Relevant bibliographies by topics / New South Wales Southern Highlands

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Academic literature on the topic 'New South Wales Southern Highlands'

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Published: 4 June 2021
Last updated: 5 February 2022

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Journal articles on the topic "New South Wales Southern Highlands"

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Read, Roger W. "Highlights of the 2009 New South Wales Southern Highlands Conference on Heterocyclic Chemistry." Australian Journal of Chemistry 63, no. 5 (2010): 725. http://dx.doi.org/10.1071/ch10182.

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Meetings that foster interaction between academic and industrial researchers, both operating at the forefront of science, serve to stimulate ideas and allow partnerships to develop. The Southern Highlands Conference brings together experts in the field of heterocyclic chemistry and, in this issue, some of the most recent advances are highlighted (The figure shows 2009 Conference student speakers with President Barbara Messerle).
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Morrison, Mark, and Michael Lockwood. "Informing Program Design for Connectivity Conservation in the New South Wales Southern Highlands, Australia." Society & Natural Resources 27, no. 1 (November 5, 2013): 70–87. http://dx.doi.org/10.1080/08941920.2013.840814.

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Cook, IO, and PY Ladiges. "Morphological variation within Eucalyptus nitens s. lat. and recognition of a new species, E. denticulata." Australian Systematic Botany 4, no. 2 (1991): 375. http://dx.doi.org/10.1071/sb9910375.

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The complete geographic range of Eucalyptus nitens s. lat. (shining gum) was sampled to determine the pattern of variation in adult and seedling morphology. Analyses of the different data sets indicated the presence of two distinct taxa: one, characterised by denticulate adult leaf margins, is described as E. denticulata sp. nov.; the other, characterised by entire leaf margins, is E. nitens s. str. Many other characters distinguish the two taxa. Mature trees of E. denticulata have leaves with higher oil gland density, longer peduncles, more cup-shaped rather than barrel-shaped fruit, more frequently exserted valves, and rounded and longer flower buds compared with E. nitens s. str. Seedlings of the two species can be distinguished mainly on the basis that those of E. denticulata have longer internodes and leaves which clasp the stem to a lesser extent. The major occurrence of E. denticulata is on the Errinundra Plateau, East Gippsland, with limited occurrences in the Baw Baw Ranges and Central Highlands of Victoria. Eucalyptus nitens s. str. is found in isolated stands in New South Wales and Victoria. The two species are allopatric, with the exception of the Baw Baw Ranges and Central Highlands of Victoria where some stands are mixed. Eucalyptus nitens s. str. is also geographically variable, comprising three distinct geographic races: northern and central New South Wales, southern New South Wales, and the Baw Baw Ranges and Central Highlands of Victoria.
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Stevenson, M. A. "Disease incidence in dairy herds in the southern highlands district of New South Wales, Australia." Preventive Veterinary Medicine 43, no. 1 (January 2000): 1–11. http://dx.doi.org/10.1016/s0167-5877(99)00082-3.

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CONYERS, M. K., and B. G. DAVEY. "THE VARIABILITY OF pH IN ACID SOILS OF THE SOUTHERN HIGHLANDS OF NEW SOUTH WALES." Soil Science 150, no. 4 (October 1990): 695–704. http://dx.doi.org/10.1097/00010694-199010000-00004.

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Chenhall, Bryan E., Brian G. Jones, and Paul F. Carr. "Contact metamorphism of pelitic, psammitic and calcareous sediments in the Southern Highlands of New South Wales." Australian Journal of Earth Sciences 35, no. 3 (September 1988): 389–401. http://dx.doi.org/10.1080/08120098808729456.

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Murphy, Michael J. "The butterfly fauna of the Pilliga Forest, a large woodland remnant in the Brigalow Belt South bioregion in northern inland New South Wales, Australia." Pacific Conservation Biology 25, no. 2 (2019): 193. http://dx.doi.org/10.1071/pc18002.

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Sixty-three butterfly species representing five families have been recorded from the Pilliga Forest in northern inland New South Wales – the largest surviving remnant of native forest on the western slopes of the Great Dividing Range. This is one of the richest recorded butterfly faunas of any location on the New South Wales western slopes and adjacent plains, reflecting the location of the Pilliga Forest in a biogeographic overlap zone between northern and southern faunal assemblages with proximity to both the western plains and outliers of the mesic eastern highlands. No narrow-range endemic species or species of state or national conservation concern were recorded; however, half of the species recorded have patchy, discontinuous distributions within their broad range due to specific habitat requirements. Some minor western range extensions are recorded and two hilltopping sites are documented. This study highlights the significant biodiversity conservation value of the Pilliga Forest in the predominantly cleared western slopes bioregions.
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Norton, Melinda A., Andrew W. Claridge, Kris French, and Alison Prentice. "Population biology of the long-nosed potoroo (Potorous tridactylus) in the Southern Highlands of New South Wales." Australian Journal of Zoology 58, no. 6 (2010): 362. http://dx.doi.org/10.1071/zo10075.

