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Дисертації з теми "Clearing of land Victoria"

Автор: Grafiati

Опубліковано: 10 грудня 2022

Оновлено: 28 січня 2023

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1

Newland, Nicholas. "Brush cutting and brush fencing : sustainable resource use or environmental impoverishment?" Title page, contents and abstract only, 1991. http://web4.library.adelaide.edu.au/theses/09ENV/09envn549.pdf.

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2

Callow, John Nikolaus. "River response to land clearing and landscape salinisation in southwestern Australia." University of Western Australia. School of Earth and Geographical Sciences, 2007. http://theses.library.uwa.edu.au/adt-WU2007.0085.

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[Truncated abstract] Land clearing is known to increase runoff, and in many dryland landscapes is also associated with rising saline watertables, causing increased stream salinity and degrading riparian vegetation. The limited understanding of how river morphology responds to these changes and the potential for vegetation-based strategies to offer river management options under these conditions, has prompted this research. In southwestern Australia the severity of salinity and recent nature of land clearing provides an appropriate setting to investigate river response. A data-based, multidisciplinary methodology was applied to determine how land clearing and landscape salinisation has altered landscape sensitivity through changes in erosive potential, system connectivity and material threshold mechanisms, and how these affect patterns of river response. The study investigated the responses of morphologically similar reaches across fifty two study sites in the Kent River and Dalyup River catchments, in the south coastal rivers region of Western Australia. Land clearing was found to have significantly altered the hydrologic regime and erosive potential in both frequency and magnitude, with flow becoming more perennial, and increased annual discharge, flood peaks and bankfull flow frequency. While sediment transport rates have also increased since land clearing, they remain low on a global scale. Human response to a reduced rainfall regime and related water security pressures has caused large hillslope areas to be decoupled from the main channels by bank and farm dam construction, and have reduced downstream transmission of change. ... By contrast, steeper-sloped mid-catchment areas with minimal vegetation degradation caused by salinity are associated with higher erosive potential. A more erosive response is observed in these reaches where floodplains have been cleared for agricultural purposes. A conceptual model of vegetation growth across the salinity gradient observed in the study catchments was developed, and applied to selected river styles to assess the potential that vegetation-based strategies offer for river management. This work identifies the unsuitability of river restoration strategies, but the potential for river restoration or remediation in a saline landscape. Hydraulic modelling demonstrated that river rehabilitation strategies such as improving the vegetation condition of the riparian buffer using native or commercial species on areas elevated above saline flow can stabilise reaches. For river styles in wide and flat valleys, there is limited potential for vegetation-based river rehabilitation under the current salinity gradient. Field observation and modelling suggest that river remediation may offer geomorphic management options in salt-affected reaches through channelisation to lower watertables, and further research on this is warranted. This work found a consistent response for river styles across the two study catchments. Based on the understanding of river response and the potential for vegetation-based river management for each style, this research offers a regional-scale tool for river management in a saline landscape.

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3

Janosy, Robert John. "Structural investigations of the early paleozoic Victoria land dike swarm in the Ferrar-Koettlitz glacier region, Southern Victoria Land, Antarctica." The Ohio State University, 1994. http://rave.ohiolink.edu/etdc/view?acc_num=osu1300117001.

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4

Horn, Kipps 1949. "Rebetika music in Melbourne, 1950-2000 : old songs in a new land, new songlines in an old land." Monash University, School of Music-Conservatorium, 2002. http://arrow.monash.edu.au/hdl/1959.1/8015.

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5

Walker, Kimberley. "Clearing the Brownfields: Offsetting the Risks to Sustainable Development of Contaminated Land." Thesis, Université d'Ottawa / University of Ottawa, 2018. http://hdl.handle.net/10393/37477.

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This research develops eight recommendations for amendments to key Ontario legislation affecting Brownfield redevelopment that, if implemented, will reduce the liability and risk associated with the development of contaminated land and benefit stakeholders, such as, municipalities and developers. Utilizing the methodology of law and economics, this research examines the legal landscape in Ontario and expands the dialogue regarding the risks of developing contaminated land. Through this examination, this research uncovers the origins of the risks of Brownfield redevelopment and extrapolates recommendations for amendments to legislation and policy that balance the liability of Brownfield redevelopment with the protection of the environment. Recent developments in environmental law appear to increase environmental protection, but actually limit Brownfield redevelopment in Ontario by increasing liability and costs. The polluter pays principle that has been entrenched in Canadian law has governed the law in respect of contaminated lands for decades. However, as society evolves, the common law is forced to re-evaluate environmental protection in the face of contaminated lands. This evolution of the law is an attempt to intervene to correct a market failure that exists with respect to contaminated lands. The increased liability associated with Brownfield redevelopment translates into heightened costs to redevelop the land, which also severely threatens environmental justice in Ontario. The recommendations in this research will benefit stakeholders, the public, and the environment. With respect to stakeholders, it will be of assistance to municipalities, cities, developers, corporations, secured lenders, mortgage insurers and the government. The risks associated with Brownfield redevelopment can be offset by the recommended corrections to legislation regarding liability and stronger policies that create accessible programs and incentives to promote just, innovative, and sustainable redevelopment.

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6

Hung, Chung-hing Mason. "A waterfront development strategy for Victoria Harbour /." Hong Kong : University of Hong Kong, 1997. http://sunzi.lib.hku.hk/hkuto/record.jsp?B19131136.

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7

Elliott, Christine Eleanor. "Physical Rock Weathering Along the Victoria Land Coast, Antarctica." Thesis, University of Canterbury. Geography, 2006. http://hdl.handle.net/10092/1305.

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The purpose of this research was to investigate the physical weathering of rock along the Victoria Land Coast, Antarctica. It was designed to contribute to the Latitudinal Gradient Project, a joint initiative between the New Zealand, Italian and United States Antarctic Programmes. The Latitudinal Gradient Project aims to improve our understanding of the ecosystems of the Dry Valleys and ice-free areas of the Ross Sea Region and, by using latitude as a proxy measure, identify how they might be affected by future climate change. The approach taken for this research was to use information on rock (from one rock group) temperature and moisture conditions gathered from three field locations to inform laboratory simulations. The laboratory simulations would then be used to investigate the weathering of small rock blocks and aggregates. Two temperature cycles approximating those experienced during summer and spring/autumn were identified and simulations undertaken in a specially adapted freezer. Three levels of moisture were applied: no moisture, half saturation and full saturation. Results of the laboratory simulations indicated that although rocks responded in different ways to different processes, granular disintegration took place even in the absence of additional moisture and did not require crossings of the 0 OC isotherm, nor were high levels of moisture required for across zero temperature cycling to produce weathering effects. A model that related weathering to latitude was developed and changes in climate explored. It was found that the weathering effect of summer and spring/autumn cycles was different and depended on rock characteristics rather than latitude. Increasing the ratio of summer to spring/autumn temperature cycles by 10% indicated that weathering could decrease or remain the same depending on the particular rock. Changes in temperature were found to be more important than changes in moisture. A weathering index that related local climate and rock properties to weathering was also developed and this highlighted the difficulties of using laboratory results to predict field rates of weathering. There were some surprising results from the field, including the presence of much more moisture on the surface of the rock, primarily from blowing snow, than had been predicted for this dry environment. This occurred even in the presence of negative rock surface temperatures. In addition, winter rock surface temperatures can fluctuate up to 25 OC, getting as warm as -10 OC. Macro-climate and changes in air temperature in response to foehn and katabatic winds were the drivers for these fluctuations.

