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Relevant bibliographies by topics / Victoria Land

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Academic literature on the topic 'Victoria Land'

Author: Grafiati

Published: 4 June 2021

Last updated: 14 March 2023

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Journal articles on the topic "Victoria Land"

1

Ford, GW, JJ Martin, P. Rengasamy, SC Boucher, and A. Ellington. "Soil sodicity in Victoria." Soil Research 31, no. 6 (1993): 869. http://dx.doi.org/10.1071/sr9930869.

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This paper gives a broad overview of the distribution and agricultural importance of sodic soils in Victoria. Sodic soils are estimated to occupy at least 13.4 Mha, representing at least 73% of Victoria's agricultural land. Most of this land is used for dryland farming; about 85% of the cropped land and 66% of the land sown to dryland pastures occurs on sodic soils. The largest sodicity class is 'alkaline sodic', dominated by a diverse range of soils (red duplex, yellow duplex, calcareous earths and self-mulching cracking clays). Alkaline sodic soils comprise half of the total agricultural land area, or about 24% of the area of land currently used for dryland cropping and 21% of the land under sown pasture. Land degradation problems are recognized as affecting most agricultural land in Victoria, and to be substantially limiting its productivity. The nature, extent and severity of the various forms of land degradation are a consequence of both intrinsic soil properties and of management practices. There is an urgent need to improve current farming practices to prevent further deterioration of the soil resource. Existing knowledge of the behaviour of sodic soils under both dryland and irrigated agriculture is reviewed. It is concluded that substantial gains in productivity are possible, but will require effective collaboration between soil scientists, agronomists, and land managers. Collation and integration of current knowledge on the properties and management of sodic soils in Victoria, and the acquisition of additional relevant information by targeted long-term research is required. Key issues for future research are identified.

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Lisker, Frank, and Martin Olesch. "The rise of Kleinschmidt Bluffs (northern Victoria Land, Antarctica)." Zeitschrift der Deutschen Geologischen Gesellschaft 154, no. 4 (June 18, 2004): 427–36. http://dx.doi.org/10.1127/zdgg/154/2004/427.

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Smykla, Jerzy, Beata Krzewicka, Karina Wilk, Steven Emslie, and Lucyna Śliwa. "Additions to the lichen flora of Victoria Land, Antarctica." Polish Polar Research 32, no. 2 (January 1, 2011): 123–38. http://dx.doi.org/10.2478/v10183-011-0009-5.

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Additions to the lichen flora of Victoria Land, Antarctica Lichens of relict penguin colonies and sites affected by active penguin colonies were investigated in Victoria Land, Ross Sea sector, continental Antarctica. A total of 17 coastal sites, seven in northern and ten in southern Victoria Land, have been investigated across 7° of latitude from 71° to 78°S. Altogether 40 taxa of lichens have been identified. Four of the recorded species are new to the Antarctic - Caloplaca erecta, C. soropelta, C. tominii and Physcia tenella; two species are new to the Victoria Land area - Lecania nylanderiana and Lecanora polytropa. The first lichen records from Beaufort Island are also provided. Data presented here expand the knowledge on the occurrence, diversity and distribution of Victoria Land lichens.

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Rocchi, S., and J. L. Smellie. "Chapter 5.1b Northern Victoria Land: petrology." Geological Society, London, Memoirs 55, no. 1 (2021): 383–413. http://dx.doi.org/10.1144/m55-2019-19.

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AbstractCenozoic magmatic rocks related to the West Antarctic Rift System crop out right across Antarctica, in Victoria Land, Marie Byrd Land and into Ellsworth Land. Northern Victoria Land, located at the northwestern tip of the western rift shoulder, is unique in hosting the longest record of the rift-related igneous activity: plutonic rocks and cogenetic dyke swarms cover the time span fromc.50 to 20 Ma, and volcanic rocks are recorded from 15 Ma to the present. The origin of the entire igneous suite is debated; nevertheless, the combination of geochemical and isotopic data with the regional tectonic history supports a model with no role for a mantle plume. Amagmatic extension during the Cretaceous generated an autometasomatized mantle source that, during Eocene–present activity, produced magma by small degrees of melting induced by the transtensional activity of translithospheric fault systems. The emplacement of Eocene–Oligocene plutons and dyke swarms was focused along these fault systems. Conversely, the location of the mid-Miocene–present volcanoes is governed by lithospheric necking along the Ross Sea coast for the largest volcanic edifices; while inland, smaller central volcanoes and scoria cones are related to the establishment of magma chambers in thicker crust.