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The population biology of the long-nosed potoroo (Potorous tridactylus) was investigated at Barren Grounds Nature Reserve and Budderoo National Park in the Southern Highlands of New South Wales (NSW). Both study areas are important conservation reserves for this threatened species, with a large gap north (~300 km) to the next known viable population on the mid-north coast of NSW at Mount Royal. Potoroos were live-trapped using bandicoot-sized cage traps, each set ~100 m apart along walking tracks and fire trails. Trapping was conducted each autumn and spring over five years to enumerate the local population of potoroos and to describe their morphometrics. The local long-nosed potoroos were larger in size than those recorded to the south on mainland Australia, but smaller than those in north-eastern NSW, supporting the concept of a latitudinal cline in body size. Sexual dimorphism was observed, with adult males having larger body weights, head lengths and pes lengths. Between one-third and two-thirds of all males and females were captured in only a single trapping session, indicative of low levels of survivorship and/or high levels of dispersal or transience. Males regularly overlapped at trap sites with females, more so than with other males, while females rarely overlapped at trap sites. Barren Grounds Nature Reserve supported a larger number of potoroos and a greater degree of home range overlap between individuals.
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Catibog-Sinha, Corazon. "Visitor Impact and Biodiversity: A Monitoring Framework for Protected Areas in Southern Highlands, New South Wales, Australia." Asia Pacific Journal of Tourism Research 13, no. 3 (September 2008): 245–63. http://dx.doi.org/10.1080/10941660802280364.

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McCormack, Robert B. "Conservation of imperiled crayfish, Euastacus dharawalus (Decapoda: Astacidea: Parastacidae), from the southern highlands of New South Wales, Australia." Journal of Crustacean Biology 33, no. 3 (January 1, 2013): 432–39. http://dx.doi.org/10.1163/1937240x-00002138.

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Dissertations / Theses on the topic "New South Wales Southern Highlands"

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Roach, Ian C., and n/a. "The setting, structural control, geochemistry and mantle source of the Monaro Volcanic Province, southeastern New South Wales." University of Canberra. Applied Science, 1999. http://erl.canberra.edu.au./public/adt-AUC20061107.131113.

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The Monaro Volcanic Province (MVP) is an Oligocene-Eocene intraplate basaltic lava field situated in the Southern Highlands of New South Wales between the towns of Cooma and Bombala. The lava pile of the MVP consists of basal sub-alkali rocks (olivine tholeiite, transitional basalt) capped by a number of thick ankaramite lavas, above which lie less numerous alkali rocks including alkali olivine basalt, nepheline basanite and olivine nephelinite. Intercalated with the lava flows are massive and matrix-supported alkali and ankaramitic hyaloclastites, alkali pillow basalts, rare tuffs, bauxitic weathering profiles, lacustrine sediments and reworked late Cretaceous to early Tertiary river gravels. The lava pile is intruded through by numerous volcanic plugs and dykes and rare maars. Volcanic centres are principally concentrated in two NW-SE trending zones parallel to major crustal-scale fractures in the Palaeozoic basement. Centres almost always lie over the intersections of two or more conjugate strike-slip or transverse fractures. The stratigraphy, whole-rock geochemistry and Sr and Nd isotopic signatures of rocks from the MVP indicate magma-genesis initially from an asthenospheric source with EM1 characteristics, gradually becoming more lithospheric with DM source characteristics. The long-lived nature of the MVP rules out a mantle plume-type source for magmas. Instead, a diapiric source is envisaged. The MVP mantle xenolith suite appears to have equilibrated at slightly higher temperatures for given pressures than the Newer Volcanics Province suite suggesting the palaeogeotherm for the MVP was slightly hotter than the "South East Australian" geotherm. Large amounts of amphibole (pargasitic hornblende, pargasite, ferroan pargasite and kaersutite) occuring within the more silica-undersaturated rocks of the MVP, and rarely within Iherzolitic xenoliths, are interpreted to have formed as selvages on mantle veins in contact with peridotite beneath the MVP. Amphiboles were later sampled by magmas rising through the same conduits and were brought to the surface. MVP ankaramite lavas feature < 2cm clinopyroxene porphyrocrysts, the cores of which are shown to have crystallised at ca. 18 kb pressure or ca. 54 km depth. This defines the base of the local crust within the MVP region. Data from the MVP support a landscape evolution model based on the isostatic rise of the Southern Highlands due to voluminous magmatic underplating since the Cretaceous. Data further support limited denudation since the Early Tertiary based on a pulsatory but high palaeogeotherm.
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King, Alison Jane 1974. "Recruitment ecology of fish in floodplain rivers of the southern Murray-Darling Basin, Australia." Monash University, Dept. of Biological Sciences, 2002. http://arrow.monash.edu.au/hdl/1959.1/8391.