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8

Baxter, James Stanley, and james baxter@rmit edu au. "Rural Land Use and Value In Northern Victoria 1880 - 1960." RMIT University. Property, Construction & Project Management, 2001. http://adt.lib.rmit.edu.au/adt/public/adt-VIT20091008.135904.

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This thesis examines rural development processes, and in particular the impact over time of infrastructure investment on locational value in a farming community in northern Victoria, Australia. Correlation between infrastructure investment and land values was found to change over time, with the full cost of infrastructure provision not reflected in increased land values. Its impact depended on the type of infrastructure, and was linked to technological changes in agricultural production that led to different demands. The study also revealed the complexity of land ownership and use during the development of typical northern Victorian farmland, and the patterns of land value that emerged. As an historical study of land development it provides a deeper understanding of rural valuation methodology and sales analysis. It also contributes to the theory of land development, and in particular rural land-use and value.

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9

Davies, Mark Thomas Lloyd. "A polar paradise the glaciation of South Victoria Land, Antarctica /." [S.l. : Amsterdam : s.n.] ; Universiteit van Amsterdam [Host], 2004. http://dare.uva.nl/document/71753.

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10

Leung, Kim-cheong Warren, and 梁儉昌. "An impact study of the land reclamation on Victoria Harbour." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 1988. http://hub.hku.hk/bib/B31257525.

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11

Yuen, Ping-shu Gomez, and 袁秉樞. "Is reclamation necessary in Victoria Harbour?" Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2000. http://hub.hku.hk/bib/B31254810.

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12

Savage, Jeni Ellen. "Provenance Analysis of the Sperm Bluff Formation, southern Victoria Land, Antarctica." Thesis, University of Canterbury. Geological Sciences, 2005. http://hdl.handle.net/10092/1497.

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Beacon Supergroup rocks of probable Devonian age, containing conglomerate clasts of lithologies unknown in outcrop in southern Victoria Land (SVL) occur in the St Johns Range to Bull Pass Region, SVL, Antarctica. The Lower Taylor Group sedimentary rocks, herein called the Sperm Bluff Formation, unconformably rest on the regionally extensive Kukri Erosion Surface that truncates local basement. The basement complex includes three Plutonic Suites, Dry Valley (DV) 1a, DVIb and DV2 of the Granite Harbour Intrusives that intrude metasedimentary rocks of the Koettlitz Group. Allibone et al. (1993b) suggested a SVL terrane accretion event may have occurred about the same time as accretion of a terrane known as the Bowers terrane in northern Victoria Land (NVL) based on changing chemistry of the CambroOrdovician granitoids. Further, it is suggested that conglomerate clasts of the Sperm Bluff Formation may have been derived from this postulated terrane (Allibone et al., 1993b; and Turnbull et al., 1994). Following extensive fieldwork provenance studies and basin analysis of the sedimentary Sperm Bluff Formation are used here to test these ideas. The Sperm Bluff Conglomerate of Turnbull et al. (1994) is re-interpreted as the Sperm Bluff Formation and described using a lithofacies-based approach. The Sperm Bluff Formation is divided into six lithofacies including 1) Conglomerate Lithofacies; 2) Pebbly Sandstone Lithofacies; 3) Crossbedded Sandstone Lithofacies; 4) Parallelbedded Lithofacies; 5) Low-angle Crossbedded Lithofacies; and 6) Interbedded Siltstone/Sandstone Lithofacies. The intimate field association of the Conglomerate, Pebbly Sandstone and Crossbedded Sandstone Lithofacies ties them to the Conglomerate Lithofacies Association whereas the other three units are independent. The Conglomerate Lithofacies Association is interpreted to represent a wavedominated deltaic environment, based on the presence of broad channels, pervasive crossbedding, paleocurrent and trace fossil data. Both Parallel-bedded and Low-angle Crossbedded Sandstone Lithofacies are interpreted as a foreshore-shore face shallow marine setting on the basis of low-angle crossbeds and trace fossil assemblages. The Interbedded Siltstone and Sandstone Lithofacies is interpreted as an estuarine environment based on alternating siltstone/sandstone beds and the presence of flaser and lenticular bedding, small crossbedded dune sets, mud drapes, syneresis cracks and diverse paleocurrent directions. An estuarine setting is tentatively favoured over a lagoonal setting due to the presence of syneresis cracks small channels and the proximity to a river delta. I suggest that the Sperm Bluff Formation is likely a lateral correlative of the Altar Mt Formation of the Middle Taylor Group, in particular the Odin Arkose Member. This interpretation is based on arkosic nature of the sedimentary rocks, regional paleocurrent patterns, the presence of salmon pink grits at Gargoyle Turrets and trace fossil assemblages. The upper most lithofacies at Mt Suess, the Low-angle Crossbedded Sandstone Lithofacies that only occurs at this site is- suggested as a lateral correlative to the Arena Sandstone, which stratigraphically overlies the Altar Mt Formation, based on quartzose composition, clay matrix, stratigraphic position and trace fossils present. Provenance analysis was carried out on sedimentary rocks and conglomerate clasts using clasts counts of conglomerates, petrographic analysis of clasts, point counts of sandstones and clasts, geochemistry and V-Pb detrital zircon analysis. Conglomerate clasts lithologies include dominantly silicic igneous clasts and finely crystalline quartzite clast amongst other subordinate lithologies such as vein quartz, schist, schorl rock, gneiss and sandstone. Despite past identification of granitoid clasts in the Sperm Bluff Formation (Turnbull et al., 1994), none were found. Rhyolitic clasts of the Sperm Bluff Formation have compositions typical of highly evolved subduction related rocks, although they have undergone post-emplacement silicification. Wysoczanski et al. (2003) date rhyolite and tuff clasts between 497±17 Ma and 492±8 Ma, placing them within error of all three Dry Valley Magmatic Suites and removing the likelihood of correlation to NVL volcanic rocks. Petrographic analysis suggests they are components of a silicic magmatic complex. Chemically the volcanic clasts appear to represent a single magmatic suite (Sperm Bluff Clast Suite), and are clearly related to the Dry Valley Plutonic Suites. Although clasts are not constrained beyond doubt to one Suite, DV2 is the best match. Quartzite clasts of the Sperm Bluff Formation are too pure and old to be derived from a local source. Detrital zircon V-Pb ages for the quartzite suggest zircons were derived from the East Antarctic Craton, and that the quartzite source rocks were deposited prior to the Ross-Delamarian Orogeny. Quartzite with a similar age signature has not been identified; however, the Junction Formation sandstone of northwest Nelson has a similar age spectrum. Sandstones from the Sperm Bluff Formation indicate derivation from a felsic continental block provenance, which contain elements of volcanic, hyperbyssal and plutonic rocks. They are arkosic to quartzose in composition and conspicuously lack plagioclase. Detrital zircon analyses give a strong 500 Ma peak in all 3 samples, characteristic of a Ross-Delamarian Orogen source, with few other peaks. The dominance of a single peak is highly suggestive oflocal derivation. The sedimentary rocks of the Sperm Bluff Formation are interpreted to be derived predominantly from the basement rocks they now overlie. The presence of the regionally extensive Kukri Erosion Surface at the lower contact of the Beacon Supergroup rocks implies an intermediate source must have existed. This most likely contained all components of the formation. I suggest that the DV2 Suite was emplaced in a subsiding, extensional intra-arc setting. Erosion of the uplifted arc region probably occurred from Late Ordovician to Silurian times with deposition of sediments in a subsiding intra-arc basin. Erosion of the rhyolitic complex in this region probably occurred, however, it is likely that some was preserved. Inversion of this basin prior to the Devonian probably provided the means for these sediments to be deposited as the Sperm Bluff Fonnation.