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Smellie, John L., and Sergio Rocchi. "Chapter 5.1a Northern Victoria Land: volcanology." Geological Society, London, Memoirs 55, no. 1 (2021): 347–81. http://dx.doi.org/10.1144/m55-2018-60.

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AbstractNeogene volcanism is widespread in northern Victoria Land, and is part of the McMurdo Volcanic Group. It is characterized by multiple coalesced shield volcanoes but includes a few relatively small stratovolcanoes. Two volcanic provinces are defined (Hallett and Melbourne), with nine constituent volcanic fields. Multitudes of tiny monogenetic volcanic centres (mainly scoria cones) are also scattered across the region and are called the Northern Local Suite. The volcanism extends in age between middle Miocene (c.15 Ma) and present but most is <10 Ma. Two centres may still be active (Mount Melbourne and Mount Rittmann). It is alkaline, varying between basalt (basanite) and trachyte/rhyolite. There are also associated, geographically restricted, alkaline gabbro to granite plutons and dykes (Meander Intrusive Group) with mainly Eocene–Oligocene ages (52–18 Ma). The isotopic compositions of the plutons have been used to infer overall cooling of climate during the Eocene–Oligocene. The volcanic sequences are overwhelmingly glaciovolcanic and are dominated by ‘a‘ā lava-fed deltas, the first to be described anywhere. They have been a major source of information on Mio-Pliocene glacial conditions and were used to establish that the thermal regime during glacial periods was polythermal, thus necessitating a change in the prevailing paradigm for ice-sheet evolution.

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Folco, L., P. Rochette, N. Perchiazzi, M. D'Orazio, M. A. Laurenzi, and M. Tiepolo. "Microtektites from Victoria Land Transantarctic Mountains." Geology 36, no. 4 (2008): 291. http://dx.doi.org/10.1130/g24528a.1.

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De Domenico, Francesca, Mariachiara Chiantore, Sabrina Buongiovanni, Maria Paola Ferranti, Serena Ghione, Simon Thrush, Vonda Cummings, Judi Hewitt, Kerstin Kroeger, and Riccardo Cattaneo-Vietti. "Latitude versus local effects on echinoderm assemblages along the Victoria Land coast, Ross Sea, Antarctica." Antarctic Science 18, no. 4 (November 14, 2006): 655–62. http://dx.doi.org/10.1017/s095410200600068x.

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Data from two new cruises is used to assess whether latitude plays any role in influencing broad-scale spatial patterns in echinoderm assemblage composition along the Victoria Land coast and the Balleny Islands as a contribution to the Latitudinal Gradient Project. Our results indicate that a latitudinal gradient is influencing assemblage structure in subtle and non-linear ways. The Balleny Islands system is different from the Victoria Land coast, probably because of a different biogeographic origin and current oceanographic conditions. Along the Victoria Land coast, latitude related differences arise when taking into account benthic biodiversity at different spatial scales. Alpha diversity increases from north to south, but beta diversity shows the opposite trend, although not linearly, suggesting the different importance of the iceberg disturbance along the northern Victoria Land coast.

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Berkman, Paul Arthur, Riccardo Cattaeno-Vietti, Mariachiara Chiantore, Clive Howard-Williams, Vonda Cummnigs, and Rikk Kvitek. "Marine research in the Latitudinal Gradient Project along Victoria Land, Antarctica." Scientia Marina 69, S2 (December 30, 2005): 57–63. http://dx.doi.org/10.3989/scimar.2005.69s257.