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Hunter, David, and n/a. "Conservation Management of Two Threatened Frog Species in South-Eastern New South Wales, Australia." University of Canberra. Applied Science, 2007. http://erl.canberra.edu.au./public/adt-AUC20081020.142239.

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The decline and extinction of amphibian species over the past three decades is widely acknowledged as one of the greatest biodiversity crises of modem time. Providing convincing data to support hypotheses about these declines has proved difficult, which has greatly restricted the development and implementation of management actions that may prevent further amphibian declines and extinctions from occurring. In this thesis, I present research that was undertaken as part of the recovery programs for the southern corroboree frog (Pseudophryne corroboree), and the Booroolong frog (Litoria booroolongensis); two species that underwent very rapid declines in distribution and abundance during the 1980's. More specifically, I investigated potential causal factors in the declines of both species using experimental and correlative studies, and examined the mechanisms by which one threatening process (chytridiomycosis) may be causing continued decline and extinction in P. corroboree. I also examined the implications of population dynamics for monitoring L. booroolongensis, and suggest a possible monitoring strategy that may reliably facilitate the implementation of recovery objectives for this species. I also tested one possible reintroduction technique aimed at preventing the continued decline and extinction of P. corroboree populations. In Chapters 2 and 3, I present the results from a series of experiments in artificial enclosures designed to examine whether the tadpoles of L. booroolongensis are susceptible to predation by co-occurring introduced predatory fish species; brown trout (Salmo trutta), rainbow trout (Oncorhynchus mykiss), European carp (Cyprinus carpio), redfin perch (Percafluviatilis), and mosquito fish (Gambusia holbrooki). I demonstrated that the tadpoles of L. booroolongensis, and a closely related species Litoria lesueuri, were palatable to non-native trout species, but not to two native predatory fish species, Gadopsis bispinosus and Galaxias olidus. A pond breeding frog species included in this experiment, Limnodynastes tasmaniensis, was palatable to both the native and non-native fish species. In a separate experiment I also demonstrated that the tadpole of L. booroolongensis is palatable to the three other introduced fish species examined in this study; C. carpio, P. fluviatilis, and G. holbrooki. In three of the experiments, the provision of rock within enclosures as a potential refuge habitat did not afford protection to L. booroolongensis tadpoles from predation by any of the five introduced fish species examined. While all the introduced fish species tested here did consume L. booroolongensis tadpoles, the results also suggested that chemical unpalatability might afford some level of protection against some of these fish species. Firstly, the addition of alternative prey items in one of the experiments reduced the proportion of tadpoles consumed, suggesting that L. booroolongensis may not be a preferred prey item. Secondly, the proportion of tadpoles consumed varied greatly among the different fish species examined, suggesting differing levels of palatability. Overall, this study supports previous research in suggesting that chemical unpalatability may be an important strategy for the tadpoles of riverine frog species in south-eastern Australia to avoid predation by native fish species, and that this strategy is less effective against introduced fish species. While L. booroolongensis currently persists in streams inhabited by a number of introduced fish species, this study supports the likelihood that these species are having a negative impact on populations of L. booroolongensis in the wild. In Chapter 4, I present the results of a study aimed at examining potential monitoring techniques for L. booroolongensis. The results of a mark-recapture exercise demonstrated that L. booroolongensis may exhibit large fluctuations in abundance from one year to the next, and through a prospective power analysis approach, I demonstrated that it would be difficult to confidently identify population trends of interest using either indices or estimates of abundance for this species. An assessment of the capacity to identify the presence or absence of L. booroolongensis using nighttime spotlight surveys demonstrated the high detectability of this species using this technique, at both the scale of 300-meter sections of stream and individual breeding areas (typically less than 10-meters of stream). This study suggests that the monitoring objectives of the L. booroolongensis recovery program would be most effectively achieved using presence/absence surveys at different scales. In Chapter 5, I present the results of a field survey aimed at determining the current distribution and habitat requirements of L. booroolongensis in the South West Slopes region of New South Wales. Of the 163 sites I surveyed across 49 streams,I located L. booroolongensis along 77 of these sites from 27 streams. Based on population and habitat connectivity, this study identified 18 