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13

Chan, Yuet-ling. "Reclamation and pollution in Hong Kong with special reference to Victoria Harbour /." Hong Kong : University of Hong Kong, 2000. http://sunzi.lib.hku.hk/hkuto/record.jsp?B2226632X.

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14

Carson, Nicholas Joseph. "The geology and geomorphology of the Denton Hills, Southern Victoria Land, Antarctica." Thesis, University of Canterbury. Geological Sciences, 2012. http://hdl.handle.net/10092/7467.

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This research is an integrated geological and geomorphological study into the Denton Hills area. The study area is part of the foothills to the Transantarctic Mountains, which divides East and West Antarctica, allowing an opportunity to investigate glacial events from both sides. As the study area is ice-free, it has allows good examination of the bedrock geology and has preserved geomorphological features allowing them to be examined and sampled. Comprehensive geological map and geomorphological maps have been produced, extending the knowledge into the spatial distribution of units and features. Both the geological and geomorphological maps reveal a complex history of evolution. The original geological units have been subjected to deformation and intrusion of large plutons. The geomorphological mapping shows ice has flowed in alternate direction through the valleys, and the valleys have had long periods where they have been occupied by large proglacial lakes. As the Antarctic ice sheets expanded they flowed into the valleys either from the west, the Royal Society Range draining the East Antarctic Ice Sheet or from the east, McMurdo Sound. Ice would flow from McMurdo Sound when the West Antarctic Ice Sheet expanded causing the grounding line of the ice sheet to move north through the Ross Sea. Surface exposure dating completed during the study has correlated the timing of glacial events to global cycles. The dating confirmed the presence of the large proglacial lake during the Last Glacial Maximum in the Miers Valley, which drained about 14 ka. The Garwood Glacier has also been directly linked to the Last Glacial Maximum with a moraine forming about 22 ka. The dating has also shown that during the Last Glacial Maximum there was little fluctuation in the size of glaciers draining the East Antarctic Ice Sheet, with features being date to the onset of the Last Glacial Maximum.

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15

Hung, Chung-hing Mason, and 洪忠興. "A waterfront development strategy for Victoria Harbour." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 1997. http://hub.hku.hk/bib/B3125939X.

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16

Gowda, Krishne. "Land reclamation and its impact on environment : a case study of Victoria Harbour /." Thesis, Hong Kong : University of Hong Kong, 1996. http://sunzi.lib.hku.hk/hkuto/record.jsp?B18139267.

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17

Chan, Yuet-ling, and 陳月玲. "Reclamation and pollution in Hong Kong with special reference to Victoria Harbour." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2000. http://hub.hku.hk/bib/B31254494.

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18

Ross, Pierre-Simon, and n/a. "Volcanology of the Mawson Formation at Coombs and Allan Hills, South Victoria Land, Antarctica." University of Otago. Department of Geology, 2005. http://adt.otago.ac.nz./public/adt-NZDU20070418.151642.

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The Jurassic Ferrar large igneous province of Antarctica contains significant mafic volcaniclastic deposits, underlying the Kirkpatrick flood basalts. In South Victoria Land, the mafic volcaniclastics are referred to as the Mawson Formation. At Coombs Hills, the Mawson is interpreted as filling a large vent complex, which was re-examined in detail to better understand vent-forming processes. Two contrasting types of cross-cutting volcaniclastic bodies were found in the complex, both of which are interpreted to have been forcefully emplaced from below into existing, non-consolidated debris. The first type consists of country rock-rich lapilli-tuff pipes. These are interpreted as fossilized remnants of subterranean debris jets which originated when phreatomagmatic explosions occurred near the walls or floor of the vent complex, causing fragmentation of both magma and country rock. The second type of cross-cutting body consists of basalt-rich tuff-breccias and lapilli-tuffs, some of which could have been generated by explosions taking place within pre-existing basalt-bearing debris, well away from the vent walls. Other basalt-rich zones, accompanied by domains of in situ peperite and coherent basalt, are inferred to have originated by less violent processes. At nearby Allan Hills, the Mawson can be divided into two informal members, m₁ and m₂. Member m₁ is exposed only at central Allan Hills, consists essentially of sedimentary material from the underlying Beacon Supergroup, and is interpreted as a [less than or equal to]180 m-thick debris avalanche deposit. Most megablocks in m₁ were derived from the late Triassic Lashly Formation, parts of which were probably only weakly consolidated in the Jurassic. Sandstone breccias dominate volumetrically over megablocks within the deposits. This indicates pervasive and relatively uniform fragmentation of the moving mass, and probably reflects the weak and relatively homogeneous nature of the material involved. The avalanche flowed into a pre-existing topographic depression carved into the Beacon sequence, and flow indicators reveal a northeastward movement. Sparse globular basaltic megablocks suggest that Ferrar intrusions played a role in triggering the avalanche. Member m₂, which is exposed at both central and southern Allan Hills, consists predominantly of metre-thick basaltic volcaniclastic layers that fall into three broad categories: (1) poorly sorted, coarse lapilli-tuff and tuff-breccia; (2) block-rich layers; (3) tuff and fine lapilli-tuff. The former type is interpreted as the deposits of high-concentration pyroclastic density currents (PDCs), probably formed during the collapse of phreatomagmatic eruption plumes. Occasional block-rich layers probably were formed by both ballistic fall from local vents and pyroclastic flows, and the finer-grained layers were probably deposited by dilute PDCs. Dilute, moist turbulent currents were also likely responsible for the generation and deposition of large ([less than or equal to]4.5 cm) rim-type accretionary lapilli. The thick layers are locally underlain by or interbedded with thin tuff ring-style volcaniclastic layers, and all the layers are underlain and invaded by basalt-rich tuff-breccias and lapilli-tuffs. COMPLETE REFERENCE: Ross, P.-S. (2005) Volcanology of the Mawson Formation at Coombs and Allan Hills, South Victoria Land, Antarctica. PhD Thesis, University of Otago, Dunedin, New Zealand, 400 pages, 46 tables, 162 figures, plus appendices.