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Brotzu, Pietro, Giuseppe Capaldi, Lucia Civetta, Giovanni Orsi, Gabriella Gallo, and Leone Melluso. "Geochronology and geochemistry of Ferrar rocks from North Victoria Land, Antarctica." European Journal of Mineralogy 4, no. 3 (June 11, 1992): 605–18. http://dx.doi.org/10.1127/ejm/4/3/0605.

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Brunetti, Claudia, Henk Siepel, Peter Convey, Pietro Paolo Fanciulli, Francesco Nardi, and Antonio Carapelli. "Overlooked Species Diversity and Distribution in the Antarctic Mite Genus Stereotydeus." Diversity 13, no. 10 (October 19, 2021): 506. http://dx.doi.org/10.3390/d13100506.

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In the harsh Antarctic terrestrial ecosystems, invertebrates are currently confined to sparse and restricted ice free areas, where they have survived on multi-million-year timescales in refugia. The limited dispersal abilities of these invertebrate species, their specific habitat requirements, and the presence of geographical barriers can drastically reduce gene flow between populations, resulting in high genetic differentiation. On continental Antarctica, mites are one of the most diverse invertebrate groups. Recently, two new species of the free living prostigmatid mite genus Stereotydeus Berlese, 1901 were discovered, bringing the number of Antarctic and sub-Antarctic species of this genus up to 15, of which 7 occur along the coast of Victoria Land and in the Transantarctic Mountains. To examine the biodiversity of Stereotydeus spp., the present study combines phylogenetic, morphological and population genetic data of specimens collected from nine localities in Victoria Land. Genetically distinct intraspecific groups are spatially isolated in northern Victoria Land, while, for other species, the genetic haplogroups more often occur sympatrically in southern Victoria Land. We provide a new distribution map for the Stereotydeus species of Victoria Land, which will assist future decisions in matters of the protection and conservation of the unique Antarctic terrestrial fauna.

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Dissertations / Theses on the topic "Victoria Land"

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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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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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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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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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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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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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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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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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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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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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Books on the topic "Victoria Land"

1

Stump, Edmund, ed. Geological Investigations in Northern Victoria Land. Washington, D. C.: American Geophysical Union, 1986. http://dx.doi.org/10.1029/ar046.

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Edmund, Stump, ed. Geological investigations in northern Victoria land. Washington, D.C: American Geophysical Union, 1986.

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N, Wikrama-Nayake P., and Voumard L. C. 1898-1974, eds. The sale of land in Victoria. 4th ed. North Ryde, N.S.W: Law Book Co., 1986.

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Baker, Wendy. Searching land records in Victoria: An introduction. Melbourne: Genie Press, 1999.

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Caldere, D. B. Aboriginal reserves & missions in Victoria. [Melbourne]: Aboriginal Lands Group, Dept. of Conservation and Environment, 1991.

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Judith, Ryan, ed. Spirit in land: Bark paintings from Arnhem Land in the National Gallery of Victoria. [Melbourne, Vic.]: The Gallery, 1990.

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1984-1985), German Antarctic North Victoria Land Expedition (4th. German Antarctic North Victoria Land Expedition 1984/85: GANOVEX IV. Hannover: Bundesanstalt für Geowissenschaften und Rohstoffe und den Geologischen Landesärmtern in der Bundesrepublik Deutschland, 1989.

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Victoria. Office of the Auditor-General. Land use and development in Victoria: The State's planning system. Melbourne, Vic.]: Victorian Auditor-General Office, 1999.

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Clode, Danielle. As if for a thousand years: A history of Victoria's Land Conservation and Environment Conservation Councils. Melbourne: Victorian Environmental Assessment Council, 2006.

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Victoria, Art Gallery of Greater. The land of the rising sun: Arts of Japan. Victoria, B.C: Art Gallery of Greater Victoria, 1998.

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Book chapters on the topic "Victoria Land"

1

Faure, Gunter, and Teresa M. Mensing. "Northern Victoria Land." In The Transantarctic Mountains, 99–144. Dordrecht: Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-90-481-9390-5_4.