populations of L. booroolongensis that are likely to be operating as independent populations. Twelve of these populations are not represented in conservation reserves, but rather occur along streams that flow through the agricultural landscape. A broad scale habitat analysis identified a positive relationship between extent of rock structures along the stream and the occurrence of L. booroolongensis, and a negative relationship between the proportion of canopy cover and this species' occurrence. At the breeding habitat scale, this study identified a positive relationship between the presence of breeding males and; number of rock crevices in the aquatic environment, extent of emergent rocks, and proportion pool. This analysis also detected a negative relationship between occupancy and water depth. These results confirm previous work suggesting the importance of rocky stream habitats to the persistence of L. booroolongensis, but also suggest how disturbance processes, such as increasing sedimentation and weed invasion, may reduce the suitability of rocky structures as breeding sites. In Chapter 6, I investigated current levels of amphibian chytrid fungus (Batrachochytrium dendrobatidis) infection in corroboree frog populations, and used retrospective screening of museum specimens to assess the possibility that this pathogen was implicated in the initial decline of the corroboree frogs. Using histology, I did not detect any B. dendrobatidis infections in corroboree frog populations prior to their decline, however using the same technique, moderate levels of infection were detected in post-decline populations of both species. Real-time PCR screening of skin swabs identified much higher overall infection rates in post-decline populations of P. corroboree (between 44% and 59%), while significantly lower rates of infection were observed in P. pengilleyi populations (14%). These results suggest that the initial and continued decline of the corroboree frogs may well be attributed to the emergence of B. dendrobatidis in populations of these species. In Chapter 7, I investigated how B. dendrobatidis may be causing the continued decline of P. corroboree through the presence of an abundant reservoir host for this pathogen. I found that populations of adult C. signifera in sub-alpine bogs carry high B. dendrobatidis infection rates (86%), but appear unaffected by this infection. An experiment involving the release of P. corroboree tadpoles into 15 natural pools resulted in metamorphs from seven of these pools testing positive for B. dendrobatidis, with all these individuals dying soon after metamorphosis. These results support the possibility that B. dendrobatidis infection in P. corroboree populations is being facilitated by the presence of large numbers of infected C. signifera in the shared environment. Chapter 8 presents the results of a population augmentation study for P. corroboree. I investigated the extent to which increasing recruitment to metamorphosis may result in population recovery in this species. This was undertaken by harvesting eggs from the field and rearing them through to mid stage tadpoles over the winter period prior to being released back to their natal ponds in spring. While I was able to increase recruitment to metamorphosis by an average of 20 percent, this did not result in a noticeable influence on the subsequent adult population size, as both manipulated and non-manipulated sites declined over the course of this study by an average of 80 percent. I observed a positive relationship between natural recruitment to a late tadpole stage and subsequent adult male population size, however there was considerable variation associated with this relationship. The relationship between recruitment and subsequent population size at the augmentation sites was consistent with the relationship observed at the non-manipulated sites. These results suggest that recruitment to metamorphosis may not be the most important life stage restricting the population recovery of P. corroboree, but that mortality during post-metamorphic stages may be more important in regulating current population size. Hence, further attempts to use captive rearing to increase P. corroboree populations in the wild should focus on the release of post-metamorphic frogs. Overall, this thesis demonstrates the value of quantitative research to the implementation and progress of threatened species recovery programs. While this research will specifically contribute to the recovery programs for L. booroolongensis and P. corroboree, it more broadly contributes to the understanding and capacity to respond to the concerning levels of amphibian extinctions currently occurring throughout the world.
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Wozga, Miroslaw Jacek. "Investigation of local fold plunge reversals present at Pasminco's Southern Operations, Broken Hill, New South Wales, Australia /." Title page, table of contents and abstract only, 1991. http://web4.library.adelaide.edu.au/theses/09SB/09sbw938.pdf.

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Figueroa, David. "Food web dynamics : new patterns from southern South America and North Wales UK, and the role of basal species structuring food webs." Thesis, Queen Mary, University of London, 2007. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.582554.

