Bibliografie tematiche / Crime New South Wales

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Letteratura scientifica selezionata sul tema "Crime New South Wales"

Autore: Grafiati
Pubblicato: 4 giugno 2021
Ultima modifica: 21 febbraio 2023

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Articoli di riviste sul tema "Crime New South Wales"

1

Mason, Gail. "A Picture of Bias Crime in New South Wales". Cosmopolitan Civil Societies: An Interdisciplinary Journal 11, n. 1 (27 marzo 2019): 47–66. http://dx.doi.org/10.5130/ccs.v11.i1.6402.

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Abstract (sommario):
Bias Crime is crime where the victim is targeted because of an aspect of their identity, including race, ethnicity, religion or sexuality. It is an extreme manifestation of cultural tension and conflict. Bias crime remains under-researched in Australia. While there has been some investigation into different types of bias crime, such as racist and homophobic offences, there is little analysis of the nature and extent of bias crime across these categories. For the first time, this article presents the results of a study into official records of bias crime held by the New South Wales Police Force. The study shows that crimes motivated by bias based on the victim’s race/ethnicity and religion are by far the most common types of bias crime reported in NSW. People from Asian, Indian/Pakistani and Muslim backgrounds are the most likely victims to report bias crime. The study also shows that there is much work to be done to encourage bias crime reporting amongst marginalised communities and improve the capacity of police to identify and accurately record bias crime. We argue that civil society has an important role to play in building partnerships with police to achieve positive change in the policing of bias crime.
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2

Clancey, Garner, e Rohan Lulham. "The New South Wales Property Crime Decline". Current Issues in Criminal Justice 25, n. 3 (marzo 2014): 839–51. http://dx.doi.org/10.1080/10345329.2014.12036001.

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3

Clancey, Garner. "Crime Risk Assessments in New South Wales". European Journal on Criminal Policy and Research 17, n. 1 (14 dicembre 2010): 55–67. http://dx.doi.org/10.1007/s10610-010-9134-7.

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4

Mulrooney, Kyle, Alistair Harkness e Huw Nolan. "Farm Crime and Farmer-Police Relationships in Rural Australia". International Journal of Rural Criminology 7, n. 1 (24 ottobre 2022): 24–45. http://dx.doi.org/10.18061/ijrc.v7i1.9106.

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Abstract (sommario):
This article presents select findings from ‘farm crime’ victimisation surveys undertaken in the two most populous Australian states of New South Wales and Victoria. We examine the findings in relation to farmer crime victimisation, their willingness to report crime, and their worry about crime, as well as farmer perspectives on policing generally and the policing of farm crime specifically. In both states, there are high levels of victimisation, high levels of worry, low- to mid-levels of confidence in the police, and there remains a gap between experiences of farm crime and reporting. Both states have police tasked specifically with addressing farm crime. The Victoria Police have Farm Crime Liaison Officers that specialise in assisting with farm related crimes, however this is a voluntary role which forms part of an officer’s larger workload. By contrast, the New South Wales Police Force Rural Crime Prevention Team is a dedicated team consisting of specialised rural crime investigators and intelligence practitioners focused on proactive and preventative interventions in farm crime. Farmers in both states were surveyed regarding their awareness and engagement with these rural policing teams, and we examined how this may shape victimisation, reporting, worry and the relationships between police and farmers. In New South Wales, awareness and direct contact with rural crime police led to both increased satisfaction with police and crime reporting. Respondents with awareness of this team also express significantly less worry of crime, whilst those with direct contact did not. We conclude the article by discussing and contextualising these findings within rural criminology and considering ways forward for the policing of farm crime.
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5

Mason, Gail, e Rachael Stanic. "Reporting and recording bias crime in New South Wales". Current Issues in Criminal Justice 31, n. 2 (3 aprile 2019): 164–80. http://dx.doi.org/10.1080/10345329.2019.1594920.

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6

Clancey, Garner, e Daren Fisher. "Crime prevention through environmental design in New South Wales". Australian Planner 53, n. 2 (9 dicembre 2015): 73–82. http://dx.doi.org/10.1080/07293682.2015.1118392.

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7

Chilvers, Marilyn, e Don Weatherburn. "The New South Wales “Compstat” Process: Its Impact on Crime". Australian & New Zealand Journal of Criminology 37, n. 1 (aprile 2004): 22–48. http://dx.doi.org/10.1375/acri.37.1.22.

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8

BYRNES, JOSHUA M., CHRISTOPHER M. DORAN e ANTHONY P. SHAKESHAFT. "Cost per incident of alcohol-related crime in New South Wales". Drug and Alcohol Review 31, n. 7 (10 maggio 2012): 854–60. http://dx.doi.org/10.1111/j.1465-3362.2012.00467.x.