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Faure, Gunter, and Teresa M. Mensing. "Glaciaton of Southern Victoria Land." In The Transantarctic Mountains, 693–758. Dordrecht: Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-90-481-9390-5_19.

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Faure, Gunter, and Teresa M. Mensing. "Southern Victoria Land; Basement Rocks." In The Transantarctic Mountains, 67–97. Dordrecht: Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-90-481-9390-5_3.

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Bockheim, James G. "Soils of North Victoria Land." In World Soils Book Series, 107–16. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-05497-1_7.

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Calkin, Parker E. "Glacial Geology of the Victoria Valley System, Southern Victoria Land, Antarctica." In Antarctic Snow and Ice Studies II, 363–412. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/ar016p0363.

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Pondrelli, S., and R. Azzara. "Upper Mantle Anisotropy in Victoria Land (Antarctica)." In Geodynamics of Lithosphere & Earth’s Mantle, 433–42. Basel: Birkhäuser Basel, 1998. http://dx.doi.org/10.1007/978-3-0348-8777-9_10.

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Hammer, William R. "Takrouna formation fossils of northern Victoria Land." In Geological Investigations in Northern Victoria Land, 243–47. Washington, D. C.: American Geophysical Union, 1986. http://dx.doi.org/10.1029/ar046p0243.

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Babcock, R. S., C. C. Plummer, J. W. Sheraton, and C. J. Adams. "Geology of the Daniels Range, north Victoria Land, Antarctica." In Geological Investigations in Northern Victoria Land, 1–24. Washington, D. C.: American Geophysical Union, 1986. http://dx.doi.org/10.1029/ar046p0001.

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Adams, C. J. "Age and ancestry of metamorphic rocks of the Daniels Range, Usarp Mountains, Antarctica." In Geological Investigations in Northern Victoria Land, 25–38. Washington, D. C.: American Geophysical Union, 1986. http://dx.doi.org/10.1029/ar046p0025.

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Wodzicki, Antoni, and Ray Robert. "Geology of the Bowers Supergroup, central Bowers Mountains, northern Victoria Land." In Geological Investigations in Northern Victoria Land, 39–68. Washington, D. C.: American Geophysical Union, 1986. http://dx.doi.org/10.1029/ar046p0039.

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Conference papers on the topic "Victoria Land"

1

Geletti, R., M. Pipan, A. Battigelli, and A. Del Ben. "New Seismic Evidences in the Victoria Land Basin, Antarctica." In 62nd EAGE Conference & Exhibition. European Association of Geoscientists & Engineers, 2000. http://dx.doi.org/10.3997/2214-4609-pdb.28.p192.

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"The Valuation of Rural Leasehold Land in Victoria, Australia." In 16th Annual European Real Estate Society Conference: ERES Conference 2009. ERES, 2009. http://dx.doi.org/10.15396/eres2009_351.

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Casacchia, Ruggero, Rosamaria Salvatori, and A. Petrangeli. "Geologic mapping in Victoria Land, Antarctica, based on multispectral satellite data." In Satellite Remote Sensing II, edited by Joan B. Lurie, James J. Pearson, and Eugenio Zilioli. SPIE, 1995. http://dx.doi.org/10.1117/12.226805.

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Arias, Austin Tanner, Jung-Woo Park, Sang-Bong Yi, and Mi Jung Lee. "Petrogenesis of the Niagara Icefalls Ultramafic-Mafic Complex, Northern Victoria Land, Antarctica." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.80.

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Morse-McNabb, Elizabeth, Kathryn Sheffield, and Rob Clark. "Time series analysis of MODIS EVI data for regular land cover mapping in Victoria, Australia." In IGARSS 2013 - 2013 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2013. http://dx.doi.org/10.1109/igarss.2013.6723530.

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Raisbeck, Peter. "Reworlding the Archive: Robin Boyd, Gregory Burgess and Indigenous Knowledge in the Architectural Archive.” between Architecture and Engineering." In The 38th Annual Conference of the Society of Architectural Historians Australia and New Zealand. online: SAHANZ, 2022. http://dx.doi.org/10.55939/a3985p56dc.