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19

Ngeh, Chiambeng Paulinus. "Effects of land clearing methods on a tropical forest ecosystem and the growth of Terminalia ivorensis (A. Chev.)." Thesis, University of Edinburgh, 1989. http://hdl.handle.net/1842/15515.

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20

Noack, Denise Helen. "The contribution of heritage agreements to conservation in the Murray Mallee of South Australia /." Title page, contents and abstract only, 1991. http://web4.library.adelaide.edu.au/theses/09ENV/09envn739.pdf.

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21

Dam, Oscar van. "Forest filled with gaps effects of gap size on water and nutrient cycling in tropical rain forest : a study in Guyana = Bos gevuld met gaten : de effecten van de grootte kronendakopeningen op de water- en nutriëntenkringloop in tropisch regenwoud : een studie in Guyana /." Georgetown, Guyana : Tropenbos Guyana Programme, 2001. http://catalog.hathitrust.org/api/volumes/oclc/48485430.html.

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22

Gilmer, Greer Jessie. "Paleoenvironmental Interpretations of the Lower Taylor Group, Olympus Range area, southern Victoria Land, Antarctica." Thesis, University of Canterbury. Geological Sciences, 2008. http://hdl.handle.net/10092/1985.

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The Devonian Taylor Group, in the Olympus Range area, southern Victoria Land (SVL), Antarctica, is separated from the basement by a regional nonconformity (Kukri Erosion Surface). A second localized unconformity within the Taylor Group called the Heimdall Erosion Surface separates the New Mountain Sandstone and older units from the younger Altar Mountain Formation. The depositional environment of the New Mountain Sandstone has long been under contention. The New Mountain Sandstone Formation is a predominantly quartzose cross-bedded sandstone. Its newly defined Mt Jason Member is a coarse arkosic small scale cross-bedded pebbly sandstone that grades up section into the rest of the quartzose New Mountain Sandstone with large scale cross beds. The New Mountain Sandstone has been divided into five lithofacies including the Basal Conglomerate Lithofacies, Pebbly Sandstone Lithofacies, Granule Cross-bedded Lithofacies, Pinstripe Cross-bedded Lithofacies and Cross-bedded Sandstone Lithofacies. Deposition was in a shoreface environment with minor coastal aeolian deposition. The environment changed from upper shoreface to lower shoreface up section, forming transgressive to highstand systems tracts. The Heimdall Erosion Surface truncates the Cross-bedded Sandstone Lithofacies and the Pinstripe Cross-bedded Lithofacies and was formed due to relative sea level fall leading to exposure and erosion of underlying sedimentary and basement rocks. It forms a type 1 sequence boundary. The New Mountain Sandstone was partially or totally lithified before erosion as shown by the jagged morphology of the eroded cross beds on the surface. It is not known when cementation of the NMS took place or how much of the formation has been eroded. The Heimdall Erosion Surface and Kukri Erosion Surface converge locally due to erosion on the Heimdall Erosion Surface and relief on the Kukri Erosion Surface. The Heimdall Erosion Surface became a shore platform and the site of deposition as relative sea level rose. The Altar Mountain Formation with its Odin Member is a cross-bedded, massive and bedded feldspathic and quartzose sandstone that fines up section and is deposited on the erosion surface. The Altar Mountain Formation is divided into four lithofacies including the Conglomerate Lithofacies, Trough Cross-bedded Lithofacies, Cross-bedded Bioturbated Lithofacies and Bedded Fine Lithofacies. Deposition was in a shoreface environment, changing up section to an inner shelf environment with minor estuarine/tidal influence near the top of the section forming transgressive to highstand to regressive system tracts. The sedimentary rocks are derived mainly from the Granite Harbour Intrusives and Koettlitz Group, which underlie the sandstones, but were exposed elsewhere in SVL. The sandstone clasts within the Conglomerate Lithofacies could be derived from underlying older Taylor Group rocks or exotic sources from outside the field area. Correlation with data from adjacent areas suggests deposition of the New Mountain Sandstone occurred in a shallow sea that existed from the Olympus Range, southwards into the Asgard Range and included Vashka Crag. The area around Sponsors Peak and to the north was exposed and supplying feldspathic and quartzose sediment and pebbles into the depositional basin. As relative sea level fell due to either tectonic uplift or eustatic processes a large area of southern Victoria Land was exposed including the Olympus and Asgard Ranges and Bull Pass-St Johns Range area. This lead to erosion of the New Mountain Formation and basement rocks. Deposition of the New Mountain Sandstone continued further south shown by the gradational contact between it and the overlying Altar Mountain Formation. Relative sea level rise led to deposition of the Altar Mountain Formation. Shallow seas once more dominated the southern Victoria Land with deltas in the east (in the Bull Pass-St Johns Range area) feeding feldspathic sediment into the depositional basin (Odin Member). Further sea level rise drowned the delta region and a shallow marine to inner shelf environment led to deposition of the rest of the Altar Mountain Formation.

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23

Frost, Ken, and mikewood@deakin edu au. "Soldier settlement after world war one in south western Victoria." Deakin University. School of Social and International Studies, 2002. http://tux.lib.deakin.edu.au./adt-VDU/public/adt-VDU20051125.102701.