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9

Clancey, Garner. "Are we still ‘Flying Blind?’ Crime Data and Local Crime Prevention in New South Wales". Current Issues in Criminal Justice 22, n. 3 (marzo 2011): 491–500. http://dx.doi.org/10.1080/10345329.2011.12035901.

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10

Gliksman, Michael. "Gender-Based Differences in the Treatment of Young Offenders by the Police and the Children's Court in New South Wales, Australia". Medicine, Science and the Law 37, n. 2 (aprile 1997): 165–69. http://dx.doi.org/10.1177/002580249703700213.

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Abstract (sommario):
It has been consistently reported that young males commit crimes with an average frequency five times greater than their female peers. Most data supporting this view are derived from juvenile court and police statistics. Studies using data derived from self-reported behaviour suggest that the true relative frequency may be closer to 2:1. Police and juvenile justice data for the year 1994–5 in New South Wales, Australia, were analysed in an attempt to determine whether court and police statistics might reflect a form of selection bias, where the likelihood of arrest, trial and/or sentence is a function of gender, rather than frequency and nature of offence. The results suggest that the 5:1 gender ratio reflects a strong component of gender bias in the workings of the juvenile justice system in New South Wales. If suspected of a given crime, young males are more likely to be denied bail and (if found guilty) to be given a harsher sentence than young females suspected (or found guilty) of the same crime. Overall, if found guilty of an offence, boys were four times more likely than girls to receive a custodial sentence. Therefore, boys are selectively denied access to alternate rehabilitation resources which are made available to girls who are in trouble with the law. The juvenile justice system in New South Wales requires careful examination and reform if such apparently deeply entrenched biases are to be eliminated.
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Più fonti

Tesi sul tema "Crime New South Wales"

1

Johnson, Andrew, of Western Sydney Hawkesbury University, Faculty of Social Inquiry e School of Ecology. "Crime, governance and numbers : a genealogy of counting crime in New South Wales". THESIS_FSI_SEL_Johnson_A.xml, 2000. http://handle.uws.edu.au:8081/1959.7/535.

Testo completo
Abstract (sommario):
This thesis is an intellectual genealogy of counting crime in New South Wales. It is a history of a system of thought which is one of the contemporary foundations of the way we interpret the nature and extent of crime today. It argues that the incitement to annually record crime statistics in New South Wales, and internationally, is immediately connected with a will to govern crime. This thesis traces this bonding of the technology of crime statistics with mentalities of government, and maintains that although the connection of these two discourses has been highly effective, it has not been one of universal domination. This is a history of the continuous state practice of compiling and publishing crime statistics. But it is also a history of discontinuities. This thesis regularly investigates shifts in the categories of recording. It locates changes in what is recorded by broadening its discussion to include localised and international debates on crime that are contemporaneous to these changes. This is not a thesis with a project to improve the way in which we record or utilise crime statistics. Its project is to write a history of how we came to record crime statistics and how we have intended to utilise these crime statistics in our practices of government. It traces the rise of counting crime and interrogates it as one of the key technologies deployed in the government of crime
Doctor of Philosophy (PhD)
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2

Johnson, Andrew. "Crime, governance and numbers : a genealogy of counting crime in New South Wales". Thesis, View thesis, 2000. http://handle.uws.edu.au:8081/1959.7/535.

Testo completo
Abstract (sommario):
This thesis is an intellectual genealogy of counting crime in New South Wales. It is a history of a system of thought which is one of the contemporary foundations of the way we interpret the nature and extent of crime today. It argues that the incitement to annually record crime statistics in New South Wales, and internationally, is immediately connected with a will to govern crime. This thesis traces this bonding of the technology of crime statistics with mentalities of government, and maintains that although the connection of these two discourses has been highly effective, it has not been one of universal domination. This is a history of the continuous state practice of compiling and publishing crime statistics. But it is also a history of discontinuities. This thesis regularly investigates shifts in the categories of recording. It locates changes in what is recorded by broadening its discussion to include localised and international debates on crime that are contemporaneous to these changes. This is not a thesis with a project to improve the way in which we record or utilise crime statistics. Its project is to write a history of how we came to record crime statistics and how we have intended to utilise these crime statistics in our practices of government. It traces the rise of counting crime and interrogates it as one of the key technologies deployed in the government of crime
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3

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

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Abstract (sommario):
Thesis (Ph.D.) -- University of Western Sydney, 2000.
A thesis submitted in fulfilment of the requirements for the degree of PhD, Department of Critical Social Sciences, University of Western Sydney, 2000. Bibliography : leaves 196-214.
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4

Scrivener, Gladys. "Rescuing the rising generation : industrial schools in New South Wales, 1850-1910". Thesis, [Campbelltown, N.S.W. : The Author], 1996. http://handle.uws.edu.au:8081/1959.7/376.