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Food webs, defined as "who eats whom" in nature, have become a central topic within community ecology and thus they have been used to understand general ecological patterns such as biodiversity and species interactions as well as material and nutrient flows within ecosystems. In South America the knowledge of the taxonomy and distribution of freshwater invertebrates is incomplete and fragmented. Previous studies have focused on specific taxonomic groups and some countries such as Brazil and Argentina. In contrast, there have been many aquatic food webs published for UK freshwater systems with high levels of taxonomic resolution. This thesis aims to examine food web patterns in two geographically separated systems. The effects of systematic taxonomic aggregation on food web properties were examined and the relationship between consumer and prey body size revisited. A total of 24 food webs were examined in Chilean and Welsh streams, where 6128 invertebrate guts were examined to establish feeding interactions. These Chilean and Welsh food webs are amongst the largest, most complete and fully resolved. In both systems there was a high proportion of basal species, combined with low proportions of top and intermediate species. Significant differences were detected in most food web properties, in comparison to previous studies, where basal species were aggregated to coarser categories. No significant relationship between the body size of the consumers and their prey was found in either Chilean or Welsh streams. These results differ substantially from published data, and we attribute these differences to the greater taxonomic resolution particularly on the basal resources.
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Katijua, Mutjinde, and n/a. "The effects of remnant patches of Eucalyptus open woodlands on the composition, quality and production of native pastures on the Southern Tablelands." University of Canberra. Resource, Environmental & Heritage Sciences, 1997. http://erl.canberra.edu.au./public/adt-AUC20060807.130528.

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Clearance of Eucalyptus woodlands has resulted in soil deterioration and lost agricultural production, due to wind erosion, salinity and soil acidity. Despite increasing efforts to reverse these trends through Landcare and other revegetation and agroforestry programs, there is a lack of experimentally-based information about the effects of trees on native pasture performance. The study was carried out in a temperate environment (Southern Tablelands, New South Wales). The altitude at the study sites ranged from 740 to 880m and the aspect at the experimental plots varied from SE to SW. The nearest site was 16 km from Canberra Airport and all sites were situated within similar rainfall isohyets as Canberra Airport. Thus climatic conditions were expected to be similar. Climate records at Canberra Airport indicate that January is the hottest month with mean maximum temperature of 27.7 �C and July is the coldest month with a maximum of 11.1 �C. Rainfall in the area ranges from 37.5 to 66.0 mm monthly average in June and October respectively. The main tree species in the study area were Eucalyptus pauciflora, E. melliodora and E. mannifera. Furthermore, Poa labillardieri, P. sieberiana, Themeda australis, Danthonia penicillata and Microlaena stipoides were the most abundant pasture species on the experimental plots. Species of clover (Trifolium spp.) were also abundant among the herbs. This study used pasture assessment techniques to quantify the effects of remnant patches of Eucalyptus open woodlands on the composition, quality and biomass production of herbaceous understorey vegetation. Microclimate and soil nutrients were also compared under trees and in the open. In addition, consumption by vertebrate grazers under Eucalyptus trees and in the open was compared. Tree density and basal area were compared with herbage standing crop. Remnant patches of Eucalyptus open woodlands modify the microclimate by reducing wind reaching the understorey vegetation. However no significant effects on ambient air temperature and relative humidity were recorded. The effect of trees on soil moisture was contingent to differences between the four sites and soil depth. Despite a 13% higher soil organic matter in the top 15 cm of soil under trees, soil total nitrogen and total phosphorus did not differ from that in the open. Surface soil pH values were lower (by 0.2 units) under the trees. No significant effect of trees on pasture species richness was found. However the classification of quadrats on the basis of species presence showed a distinction between species composition under trees and in the open at one of the four sites. vi The contribution of pasture species to total dry weight on plots under trees and in the open did depend on the particular species involved and was also contingent to differences between sites. However at the sites where Vulpia bromoides and Poa sieberiana were abundant, the two species dominated the biomass under trees. Whereas Microlaena stipoides var. stipoides dominated the biomass under trees at two sites and in the open at only one of the four sites. Pasture total N content differed between sites. Two of the sites had significantly higher (5.9% and 19.7%) N content under trees. On the contrary, pastures at one site contained 18.7% higher N content in the open. The total P content was 18% higher in pastures under trees. Overall, the pasture standing crop under trees was 15% less than in the open during August to May. Vertebrate grazers consumed about the same amount of pasture under the trees and in the open at the four experimental sites.
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Brown, Peter Robert, and n/a. "Pasture response following rabbit control on grazing land." University of Canberra. Resource & Environmental Science, 1993. http://erl.canberra.edu.au./public/adt-AUC20061113.144813.

