Academic literature on the topic 'Land subdivision Victoria'

Cities are facing dramatic challenges due to population growth and the massive development of high-rises and complex structures, both above and below the ground surface. Decision-makers require access to an efficient land and property information system, which is digital, three-dimensional (3D), spatially accurate, and dynamic containing interests in land (rights, restrictions and responsibilities—RRRs) to manage the legal and physical complexities of urban environments. However, at present, building subdivision workflows only support the two-dimensional (2D) building subdivision plans in PDF or image formats. These workflows result in a number of issues, such as the plan preparation being complex, the examination process being labor intensive and requiring technical expertise, information not being easily reusable by all subdivision stakeholders, queries, analyses, and decision-making being inefficient, and the RRRs interpretation being difficult. The aim of this research is to explore the potential of using Building Information Modelling (BIM) and its open standards to support the building subdivision workflows. The research that is presented in this paper proposes a BIM-driven building subdivision workflow, evaluated through a case study in the state of Victoria, Australia. The results of the study confirmed that the proposed workflow could provide a feasible integrated mechanism for stakeholders to share, document, visualize, analyze, interpret, and reuse 3D digital cadastral data over the lifespan of a building subdivision project.

Detailed geological mapping and geochemical analysis of early Palaeozoic granitoid plutons and dykes from the Taylor Valley and Ferrar Glacier region in south Victoria Land reveal two distinct suites. This suite subdivision-approach is a departure from previous lithology-based schemes and can be applied elsewhere in south Victoria Land. The older calc-alkaline Dry Valleys 1 suite is dominated by the compositionally variable Bonney Pluton, a flow-foliated concordant pluton with an inferred length of over 100 km. Plutons of this suite are elongate in a NW-SE direction and appear to have been subjected to major structural control during their emplacement. The younger alkali-calcic Dry Valleys 2 suite comprises discordant plutons and numerous dyke swarms with complex age relationships. Field characteristics of this suite indicate that it was passively emplaced into fractures at higher levels in the crust than the Dry Valleys 1 suite. Whole-rock geochemistry confirms this suite subdivision based on field relationships and indicates that the two suites were derived from different parent magmas by fractional crystallization. The Dry Valleys 1 suite resembles Cordilleran I-type granitoids and is inferred to be derived from partial melting of the upper mantle and/or lower crust above an ancient subduction zone. The Dry Valleys 2 suite resembles Caledonian I-type granitoids and may have resulted from a later episode of crustal extension.

An examination of planned suburbanisation is provided in this study through a discussion of the activities of the Home Smith and Company, and in particular, by an examination of the development and building of one of the Company's premier subdivisions, Kingsway Park. The study presents further evidence that the inter-war period encompassed a pivotal period in the evolving city-building process, bridging the transition between the fragmentary system employed in building the Victorian suburbs and the highly integrated land development process in place today.

During the late 1700s, the Kadohadacho (hereafter Caddo), a peaceful tribe of agriculturists and hunters, weakened by near-constant pressure from the more war-like Osage and the ravages of various epidemics, began to migrate from their traditional homeland near the Great Bend of the Red River south into northwestern Louisiana and adjacent East Texas. By the time of the Louisiana Purchase in 1803, the Caddo villages under their caddi Dehahuit were concentrated in the Sodo Lakes region west and northwest of modern-day Shreveport. Much of what we know today about the location of these settlements, and specifically Dehahuit’s village, are found in the writings of Indian agents and the field notes and plat maps of period surveyors. In this article we will examine these and other relevant documents and present a case for the location of the village of this historic figure. It is the contention of the author, based on material to be presented in the pages to follow, that Dehahuit’s village will ultimately be found to lie northwest of Waskom, Texas on the southern terraces of Paw Paw Bayou beneath the neatly manicured lawns of the Victoria Wood subdivision. The site is depicted on the 1838 American surveys of northwestern Louisiana as lying on the Natchitoches-to-Pecan Point Road on the section line between Sections 2 and 3 of T17N, R17W. In support of this argument, we will examine in this article (1) a relatively definitive 1840 statement regarding the location of Dehahuit’s village by Jehiel Brooks, long-time Caddo Agent and the individual who engineered the sale of the Caddo lands to the United States; (2) the well-known 1805 statement of Red River Agent John Sibley in which he noted that the Caddo lived some 35 miles west of the Red River on a bayou “called, by them, Sodo;” and (3) a memorial statement by the Caddo themselves regarding the re-location of some of their villages as required by Article 4 of the 1835 treaty cession.