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This thesis addresses the physical aspects of farming on soldier settlement blocks in south west Victoria. The undeveloped land, high establishment costs, stock losses through animal diseases and lack of managerial skills all contributed to the settlers' inability to meet their financial commitments. These factors are analysed, as are the effects of declining rural commodities prices during the 1920s and 1930s. In addition, the relationship between the settlers and the successive administrative agencies is examined. The scheme was administered by the Closer Settlement Board from its inception until 1932 and much of the discussion during this period concerns the interaction between settler and inspector. Soldier settlement after World War One represented one of the last attempts to create a large body of 'yeoman' farmers. From the early 1920s there was an increasing dichotomy between the 'yeoman' and the 'managerial' ideologies. This dichotomy placed additional pressure on soldier settlers who were expected to be 'efficient' without adequate finances. In the post C.S.B. era, the focus shifts to the attempts by the Closer Settlement Commission to salvage the scheme and its greater understanding of the problems faced by the settlers. While this part of the thesis necessarily becomes more political, the physical and financial environment in which the soldier settlers worked was still an important factor in their success or failure. Unlike the C.S.B. which tended to blame soldier settlers for their situation, the Commission acknowledged that settlers' ability to succeed was often constrained by circumstances beyond their control. Under the latter administration, instalments were written off, additional land was allocated and finally the blocks were revalued to guarantee the men at least some equity in their farms. Those settlers who had survived until these changes were instituted received a 'successful outcome of their life's work'.

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24

Vázquez, Becerra Guadalupe Esteban. "Geodesy in Antarctica a pilot study based on the TAMDEF GPS network, Victoria Land, Antarctica /." Columbus, Ohio : Ohio State University, 2009. http://rave.ohiolink.edu/etdc/view?acc%5Fnum=osu1236711490.

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25

Pino, Ivano <1977&gt. "Monitoring Ice Velocity Field in Victoria Land (Antarctica) Using Cross-Correlation Techniques on Satellite Images." Doctoral thesis, Alma Mater Studiorum - Università di Bologna, 2008. http://amsdottorato.unibo.it/1177/.

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26

Mulumba, Lukman Nagaya. "Land use effects on soil quality and productitivity in the Lake Victoria Basin of Uganda." The Ohio State University, 2004. http://rave.ohiolink.edu/etdc/view?acc_num=osu1095711869.

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27

Vazquez, Becerra Guadalupe Esteban. "GEODESY IN ANTARCTICA: A PILOT STUDY BASED ON THE TAMDEF GPS NETWORK, VICTORIA LAND, ANTARCTICA." The Ohio State University, 2009. http://rave.ohiolink.edu/etdc/view?acc_num=osu1236711490.

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28

Mulumba, Lukman Nagaya. "Land use effects on soil quality and productivity in the Lake Victoria Basin of Uganda." Connect to this title online, 2004. http://rave.ohiolink.edu/etdc/view?acc%5Fnum=osu1095711869.

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Thesis (Ph. D.)--Ohio State University, 2004.
Title from first page of PDF file. Document formatted into pages; contains xv, 166 p.; also includes graphics (some col.). Includes bibliographical references (p. 134-153).

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29

Cleary, Susan J. Duffy Charles Gavan. "After the gold and the grass : the introduction of novel industries into the colony of Victoria 1862 to 1872 /." Title page, table of contents and abstract only, 2003. http://web4.library.adelaide.edu.au/theses/09ARM/09armc6234.pdf.

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30

Croggon, Janice. "Strangers in a strange land : converging and accommodating Celtic identities in Ballarat 1851-1901." University of Ballarat, 2002. http://archimedes.ballarat.edu.au:8080/vital/access/HandleResolver/1959.17/14598.

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"This thesis examines the paths by which four Celtic ethnic identities, Cornish, Welsh, Scottish and Irish, responded to the specific society and culture of the Victorian goldfields between 1850-1901. The individual Celtic groups intersected, harmonised and contested with each other in a process through which they retained their identities and yet managed to move towards becoming part of a larger, more-encompassing unity."
Doctor of Philosophy

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31

Mensing, Teresa Marie. "Geology and petrogenesis of the Kirkpatrick Basalt, Pain Mesa and Solo Nunatak, Northern Victoria Land, Antarctica /." The Ohio State University, 1987. http://rave.ohiolink.edu/etdc/view?acc_num=osu14873326364761.

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32

Yeung, Hoi-yan. "Property rights to views : a study of the history of reclamation in Victoria Harbour /." Hong Kong : University of Hong Kong, 2001. http://sunzi.lib.hku.hk/hkuto/record.jsp?B24521036.

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33

O'Toole, Timothy Finn. "The Lower Taylor Group: Taylor and Wright Valleys, southern Victoria Land, Antarctica; Paleoenvironmental Interpretations and Sequence Stratigraphy." Thesis, University of Canterbury. Department of Geological Sciences, 2010. http://hdl.handle.net/10092/4202.