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The experiments described in this thesis were designed to assess changes in pasture dynamics (biomass and species composition of pasture) of grazing land on the Southern Tablelands of ACT and NSW, after 16 combinations of rabbit control treatments had been applied. The rabbit control performed by CSIRO Division of Wildlife and Ecology consisted of all combinations of presence-absence of Poisoning (using sodium monofluoroacetate, 1080: POIS), Ripping (ripping warrens using a tractor fitted with ripping tynes: RIP), Fumigation (pressure fumigation using chloropicrin: FUM) and repeated follow-up fumigation (using phostoxin pellets one, six and eighteen months after completion of the initial treatment: ANN). The pasture was assessed before treatments were applied, and every six months after rabbit control treatments. Treatment combinations were assigned randomly in a 24 factorial design on a total of 32 sites. There was a significant increase of pasture biomass at the RIP+ANN treatment at post-treatment sample 5. The analysis of covariance did not detect any other significant increase or decrease of pasture biomass for any rabbit control treatment, at any posttreatment sample. A significant increase of grass species occurred for the treatments of POIS+RIP+FUM, POIS and RIP+ANN for the post-treatment samples of 1, 3 and 5 respectively. There was a significant increase of thistles at the rabbit control treatments of POIS+RIP+FUM+ANN (post-treatment sample 1), RIP, ANN, RIP+FUM, RIP+FUM+ANN and POIS+RIP+FUM+ANN (post-treatment sample 3) and RIP and FUM+ANN (post-treatment sample 5). A significant increase of weeds occurred at FUM (post-treatment sample 3) and at FUM+ANN (post-treatment sample 5). No significant changes in the amount of herbs or legumes was apparent for any rabbit control treatment or post-treatment sample. There were no significant decreases for any species group. Except for the significant results for post-treatment sample 1, all significant increases of biomass for any species group occurred during spring (post-treatment sample 3 and 5) which suggests a growth phase during spring then subsequent dieback (particularly for thistles and weeds), as any change was not detected in the following autumn sample. No strong trend is evident for any particular rabbit control treatments, or any combination of treatments. Analysis of covariance revealed that the rabbit control treatment of RIP+ANN showed significant increases in both total biomass of pasture and grass biomass during post-treatment sample 5. This treatment reduced the number of active entrances the most. Significant positive correlations were found between pasture biomass (total) with grass, herb, legume, thistle and weed species groups. Significant negative correlations between grass biomass and the number of active entrances were found when the rabbit control had been highly effective in reducing the number of active entrances. When rabbit control had not been very successful, there was a significant positive but low correlation with the number of active entrances. There was no significant relationship between the number of active entrances with the weight of rabbit dung pellets. It is reasoned that they are different measures of rabbit abundance. More rabbit dung pellets were found closer to the warren than further away from the warren, but there was no correlation between rabbit dung and pasture biomass. Rainfall was above average for most of the experiment, biomass increased accordingly, and rabbit control was highly successful. The resulting changes in the pasture were difficult to detect, although some increases in species composition groups occurred. It is reasoned that the changes observed are partly attributable to seasonal conditions, and to high rainfall. Grazing by domestic animals, sheep and cattle, had been found to be consistent throughout the experiment.
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Harrison, Steve, University of Western Sydney, College of Arts, and Centre for Cultural Research. "An examination of the geological resources of the Southern Highlands of NSW as raw materials for studio ceramics." 2007. http://handle.uws.edu.au:8081/1959.7/29709.