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In her book Decolonising Solidarity: Dilemmas and Directions for Supporters of Indigenous Struggles, Clare Land suggest how non-Indigenous people might develop new frameworks supporting Indigenous struggles. Land argues research is deeply implicated with processes of colonisation and the appropriation of indigenous knowledge. Given that architectural archives are central to the research of architectural history, how might these archives be decolonised? This paper employs two disparate archives to develop a framework of how architectural archivists might begin to decolonise these archives. Firstly, these archives are the Grounds Romberg and Boyd Archive (GRB) at the State Library of Victoria (SLV). Secondly, the Greg Burgess Archive is now located at Avington, Sidonia in Victoria. The materials from each of these archives will be discussed in relation to two frameworks. These are the Tandanya-Adelaide Declaration endorsed by The Australian Society of Archivists (ASA) and the Indigenous Cultural and Intellectual Property (ICIP) framework developed by Janke (2019). These archival frameworks suggest how interconnected architectural histories and historiographies might be read, reframed and restored. Decolonising architectural archives will require a continuous process of reflection and political engagement with collections and archives. In pursuing these actions, archivists and architectural historians can begin to participate in the indigenous Reworlding of the archive.

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Lozej, A., I. Tabacco, F. Merlanti, and M. Pavan. "Preliminary Results of Seismic and GPR Surveys on the Hells Gate lce Shelf (Victoria Land -Antarctica)." In 1st EEGS Meeting. European Association of Geoscientists & Engineers, 1995. http://dx.doi.org/10.3997/2214-4609.201407430.

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Hur, Soon Do, Sang-Bum Hong, Heejin Hwang, Khanghyun Lee, Yeongcheol Han, Jinho Ahn, Ji-Woong Yang, and Youngjoon Jang. "Reconstruction of Past Climate and Environmental Changes Using High Resolution Ice Core Records in Victoria Land, Antarctica." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.1117.

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Kim, Daeyeomg, Munjaef Park, and Sung-Hyun Park. "Microstructures of Mantle Peridotites and their Implications on Seismic Anisotropy Around Mt. Melbourne, Northern Victoria Land, Antarctica." In Goldschmidt2020. Geochemical Society, 2020. http://dx.doi.org/10.46427/gold2020.1298.

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Sheffield, Kathryn, and Elizabeth Morse-McNabb. "Creating an historical land cover data set for the Wimmera region, Victoria, Australia from the USGS Landsat archive." In IGARSS 2013 - 2013 IEEE International Geoscience and Remote Sensing Symposium. IEEE, 2013. http://dx.doi.org/10.1109/igarss.2013.6723367.

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Reports on the topic "Victoria Land"

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Kerrigan, Susan, Phillip McIntyre, and Marion McCutcheon. Australian Cultural and Creative Activity: A Population and Hotspot Analysis: Ballarat. Queensland University of Technology, 2020. http://dx.doi.org/10.5204/rep.eprints.206963.

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Description Ballarat sits on Wathaurong land and is located at the crossroads of four main Victorian highways. A number of State agencies are located here to support and build entrepreneurial activity in the region. The Ballarat Technology Park, located some way out of the heart of the city at the Mount Helen campus of Federation University, is an attempt to expand and diversify the technology and innovation sector in the region. This university also has a high profile presence in the city occupying part of a historically endowed precinct in the city centre. Because of the wise preservation and maintenance of its heritage listed buildings by the local council, Ballarat has been used as the location for a significant set of feature films, documentaries and television series bringing work to local crews and suppliers. With numerous festivals playing to the cities strengths many creative embeddeds and performing artists take advantage of employment in facilities such as the Museum of Australian Democracy at Eureka. The city has its share of start-ups, as well as advertising, design and architectural firms. The city is noted for its museums, its many theatres and art galleries. All major national networks service the TV and radio sector here while community radio is strong and growing.

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