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The Devonian Taylor Group (the lower Beacon Supergroup), in the Taylor and Wright Valleys, southern Victoria Land (SVL), Antarctica, is separated from basement by a regional nonconformity, the Kukri Erosion Surface. Thereafter the Taylor Group sediments, observed in this thesis, are affected by two localized unconformities; the Windy Gully Erosion Surface, separating the Terra Cotta Siltstone Formation (TCzst) and older units from the younger overlying New Mountain Sandstone; and the Heimdall Erosion Surface (HES), separating the New Mountain Sandstone Formation (NMSst) and older units from the overlying Altar Mountain Formation. The depositional environments of the Windy Gully Sandstone, New Mountain Sandstone and Altar Mountain Formations have long been under debate. The Kukri Erosion Surface (KES) truncates the crystalline basement and separates the basement rock from the overlying Beacon Supergroup. Interpretation of the erosion surface characteristics and the directly overlying basal conglomerate lithofacies (WG-BCL) suggest a high relief rocky shore platform environment during a sustained and significant relative sea level fall. The environment has been suggested to be similar to what is currently seen on the West Coast, New Zealand today. The Windy Gully Sandstone Formation directly overlies the KES and consists of a basal conglomerate (WG-BCL) followed by moderately to well sorted tabular and trough cross bedded felds- to subfeldsarenites. At one location an interbedded siltstone and cross bedded sandstone lithofacies was observed and interpreted as a tidal flat. Overall interpretation of the WGSst suggests continued progradation from a rocky shore platform (WG-BCL) to a series low angle beach, to shallow marine, and back to low angle beach environments. This occurred during a relative sea level rise. Shallowing of the water column produced a gradational relationship with the Terra Cotta Siltstone Formation (TCzst).. The fine to very fine sandy mottled, well laminated siltstones moving to very fine fissile dark siltstones suggest a progression from sandy estuarine to a mud flat environment. The Terra Cotta Siltsone is truncated by the Windy Gully Erosion Surface The Windy Gully Erosion Surface is observed in the Handsley Valley by the presence of TCzst rip-up clasts in the directly overlying New Mountain Sandstone Formation. Elsewhere the horizon is either very sharp or has desiccation cracks present suggesting a cessation of deposition and subaerial exposure respectively. This suggests a small relative fall in sea level with only localized erosion. The New Mountain Sandstone Formation (NMSst) predominantly consists of a series of low angle tabular and higher angle trough cross beds. It has a subfeldsarenite base that progressively becomes a pure quartz arenites. Interpretation suggests an initial beach environment with rejuvenated sediments moving to quartzose shallow marine and back to beach environments. This represents a relative sea level rise with continued progradation The NMSst is truncated in the north by the HES forming a characteristic saw tooth pattern in the cross bedded sandstones; elsewhere the HES is represented by a feldspathic influx moving into the Altar Mountain Formation. The HES was formed due to a significant relative sea level fall leading to exposure and erosion of lithified NMSst cross beds in the north but continuation of deposition in the south. The Altar Mountain Formation consists of tabular and trough cross bedded subfields- to feldsarenites. The Odin Arkose Member directly overlying the HES is a granule to cobble conglomerate in the north where the HES is erosional and very coarse sand to granule feldsarenite in the south where the HES is conformable. This has been interpreted as a pebbly shore platform to coarse sandy to granular beach environment. The following Altar Mountain Formation is interpreted as a continuation of medium to coarse sandy beach environments with influxes of coarser sediments and possibly moving into shallow marine in places. Sequence stratigraphy identifies three stratigraphic sequences: S1, the Windy Gully Sandstone and Terra Cotta Siltstone Formations; S2, the New Mountain Sandstone Formation; and S3, the Altar Mountain Formation. The first two sequences (S1&S2) show a clear progression through transgression to a high stand systems tract through regression to a low stand systems tract. The Altar Mountain Formation follows a very similar trend but due to the lack of time and data the above measures have been speculated. Zircon age dating suggests the source of the sediments in the area come from the Neoproterozic Skelton Group and the DV2a Granite Harbour Intrusives, both directly underlying the sandstones but are exposed elsewhere in SVL. Laminated sandstone clasts within the New Mountain Basal Conglomerate Lithofacies (NM-BCL) are suggested to be sourced from recycled sediments directly below. Other exotic clasts are also observed in the lithofacies are of unknown origin.

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34

Yeung, Hoi-yan, and 楊愷欣. "Property rights to views: a study of the history of reclamation in Victoria Harbour." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2001. http://hub.hku.hk/bib/B31242625.

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35

Mainville, Daniel Mark, and daniel mainville@dse vic gov au. "The Impacts of Agriculture and Plantation Forestry in a Selection of Upper Catchments of the Strzelecki Ranges, Victoria." RMIT University. Civil, Environmental and Chemical Engineering, 2007. http://adt.lib.rmit.edu.au/adt/public/adt-VIT20080509.162820.

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The intensive nature of land uses in the Strzelecki Ranges poses significant threats to landscape values and water quality. A comprehensive catchment strategy was developed based on sustainability science concepts incorporating the careful management of landscape values, proper land management approaches, and government policy and legislative change to ensure that agriculture, forestry and other land uses become sustainable in this sensitive environment. The readily measurable water quality indicators of turbidity, flow, electrical conductivity, and water temperature were used to determine the impacts of the major land uses in the Strzeleckis. From a water quality perspective, there was a trend of decreasing water quality with increasing intensity in land management. However, from a total sediment load perspective, the forest area contributed the highest total sediment load due to higher volumes of steam flow suggesting that natural processes in the Strzeleckis may remain the principal mechanisms for sediment movement within the catchment. An incidental but significant finding was extensive bioturbation along the riparian zone of the plantation area, the extent of which was not observed in the other catchments. This finding suggested that bioturbation may have been the most significant contributor to poorer water quality flowing from in the plantation catchment. The project developed insights into the major environmental processes active in the upper catchment of the Morwell River. Understanding of the contributions to total sediment loads from natural erosional processes and bioturbation, findings related to the impacts on water quality from agricultural practices, and encountering negligible impacts from conservative timber harvesting practices demonstrate that catchment management approaches need to be tailored to achieve sustainability in land uses across the landscape. Key recommendations include the re-establishment and protection of riparian zones in agricultural catchments, the careful assessment and setting of stream buffer zone widths for timber harvesting operations, and the need for further work to map the extent of natural processes such as bioturbation and stream bank erosion. To mitigate these issues, government policy and legislation will need to focus on the preservation and enhancement of the Crown land riparian zones. Recommended changes to current administrative land management arrangements for these sensitive areas include a move from licensing riparian zones for agricultural practices such as grazing to conservation.

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36

Morris, Jason C. "The groma and the gladius : Roman surveyors in the later Republic : a thesis submitted to the Victoria University of Wellington in fulfilment of the requirements for the degree of Master of Arts in Classics /." ResearchArchive@Victoria e-Thesis, 2010. http://hdl.handle.net/10063/1318.

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37

Laurent, Nathan R. "Mapping the landscape of public policy debate through analysis of evidence-based arguments in news media content: A case study." Thesis, Queensland University of Technology, 2016. https://eprints.qut.edu.au/98725/1/Nathan%20Laurent%20Thesis.pdf.

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This case study of the debate around broad-scale land-clearing in Queensland adds to knowledge about the place of news media in resolving public policy issues. It includes an historical account of the issue, and from the evidence of newspaper contents, observes that some parties in such debates are likely to only conditionally accept policy outcomes, such as enacted legislation. Focusing on the regulation of broad-scale land-clearing between 1998 and 2006, the study identifies, analyses, and compares relevant, evidence-based arguments from policy stakeholders published in two Queensland newspapers: a metropolitan daily and a rural industry weekly.

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38

Kenge, James Gunya. "Participatory watershed management to decrease land degradation and sediment transport in Kagera and Nyando catchments of Lake Victoria basin." Thesis, Linköping University, Department of Water and Environmental Studies, 2009. http://urn.kb.se/resolve?urn=urn:nbn:se:liu:diva-51952.