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An investigation of the geological resources of the Southern Highlands was undertaken and over two hundred samples were collected and examined for possible use as stoneware ceramic ingredients. Thirty four of these samples were tested for possible use as clay body ingredients, while sixty five samples were selected for assessment as glaze ingredients. A wood fired kiln was built from firebricks produced from a local deposit of a white bauxite related material. Materials selected as a result of these tests were combined to create ceramic objects fired at stoneware temperatures. The most interesting result of the investigation was the discovery of a number of small weathered dykes and sills, samples from which were developed into workable ceramic clay bodies and glazes using a simple empirical testing procedure. A previously unknown excellent white translucent native porcelain stone or ‘bai tunze’ was discovered and developed into a workable porcelain body. Some iron stained porcelain bodies that ‘flashed’ red in the wood firing kiln were also developed. Exhibitions of the creative work produced were shown in the ‘Legge Gallery’, a Fine Art gallery in Sydney. Two critical reviews of those shows appeared in the magazine Craft Arts International, No. 64, 2005, pp 106-107 and The Journal of Australian Ceramics, Vol 46 #1 pp 21-24. Several papers were published detailing various aspects of the research: “The Search for Raw Materials in the Southern Highlands” in The Journal of Australian Ceramics, Vol 41#3, pp 22-23; “Flotation – A method of refining useful minerals”, in The Journal of Australian Ceramics, Vol 41#3, pp 24-25; “Magic Dirt” in The Journal of Australian Ceramics, Vol 46 #1 pp 76-79; “New work from an old landscape”, in Ceramics Technical, 24, 2007. pp 45-52;“From the ground up”, in Ceramic review, issue 222, 2006, pp 54-55. The research concludes that the Southern Highlands of New South Wales is geologically rich in suitable materials for the production of stoneware ceramics and that there are a few specific bai tunze like materials that are very interesting and have considerable aesthetic potential. The research determined that these bai tunze like materials are potentially capable of being developed into clay bodies and glazes of great beauty.
Doctor of Philosophy (PhD)
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Rutherford, Lachlan Stuart. "Developing a tectonic framework for the Southern Curnamona Cu - Au Province : geochemical and radiogenic isotope applications." 2006. http://hdl.handle.net/2440/37818.

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"Two independent geochronological techniques specifically targeting post-kinematic or late-stage growth of kyanite, staurolite and late-stage garnet in the southern Curnamona Province has found that these minerals grew during the Delamerian Orogeny (~530-500 Ma). Prograde metamorphism during the Delamerian Orogeny attained kyanite-staurolite-garnet grade (amphibolite-facies). Previous interpretations of an anticlockwise P-T path for the Olarian Orogeny need revising, as these interpretations have been shown in this study to be based on textural relationships spanning ~1100 million years. This highlights the importance of in situ geochronological techniques in defining robust P-T-t paths for a region." --p. 121 of source document.
Thesis (Ph.D.)--School of Earth and Environmental Sciences, 2006.
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Books on the topic "New South Wales Southern Highlands"

1

Lindley, David. Early Gundagai: Thomas Lindley (1807-1862), emancipist in southern New South Wales. Yass, N.S.W: T. Greensmith, 2002.

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Anderson, Christine Vivien. Heroes of the long paddock: The drovers of Southern New South Wales. Wagga Wagga, N.S.W: Triple D Books, 2006.

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The southern tree of liberty: The democratic movement in New South Wales before 1856. Annandale, N.S.W: Federation Press, 2006.

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McGowan, Barry. Lost mines revisited: Historic mining communities of the Monaro, Southern Tablelands, and South West Slopes Districts of New South Wales. Canberra, ACT: B. McGowan, 1996.

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Colwell, James B. Rig seismic research cruise 13: Structure and stratigraphy of the northeast Gippsland Basin and southern New South Wales margin : initial report. Canberra: Australian Govt. Pub. Service, 1987.

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Colwell, James B. Rig seismic research cruise 13: Structure and stratigraphy of the northeast Gippsland Basin and southern New South Wales margin : initial report. Canberra: Australian Government Publishing Service, 1987.

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Jane Cavanough : Anthea Prell and Tim North. Gardens of the Southern Highlands : New South Wales 1828-1988. Australian Garden Journal, 1988.

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Thomas, Tyrone. 70 Walks in Southern New South Wales and ACT. Michelle Anderson Publishing, 1998.

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Hunter, John. Historical Journal of the Transactions at Port Jackson And Norfolk Island: An With the Discoveries Which Have Been Made in New South Wales And in the Southern Ocean. IndyPublish.com, 2006.

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Sturt, Charles. Two Expeditions into the Interior of Southern Australia, During the Years 1828, 1829, 1830, And 1831 Vol. 2: With Observations on the Soil, Climate, and General Resources of the Colony of New South Wales. University of Cambridge ESOL Examinations, 2011.

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Book chapters on the topic "New South Wales Southern Highlands"

1

Ingold, Derek. "Developments in a Mixed Farming System in Southern New South Wales, Australia." In Rainfed Farming Systems, 1093–102. Dordrecht: Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-1-4020-9132-2_44.

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Fisher, John A., and Brendan J. Scott. "Are we justified in breeding wheat for tolerance to acid soils in southern New South Wales?" In Genetic Aspects of Plant Mineral Nutrition, 1–8. Dordrecht: Springer Netherlands, 1993. http://dx.doi.org/10.1007/978-94-011-1650-3_1.

