caves Limestone, very close to its faulted western boundary with Ordovician cherts. Aragonite at Wiburds Lake Cave is associated with weathered pyritic dolomitised limestone, an altered, dolomitised mafic dyke in a fault shear zone, and also with bat guano minerals. Aragonite speleothems include a spathite, cavity fills, vughs, surface coatings and anthodites. Calcite occurs in small quantities at the aragonite sites. Calcite-inhibitors associated with aragonite include ions of magnesium, manganese and sulfate. Phosphate is significant in some areas. Low humidity is significant in two areas. Other sites briefly examined at Jenolan include Glass Cave, Mammoth Cave, Spider Cave and the show caves. Aragonite in Glass Cave may be associated with both weathering of dolomitised limestone (resulting in anthodites) and with bat guano (resulting in small cryptic forms). Aragonite in the show caves, and possibly in Mammoth and Spider Cave is associated with weathering of pyritic dolomitised limestone. Wombeyan Caves are developed in saccharoidal marble, metamorphosed Silurian Wombeyan Caves Limestone. Three sites were examined in detail at Wombeyan Caves: Sigma Cave, Wollondilly Cave and Cow Pit (a steep sided doline with a dark zone). Sigma Cave is close to the south east boundary of the Wombeyan marble, close to its unconformable boundary with effusive hypersthene porphyry and intrusive gabbro, and contains some unmarmorised limestone. Aragonite occurs mainly in a canyon at the southern extremity of the cave and in some other sites. In Sigma Cave, aragonite deposition is mainly associated with minerals containing calcite-inhibitors, as well as some air movement in the cave. Calcite-inhibitors at Sigma Cave include ions of magnesium, manganese, sulfate and phosphate (possibly bat origin), partly from bedrock veins and partly from breakdown of minerals in sediments sourced from mafic igneous rocks. Substrates to aragonite speleothems include corroded speleothem, bedrock, ochres, mud and clastics. There is air movement at times in the canyon, it has higher levels of CO2 than other parts of the cave and humidity is high. Air movement may assist in the rapid exchange of CO2 at speleothem surfaces. Wollondilly Cave is located in the eastern part of the Wombeyan marble. At Wollondilly Cave, anthodites and helictites were seen in an inaccessible area of the cave. Paramorphs of calcite after aragonite were found at Jacobs Ladder and the Pantheon. Aragonite at Star Chamber is associated with huntite and hydromagnesite. In The Loft, speleothem corrosion is characteristic of bat guano deposits. Aragonite, vaterite and calcite were detected in surface coatings in this area. Air movement between the two entrances of this cave has a drying effect which may serve to concentrate minerals by evaporation in some parts of the cave. The presence of vaterite and aragonite in fluffy coatings infers that vaterite may be inverting to aragonite. Calcite-inhibitors in the sediments include ions of phosphate, sulphate, magnesium and manganese. Cave sediment includes material sourced from detrital mafic rocks. Cow Pit is located near Wollondilly Cave, and cave W43 is located near the northern boundary of the Wombeyan marble. At Cow Pit, paramorphs of calcite after aragonite occur in the walls as spheroids with minor huntite. Aragonite is a minor mineral in white wall coatings and red phosphatic sediments with minor hydromagnesite and huntite. At cave W43, aragonite was detected in the base of a coralloid speleothem. Paramorphs of calcite after aragonite were observed in the same speleothem. Dolomite in the bedrock may be a source of magnesium-rich minerals at cave W43. Walli Caves are developed in the massive Belubula Limestone of the Ordovician Cliefden Caves Limestone Subgroup (Barrajin Group). At the caves, the limestone is steeply bedded and contains chert nodules with dolomite inclusions. Gypsum and barite occur in veins in the limestone. At Walli Caves, Piano Cave and Deep Hole (Deep Cave) were examined for aragonite. Gypsum occurs both as a surface coating and as fine selenite needles on chert nodules in areas with low humidity in the caves. Aragonite at Walli caves was associated with vein minerals and coatings containing calcite-inhibitors and, in some areas, low humidity. Calcite-inhibitors include sulfate (mostly as gypsum), magnesium, manganese and barium. Other caves which contain aragonite are mentioned. Although these were not major study sites, sufficient information is available on them to make a preliminary assessment as to why they may contain aragonite. These other caves include Flying Fortress Cave and the B4-5 Extension at Bungonia near Goulburn, and Wyanbene Cave south of Braidwood. Aragonite deposition at Bungonia has some similarities with that at Jenolan in that dolomitisation of the bedrock has occurred, and the bedding or jointing is steep allowing seepage of water into the cave, with possible oxidation of pyrite. Aragonite is also associated with a mafic dyke. Wyanbene cave features some bedrock dolomitisation, and also features low grade ore bodies which include several known calcite-inhibitors. Aragonite appears to be associated with both features. Finally, brief notes are made of aragonite-like speleothems at Colong Caves (between Jenolan and Wombeyan), a cave at Jaunter (west of Jenolan) and Wellington (240\,km NW of Sydney).
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Keogh, Andrew James, of Western Sydney Hawkesbury University, Faculty of Science and Technology, and School of Applied and Environmental Sciences. "Systems management of Glenbrook Lagoon, New South Wales." THESIS_FST_AES_Keogh_A.xml, 1996. http://handle.uws.edu.au:8081/1959.7/423.