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Attention to participatory watershed management is increasing across the developing world as soil erosion continues to degrade agricultural land; reservoirs and irrigation infrastructure are clogged with sediment. The realization of the importance of watersheds is crucial for sustainable utilization especially in developing countries where rural livelihoods and economies are highly dependant on the exploitation of natural resources. The Lake Victoria basin is characterized by high population pressures, low productive subsistence agriculture, poor farming methods, loss of soil fertility and deforestation due to demand of fuel wood and charcoal, timber and building materials that are posing serious threat to watersheds. High population density in the basin also means new needs emerge too fast to which rural societies cannot respond in time leading to more area expansion for agricultural land. In spite of positive efforts under the Lake Victoria Basin Commission, there remains a huge gap between policy and institutional framework development at the top level and the actual implementation of actions on the ground to prevent land degradation, soil erosion and decrease sediment load. The study focused on Kagera and Nyando catchments of Lake Victoria Basin and aiming to establish if there exist and the extent to which participatory watershed management has been implemented on the ground to decrease land degradation and sediment load. It therefore provides an insight into watershed management in the Kagera and Nyando catchments by illustrating the link between policy formulation and actual implementation and enforcement.

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39

Siles, Brenda. "The Politics of Land Distribution: Ingenio Victoria de Julio- El Timal, a Case Study of Nicaraguan Rural Conflicts after 1990." ScholarWorks@UNO, 2016. http://scholarworks.uno.edu/honors_theses/77.

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One of the greatest legacies of the Sandinista Revolution was agrarian reform. Despite the amount of land redistributed, this process happened without any form of legal documentation to support the transfer of property from one owner to the next. The end of the civil war, the peace accords and the transition of power from left to right-wing parties produced conflicting policies that would bring high levels of complexity to the system of land tenure in the country. The case of the state-owned sugar mill, Ingenio Victoria de Julio – El Timal is of one the most emblematic examples of how slow and inefficient Nicaraguan institutions have been in solving land tenure issues in 26 years.

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40

MacGregor, Angus James. "A palaeoecological reconstruction of the Lower Snowy River, East Gippsland, Victoria : environmental response to climate change, land use, and river regulation /." Title page, contents and abstract only, 2001. http://web4.library.adelaide.edu.au/theses/09AEVH/09aevhm147.pdf.

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41

Elsner, Martin [Verfasser], Reinhard [Akademischer Betreuer] Gaupp, and Hilmar von [Akademischer Betreuer] Eynatten. "Triassic to early Jurassic sandstones in North Victoria Land, Antarctica : composition, provenance, and diagenesis / Martin Elsner. Gutachter: Reinhard Gaupp ; Hilmar von Eynatten." Jena : Thüringer Universitäts- und Landesbibliothek Jena, 2011. http://d-nb.info/1016555075/34.

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42

Oliveira, Adriano. "Using Blockchain to manage contracts for land clearing with sheep." Master's thesis, 2019. http://hdl.handle.net/10773/29422.

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Land clearing services are quickly spreading, mostly due to legal requirements imposed on field owners to force them to clean their terrains in order to prevent the spread of eventual wildfi res. These land clearing services are traditionally made with the help of machinery or chemicals, which is costly and heavy on the environment. An alternative is a process which is not a novelty in itself - bringing grazing animals, usually sheep, to the terrain, and have them eat the unwanted weeds. This is a cheaper and more environmental-friendly way of conducting a land clearing service. In order to increase the eficiency of this process, the SheepIT project was created, which brought the possibility of exerting a better control over the animals with the use of smart devices, which also enable valuable data collection. This dissertation is built on top of the SheepIT project and aims at being the bridge between owners of fields who intend on paying for these services, and the owners of sheep acting as service providers and looking to nd clients. The goal is to create a platform where they can publicize their intents, contractualize services and manage them. Blockchain technology was then used in order to guarantee the provenance and integrity of important data Flowing through the system, in order to generate trust between all the users of the platform.
Os serviços de limpeza de terreno estão rapidamente a ganhar popularidade, principalmente devido a requisitos legais impostos a donos de terrenos, que têm como objetivo a prevenção de eventuais fogos florestais. Estes serviços de limpeza são tradicionalmente feitos com recurso a maquinaria ou produtos químicos, o que acaba por ser um processo custoso e com impacto no ambiente. Uma solução alternativa é um processo que não é uma novidade por si só - o uso de animais de pastagem para a remoção das espécies vegetais indesejáveis. Esta é uma alternativa com um custo monetário e ambiental reduzido. Para aumentar a eficiência deste processo, o projeto SheepIT foi criado, e trouxe a possibilidade de exercer um melhor controlo sobre os animais através do uso de aparelhos eletrónicos, que simultaneamente permitem uma coleção de dados importantes. Esta dissertação acresce ao trabalho desenvolvido no projeto SheepIT, e tem como objetivo tornar-se uma ponte entre donos de terrenos que tencionam pagar por serviços de limpeza de terreno, e donos de rebanhos que atuam como prestadores desse serviço e estão à procura de clientes. O objetivo final é criar uma plataforma onde os utilizadores possam publicitar as suas intenções, contratualizar serviços de pastagem, e gerir os mesmos. A tecnologia blockchain é então usada para garantir a proveniência e integridade de dados importantes que passam pelo sistema, com o intuito de fomentar confiança entre os utilizadores da plataforma
Mestrado em Engenharia de Computadores e Telemática

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43

Schneider, Kathryn Erica. "Response of ant communities to vegetation clearing and habitat fragmentation in Central Queensland." 2004. http://arrow.unisa.edu.au:8081/1959.8/24953.

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Habitat fragmentation involves the break-up of continuous native vegetation into remnant patches that are set in a matrix of altered habitat. The consequences of habitat fragmentation include the loss of original habitat which is followed by reductions in remnant size that increase edge effects and reduce habitat quality, and also increase the isolation of remnants from one another. Habitat fragmentation is an international environmental concern that also effects Australia. Over the last ten years Queensland has been responsible for some ninety percent of the clearing occurring in Australia, and as a result recorded some of the highest vegetation clearing rates in the world.
thesis (PhDEnvironmentalManagement)--University of South Australia, 2004.

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44

Segger, Cara. "Landscapes in transition at the northern edge of downtown Victoria." 2005. http://hdl.handle.net/1828/735.

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45

Zwane, Alix Peterson. "Essays in environment and development." 2002. http://catalog.hathitrust.org/api/volumes/oclc/52628924.html.

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46

Sauter, Jennifer Anne. "Identifying land for community gardens in the City of Victoria: exploring the process of creating and conducting an urban agriculture land inventory." Thesis, 2014. http://hdl.handle.net/1828/5664.