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Osborne, W. S., K. Kukolic, and K. D. Williams. "Conservation of reptiles in lowland native grasslands in the Southern Tablelands of New South Wales and the Australian Capital Territory." In Herpetology in Australia, 151–58. P.O. Box 20, Mosman NSW 2088, Australia: Royal Zoological Society of New South Wales, 1993. http://dx.doi.org/10.7882/rzsnsw.1993.022.

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Poiner, Gretchen. "A community in crisis: bushfire in a district of the Southern Tablelands of New South Wales." In Australian Ways, 33–50. Routledge, 2020. http://dx.doi.org/10.4324/9781003114987-3.

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Fraser, David. "Mapping Areas Susceptible to Soil Salinity in the Irrigation Region of Southern New South Wales, Australia." In Remote Sensing of Soil Salinization. CRC Press, 2008. http://dx.doi.org/10.1201/9781420065039.pt2.

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Beinart, William, and Lotte Hughes. "Sheep, Pastures, and Demography in Australia." In Environment and Empire. Oxford University Press, 2007. http://dx.doi.org/10.1093/oso/9780199260317.003.0011.

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Succeeding phases of British economic growth prompted strikingly different imperatives for expansion, for natural resource exploitation, and for the social organization of extra-European production. In the eighteenth century, sugar, African slaves, and shipping in the Atlantic world provided one major dynamic of empire. But in the nineteenth century, antipodean settlement and trade, especially that resulting from expanding settler pastoral frontiers, was responsible for some of the most dramatic social and environmental transformations. Plantations occupied relatively little space in the new social geography of world production. By contrast, commercial pastoralism, which took root most energetically in the temperate and semi-arid regions of the newly conquered world, was land-hungry but relatively light in its demands for labour. The Spanish Empire based in Mexico can be considered a forerunner. By the 1580s, within fifty years of their introduction, there were an estimated 4.5 million merino sheep in the Mexican highlands. The livestock economy, incorporating cattle as well as sheep, spread northwards through Mexico to what became California by the eighteenth century. Settler intrusions followed in the vast landmasses of southern Latin America, southern Africa, Australia, and New Zealand. Australia was one of the last-invaded of these territories, and, in respect of the issues that we are exploring, was in some senses distinctive. Unlike Canada and South Africa, there was no long, slow period of trade and interaction with the indigenous population; like the Caribbean, the Aboriginal people were quickly displaced by disease and conquest. The relative scale of the pastoral economy was greater than in any other British colony. Supply of meat and dairy products to rapidly growing ports and urban centres was one priority for livestock farmers. Cattle ranching remained a major feature of livestock production in Australia. Bullock-carts, not dissimilar to South African ox-wagons, were essential for Australian transport up to the 1870s. But for well over a century, from the 1820s to the 1950s and beyond, sheep flooded the southern lands. Although mutton became a significant export from New Zealand and South America, wool was probably the major product of these pastoral hinterlands—and a key focus of production in Australia and South Africa. The growth in antipodean sheep numbers was staggering.
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Conference papers on the topic "New South Wales Southern Highlands"

1

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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Sainsbury, David. "Analysis of River Bed Cracking Above Longwall Extraction Panels in the Southern Coalfield of 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_137.

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"Linking wetland hydrology to ecological outcomes in the Lowbidgee wetlands in Southern New South Wales." In 19th International Congress on Modelling and Simulation. Modelling and Simulation Society of Australia and New Zealand (MSSANZ), Inc., 2011. http://dx.doi.org/10.36334/modsim.2011.e15.wen.

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"Cell-based IQQM Wetland Modelling for Yanga National Park, a forested lowland floodplain in southern New South Wales." In 19th International Congress on Modelling and Simulation. Modelling and Simulation Society of Australia and New Zealand (MSSANZ), Inc., 2011. http://dx.doi.org/10.36334/modsim.2011.i7.mackay.

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Reports on the topic "New South Wales Southern Highlands"

1

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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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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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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Main, P. T., and P. de Caritat. Geochemical survey of the southern Thomson Orogen, southwestern Queensland and northwestern New South Wales: the chemical composition of surface and near-surface catchment outlet sediments. Geoscience Australia, 2016. http://dx.doi.org/10.11636/record.2016.011.

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Savings Bank of New South Wales - Southern - Signature Register - Accounts 1-13800 - 1868-1878. Reserve Bank of Australia, March 2021. http://dx.doi.org/10.47688/rba_archives_2006/21991.

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Savings Bank of New South Wales - Southern - Depositors Ledgers - Accounts 1-1000 - 1868-1877. Reserve Bank of Australia, March 2021. http://dx.doi.org/10.47688/rba_archives_2006/21989.

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