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Glenbrook Lagoon, an 8 hectare lake receiving rainfall runoff from a residential catchment, is experiencing nutrient enrichment problems expressed as excessive aquatic plant presence. This study aims to assess the relative nutrient contribution of the total system compartments, including catchment loading, water column, aquatic plants and surface sediment. This information is utilised in the formulation of management strategies which may produce a sustainable nutrient reduction and general improvement in the system. The total nutrient content of the aquatic system was determined to be high in comparison with the present nutrient loading from the catchment. The ideal management case considers nutrient reduction of the surface sediment compartment firstly, followed by the aquatic plant community, with the water column and catchment influence as relatively low priority compartments. Various strategies for managing these are proposed. The total system benefits of the ideal management case are reductions in nutrients, aquatic plant biovolume and suspended solid loading. Unavoidable constraints placed upon the ideal management case include the excessive aquatic plant presence restricting accessability to the surface sediment for dredging. The resulting best management case requires aquatic plant eradication prior to sediment management, with the total system benefits associated with the ideal management case being retained.
Master of Science (Hons)
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Elliott, Malcolm Gordon, of Western Sydney Hawkesbury University, and Faculty of Environmental Management and Agriculture. "Grass tetany of cattle in New South Wales." THESIS_FEMA_xxx_Elliott_M.xml, 2000. http://handle.uws.edu.au:8081/1959.7/7.

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Over the last 60 years, grass tetany has been recognised as a significant lethal condition in sheep and cattle.Outcomes from this study include documentation of the likely precursors to grass tetany, ways to recognise these precursors, and long term practices that will enable producers to minimise livestock deaths. The benefit of this research to beef producers is that the environmental circumstances thought to be associated with outbreaks of grass tetany have been identified, along with remedial action that can be taken to prevent deaths occurring.Recommendations to industry on best practice to be adopted by leading producers to minimise outbreaks of grass tetany are made.This study provides an alternate strategy for the management of grass tetany in beef cattle, to the more clinical approaches previously recommended. It is suggested that losses from this economically important metabolic disease can be minimised if management practices of beef cattle producers in eastern Australia can incorporate a more holistic approach to farm management, which takes account of the soil/plant/animal/climate inter-relationships.
Master of Science (Hons)
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10

Wood, Susan, and s2000093@student rmit edu au. "Creative embroidery in New South Wales, 1960 - 1975." RMIT University. Architecture and Design, 2006. http://adt.lib.rmit.edu.au/adt/public/adt-VIT20070206.160246.

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In the years between 1960 and 1975 in NSW there emerged a loosely connected network of women interested in modern or creative embroidery. The Embroiderers' Guild of NSW served as a focus for many of these women, providing opportunities for them to exhibit their work, and to engage in embroidery education as teachers or as learners. Others worked independently, exhibited in commercial galleries and endeavoured to establish reputations as professional artists. Some of these women were trained artists and wanted embroidery to be seen as 'art'; others were enthusiastic amateurs, engaged in embroidery as a form of 'serious leisure'. They played a significant role in the development of creative embroidery and textile art in NSW and yet, for the most part, their story is absent from the narratives of Australian art and craft history. These women were involved in a network of interactions which displayed many of the characteristics of more organised art worlds, as posite d by sociologist Howard Becker. They produced work according to shared conventions, they established co-operative links with each other and with other organisations, they organised educational opportunities to encourage others to take up creative embroidery and they mounted exhibitions to facilitate engagement with a public audience. Although their absence from the literature suggests that they operated in isolation, my research indicates that there were many points of contact between the embroidery world, the broader craft world and the fine art community in NSW. This thesis examines the context in which creative embroiderers worked, discusses the careers of key individuals working at this time, explores the interactions between them, and evaluates the influence that they had on later practice in embroidery and textiles in NSW.
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Books on the topic "New South Wales coast"

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Gleeson, Max. Shipwrecks, storms & seamen of the New South Wales Coast. Caringbah, N.S.W: Max Gleeson, 1996.

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Coast: A history of the New South Wales edge. Sydney, N.S.W: NewSouth Publishing, University of New South Wales Press, 2013.

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Nayutah, Jolanda. Our land, our spirit: Aboriginal sites of North Coast, New South Wales. Lismore, N.S.W: North Coast Institute for Aboriginal Community Education, 1988.

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Neil, Thomson. Identification of aborigines in hospital admissions in the North Coast Health Region, New South Wales. [N.S.W.]: Australian Institute of Health and North Coast Health Region of the New South Wales Department of Health, 1990.