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Abstract (sommario):
The Industrial Schools Act introduced State coercion into the ‘childcare’ of the colony, and industrial schools became legal enforcers for other welfare institutions. This thesis provides an account of two industrial schools in nineteenth and early twentieth century New South Wales, focusing on the children and the lives they lived within the institutions and relying heavily upon primary sources. NSS Vernon enrolled destitute, neglected and delinquent boys. The curriculum, combined with an elaborate system of rewards, proved effective as reformative agents and after 1911 the ship’s coercive function was taken over by other reformatory schools and by a system of probation. About one third of girls admitted to ISG Newcastle were older, sexually delinquent girls. Inappropriate site, inadequate preparation, insufficient and untrained staff, lack of suitable curriculum and denial of support from the Colonial Secretary led to total failure of the school. Physical and verbal abuse was in evidence at Newcastle and resurfaced after the change of enrollments to mostly older girls about the time of the school’s transfer to Parramatta in 1887. After 1905 committals were aimed at maintaining street order and parental authority, to house the ‘uncontrollables’ and ‘incompetents’ and to provide a lock hospital for the control of venereal disease. The expressed purpose of the school to provide ‘good useful women’ dovetailed neatly with the introduction of probation, mostly for boys, which was enforced ‘through the mother’
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5

Asquith, Nicole L. "Text and context of malediction a study of antisemitic and heterosexist hate violence in New South Wales 1995-2000 /". Connect to this title online, 2004. http://eprints.unimelb.edu.au/archive/00001424/.

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6

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

Testo completo
Abstract (sommario):
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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7

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

Testo completo
Abstract (sommario):
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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8

Keogh, Andrew James, of Western Sydney Hawkesbury University, Faculty of Science and Technology e 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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Abstract (sommario):
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.
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Elliott, Malcolm Gordon, of Western Sydney Hawkesbury University e 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.
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Wood, Susan, e 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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Libri sul tema "Crime New South Wales"

1

Jones, Craig. Evaluating police operations. Sydney: New South Wales Bureau of Crime Statistics and Research, 2004.

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2

Easteal, Patricia Weiser. Vietnamese refugees: Crime rates of minors and youths in New South Wales. Canberra: Australian Institute of Criminology, 1989.

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Tomsen, Stephen. Hatred, murder, and male honour: Anti-homosexual homicides in New South Wales, 1980-2000. Canberra: Australian Institute of Criminology, 2002.

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4

Milliss, Roger. Waterloo Creek: The Australia Day massacre of 1838, George Gipps and the British conquest of New South Wales. Ringwood, Vic: McPhee Gribble, 1992.

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5

(Firm), Urbis Keys Young, e Network of Government Agencies, a cura di. You shouldn't have to hide to be safe: A report on homophobic hostilities and violence against gay men and lesbians in New South Wales. Sydney]: NSW Attorney General's Dept., 2003.

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6

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

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7

New South Wales: The New South Wales Additional Instructions 1986. London: HMSO, 1986.

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8

Sue, Kendrick, a cura di. The Shoalhaven: South Coast, New South Wales. Nowra, N.S.W: Lightstorm Pub., 1995.

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9

Britts, M. G. Traffic law (New South Wales). Sydney: Lawbook Co., 2006.

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10

Holmes, G. G. Diatomite in New South Wales. [Sydney]: Dept. of Minerals and Energy, Geological Survey of New South Wales, 1989.

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Capitoli di libri sul tema "Crime New South Wales"

1

Bailey, Victor. "Petitioner wants to join Convict Husband in New South Wales, 1829". In Nineteenth-Century Crime and Punishment, 148. London: Routledge, 2021. http://dx.doi.org/10.4324/9780429504013-23.

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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, e 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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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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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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6

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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7

Arnold, Guy. "Crime and Violence". In The New South Africa, 83–90. London: Palgrave Macmillan UK, 2000. http://dx.doi.org/10.1057/9780230213852_9.

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Chapman, D. M. "Australia--New South Wales and Queensland". In The GeoJournal Library, 415–22. Dordrecht: Springer Netherlands, 1988. http://dx.doi.org/10.1007/978-94-009-2999-9_45.

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Bird, Eric. "Lord Howe Island – (New South Wales)". In Encyclopedia of the World's Coastal Landforms, 1239–46. Dordrecht: Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-1-4020-8639-7_226.

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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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Atti di convegni sul tema "Crime New South Wales"

1

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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2

Senden, David van, e 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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3

Conway, Andrew, Michelle Blom, Lee Naish e 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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4

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

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5

Radoll, Peter, Sebastian Fleissner, Duncan Stevenson e 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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6

Zhu, Qinggaozi, Xihua Yang e 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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7

Catalan, Alex, e 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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8

"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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Duc, Hiep Nguyen, Sean Watt, David Salter e 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, e 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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Rapporti di organizzazioni sul tema "Crime New South Wales"

1

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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2

Kyi, D., J. Duan, A. Kirkby e 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 e 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 e 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 e 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., e 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 e 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 e 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., e 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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