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The City of Victoria is experiencing increased food insecurity due to its location on Vancouver Island in British Columbia, and a lack of food production in the city. The practice of urban agriculture presents a potential solution, enhancing food security by localizing resources, while increasing access and participation with local food production. Based on urban agriculture land inventories (UALIs) conducted in Portland, Vancouver and Nanaimo, my research evaluates and develops site selection criteria specific to Victoria for conducting a community garden land inventory focused on identifying land for allotment and commons gardens. I also examine the underlying barriers or supports for allotting land to urban agriculture in Victoria. To generate site selection criteria and explore the barriers and supports, I conducted interviews with urban agriculture experts, including city planners; community garden activists, educators and individuals involved in non-profits, and urban producers engaged in urban food production. The site selection criteria were further assessed as primary criteria for their application in GIS or secondary criteria to be considered during site visits. The final primary site selection criteria were land use and type, water availability (within 6.8 m), proximity to density users (within 400 m), minimum size thresholds of 1189.2 m2 for allotment gardens and 139.4 m2 for commons gardens, and excluding buildings, heritage designations, and protected green space. The analysis of the primary criteria resulted in a map illustrating 248 potential sites for community gardens in Victoria, whereby 213 were only suitable for commons gardens and 35 were suitable for allotment or commons gardens due to the larger size threshold. Four of the resulting sites were ground-truthed using site visits, and had medium to high potential for community gardens. The site visits documented secondary criteria, including proximity to community hub or prominent location, sunlight, ecologically sensitive area, cedar trees, and pollinator habitat or vegetation. Highlights from the interviews included identifying the most influential factors to allotting land to urban agriculture: the perception and awareness of urban agriculture, the community, the politics of City Council and staff support, and the costs or financial supports associated with community gardens. Overall, this research provides a model for the decision making process behind establishing an UALI, and contributes to understanding the challenges to allotting land to agriculture in the urban environment.
Graduate
0768
0473
jsauter@uvic.ca

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47

Winter, Diane Marie. "Diatom biostratigraphy and early to mid-Pliocene paleoecology, southern Victoria Land Basin, McMurdo Sound, Antarctica." 2009. http://proquest.umi.com/pqdweb?did=1694433091&sid=1&Fmt=2&clientId=14215&RQT=309&VName=PQD.

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Thesis (Ph.D.)--University of Nebraska-Lincoln, 2009.
Title from title screen (site viewed July 21, 2009). PDF text: xi, 160 p. : ill. (some col.), col. maps ; 5.84 Mb. UMI publication number: AAT 3350458. Includes bibliographical references. Also available in microfilm and microfiche formats.

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48

Mackin, Nancy. "Architecture, development and ecology : Garry Oak and Peri - urban Victoria." Thesis, 2000. http://hdl.handle.net/2429/10661.

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This thesis seeks to explain how site-scale design decisions can assist retention of rare plant communities concentrated in and near settled areas. To do so it focuses on a specific species and development context. Explanations are sought through examination of case studies of landuse developments in proximity to retained Garry oak plant communities located in the perimeter of Victoria, British Columbia. In the study region, exponential declines in species populations, health, and diversity of rare Garry oak ecosystems have been largely attributed to impacts from land-use developments. Over the past century, land-use developments have transformed the floral, spatial, structural and functional characteristics of the settled landscape. Isolated islands of imperiled plant associations remain on protected bioreserves: for recruitment and connectivity, these rare fauna rely on private-land greenways. Architectural teams have the potential to influence the decision-making processes that create ecologically-vital greenspace on private land, thereby enhancing survival for declining plant communities. Case-study evidence for the importance of land-use decisions on diminishing Garry oak meadow is gathered through vegetation surveys conducted on Garry oak meadow in proximity to six architectural projects on Victoria's western edge. Observed changes in growth extensions are then categorized in relation to human activities associated with built form, and correlated with principles from Landscape Ecology. An ARC of design strategies, developed in primary research by K. D. Rothley is adapted for architectural use as follows: firstly, AREA of a plant community is kept free of encroachment by the orderly frame established around vegetation; secondly, RARE SPECIES and habitat are identified with borders or signage; thirdly, CONNECTIVITY between retained landscapes is secured by siting roads and buildings to minimize ecosystem fragmentation. To effectively communicate preexisting landscape ecology principles, grouped under the ARC of strategies, illustrations and key-word phrases are developed. These principles, when integrated into architectural teams' structural knowledge, extend the architects' perceived role beyond aesthetics and economic efficiency. Enhancing habitat value through retention or restoration of rare ecosystems at the margins of suburban development, becomes an additional realm of influence for professional teams designing the spatial configurations of peri-urban landscapes.

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49

Kidd, Jeffrey N. "The development and investigation of a systems model of farm tourism in Victoria." Thesis, 2003. https://vuir.vu.edu.au/17940/.

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The marketing of farms for tourism and recreation purposes has been taking place for many years. Farmers have frequently sought to supplement their farm income through providing accommodation and recreation facilities to paying guests. This study concentrates on one state of Australia, Victoria, and has two main aims. The first aim is to develop a systems model of farm tourism that reveals the roles played by various stakeholders. The second aim is to examine farm tourism from a systems perspective, and to explore the attitudes of both farmers and guests to their experiences. In addition, the comments of local government authorities are also investigated. The purpose of the study, in broad terms, is to develop a systems model of farm tourism in Victoria, Australia. In order to do this, the study reviews the literature and then examines the evolution and development of farm tourism in general, through a detailed analysis of the relationships between host farm operators and their visitors. is hoped that the present study will shed some light on an industry which has been largely ignored by most writers and researchers in the different disciplines represented in this topic. The research objectives are, firstly, to develop a systems model of farm tourism; secondly, to examine and describe the scope of farm tourism in Victoria, from the point of view of the farmer; thirdly, to describe the evaluation of the farm tourism experience by the guests who have visited farms in Victoria; and, finally, to investigate the attitudes and involvement of local government bodies in Victoria to farm tourism. Tourism in general is examined, as well as the relationship between agriculture and tourism, leading to a discussion of the definition of rural tourism. General trends in rural tourism are identified, and their relevance to farm tourism is explained. The definition of farm tourism is then covered, with commentary on the application of the characteristics of tourism to the farm tourism industry. Trends in farming are mentioned, which point to the importance of farm tourism as an alternative source of income for the farmer, and a useful form of diversification from farm operations, reducing dependence on one source of income. The concepts of leisure and recreation are also considered, and their relevance to farm tourism is identified.

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50

Choudhury, Madhumita [Verfasser]. "Biodiversity and zoogeography of the Isopoda (Crustacea: Malacostraca) from the Victoria Land coast, Ross Sea, Antarctica / vorgelegt von Madhumita Choudhury." 2009. http://d-nb.info/995302103/34.

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