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Tibby, John. A mid- to late-Holocene diatom and pollen palaeoecology of the Tuross Lake system, South Coast, New South Wales. Clayton, Vic., Australia: Dept. of Geography and Environmental Science, Monash University, 1996.

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Australian Beach Safety and Management Program., Surf Life Saving Australia, and University of Sydney. Coastal Studies Unit., eds. Beaches of the New South Wales coast: A guide to their nature, characteristics, surf and safety. 2nd ed. Sydney: Sydney University Press, 2007.

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Short, Andrew D. Beaches of the New South Wales coast: A guide to their nature, characteristics, surf, and safety. Sydney, NSW: Coastal Studies Unit, University of Sydney, 1993.

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Ryan, John Julian. The land of Ulitarra: Early records of the aborigines of the mid-north coast of New South Wales. Lismore: New South Wales Dept. of Education North Coast Regional Office, 1988.

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Jackson, R. V. Jeremy Bentham on the cost of the convict colony in New South Wales. Canberra, Australia: Australian National University, 1986.

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Connolly, Brendan. Paddocks, palaces, and picture shows: The colourful history of the cinemas of the Central Coast of New South Wales. Campbelltown, NSW: Australian Cinema and Theatre Society, 1996.

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Book chapters on the topic "New South Wales coast"

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Burr, Andrew, Anne Eckenroth, Ruta Kersyte, and Kesarin Jaitham. "Australia: The East Coast model (with New South Wales as the principal legislation)." In International Contractual and Statutory Adjudication, 34–71. New York, NY : Informa Law from Routledge, 2017. | Series: Construction practice series: Informa Law from Routledge, 2017. http://dx.doi.org/10.4324/9781315294537-3.

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Mahony, M. J. "The status of frogs in the Watagan Mountains area the Central Coast of New South Wales." In Herpetology in Australia, 257–64. P.O. Box 20, Mosman NSW 2088, Australia: Royal Zoological Society of New South Wales, 1993. http://dx.doi.org/10.7882/rzsnsw.1993.039.

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Adam, Paul. "Planning for the future of the New South Wales coast: history and science in the quest for certainty." In Conserving Marine Environments, 49–54. P.O. Box 20, Mosman NSW 2088, Australia: Royal Zoological Society of New South Wales, 2003. http://dx.doi.org/10.7882/fs.2003.006.

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White, A. W. "Ecological and behavioural observations on populations of the toadlets Pseudophryne coriacea and Pseudophryne bibronii on the Central Coast of New South Wales." In Herpetology in Australia, 139–50. P.O. Box 20, Mosman NSW 2088, Australia: Royal Zoological Society of New South Wales, 1993. http://dx.doi.org/10.7882/rzsnsw.1993.021.

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Thom, Bruce. "New South Wales." In Encyclopedia of the World's Coastal Landforms, 1229–38. Dordrecht: Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-1-4020-8639-7_225.

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Plowman, David, and Keri Spooner. "Unions in New South Wales." In Australian Unions, 104–21. London: Macmillan Education UK, 1989. http://dx.doi.org/10.1007/978-1-349-11088-9_5.

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Wallace, Valerie. "Republicanism in New South Wales." In Scottish Presbyterianism and Settler Colonial Politics, 219–44. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-70467-8_10.

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Laidlaw, Ronald W. "New South Wales 1821–51." In Mastering Australian History, 96–120. London: Macmillan Education UK, 1988. http://dx.doi.org/10.1007/978-1-349-09168-3_5.

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Frahm, Michael. "Australia: Ombudsman New South Wales." In Australasia and Pacific Ombudsman Institutions, 117–29. Berlin, Heidelberg: Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-33896-0_8.

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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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Conference papers on the topic "New South Wales coast"

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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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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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"Modelling hydrological changes in New South Wales under future climate change." In 21st International Congress on Modelling and Simulation (MODSIM2015). Modelling and Simulation Society of Australia and New Zealand, 2015. http://dx.doi.org/10.36334/modsim.2015.g4.young.

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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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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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Duc, Hiep Nguyen, Sean Watt, David Salter, and Toan Trieu. "Modelling October 2013 Bushfire Pollution Episode in New South Wales, Australia." In 31st International Symposium on Automation and Robotics in Construction. International Association for Automation and Robotics in Construction (IAARC), 2014. http://dx.doi.org/10.22260/isarc2014/0072.

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Fityus, Stephen, and J. Gibson. "Rock Mass Stability in the Southern New England Fold Belt, New South Wales, Australia." In First Southern Hemisphere International Rock Mechanics Symposium. Australian Centre for Geomechanics, Perth, 2008. http://dx.doi.org/10.36487/acg_repo/808_57.

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Reports on the topic "New South Wales coast"

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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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Garthwaite, M. C., and T. Fuhrmann. Subsidence monitoring in the Sydney Basin, New South Wales: results of the Camden Environmental Monitoring Project. Geoscience Australia, 2020. http://dx.doi.org/10.11636/record.2020.016.

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