School of Geography - Theses
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ItemMelbourne's inner industrial zone: a study of industrial location( 1963)In most civilised communities, there are, within their history of development, certain stages in which primary production forms the major activity of the people. Gradually, changing social and economic conditions have created demand for the local manufacture of some goods. As the scope of the existing economy is broadened, secondary production becomes more prominent in the economic picture. Such development has been experienced by many countries of the world, and Australia, though still a comparatively young country, is no exception. Victoria has, for a long time, depended on her production and export of primary produce, especially wool, and wheat. The time has already come for the State to pay greater attention to its secondary industries, though not necessarily at the expense of primary production. It is perfectly clear that industrial development in Victoria is not recent at all, but equally true is the fact that secondary industry is still immature. The Melbourne metropolitan area, with its central position, its port and transport facilities and its concentration of population is undoubtedly the heart for manufacturing development. Industries in Melbourne, especially in the inner suburbs, are nearly as old as the State; but the amount of literature on the industrial development of Melbourne is limited Therefore, the purpose of this study is to present a general picture of the development of industries in this part of Australia, and the present industrial structure of what is termed the "Inner Industrial Zone" of Melbourne. The study is meant to explain and analyse the function and structure of industries, their growth and their spatial relations within the study area. The location and locational requirements of the dominant industrial groups will be discussed in greater detail and it is hoped that such a study wills lead to more interesting and important studies of the industrial development of the whole Metropolitan area or even of Victoria.
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ItemMultiple purpose river basin development: principles and practice in the Latrobe Valley of Victoria( 1968)No abstract available
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ItemThe historical geography of Australian coastal shipping( 1974)This thesis has been made possible by the help and encouragement of many, particularly during my later school years when shipping first became a serious interest, and I should like to thank generally both friends and waterfront personnel who took me on board various vessels or around the Sydney and Melbourne Waterfront complexes. Particular thanks for help during the preparation of this work go to Dr. T, M. Perry for his patient supervision and advice, and thanks to Staff of the Latrobe Library, Melbourne, of the public reference libraries at Adelaide, Launceston and Brisbane, and of university libraries at Melbourne, Monash and Queensland, for access to bound volumes of newspapers and periodicals, to several shipping companies for information about their services and history, and in particular to the Adelaide Steamship Company, the Australian National Line, and the State Shipping Service of Western Australia and their ships' crews for arranging visits to their ships. I should also like to acknowledge access to the Green and Dufty collection of ship photographs for reference.
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ItemAgriculture and land use in the Ovens and Kiewa River valleys of N. E. Victoria( 1964)No abstract available
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ItemRepresentation in the Australian House of Representatives 1890-1901( 1975)This is a study of certain territorial aspects of representation in the first Australian House of Representatives. It consists of two parts. The first part considers the way in which representation was to be divided amongst the States and Territories of the Commonwealth. The second part considers the way in which one State (Victoria) was first divided into constituencies. It is possible to examine the allocation of representation to areas and the selection of electoral boundaries at a variety of scales; from that of the members of an international organisation to that of the ridings of a shire. At the smaller scales, existing boundaries are, in most cases, adopted as electoral boundaries. At the larger scales new electoral boundaries are, in most cases, delimited. Nevertheless, the allocation of representation to areas and the selection of electoral boundaries are always interconnected. Each part of this study consists of two sections. The first section describes what took place, what alternatives were suggested and what arguments were used on both sides (Chapter Two and Chapter Four). The second section is, in each case, an attempt to evaluate what took place. The mechanism for allocating representation to the States and Territories is evaluated in two ways; first by investigating its internal consistency and implications and secondly by comparing the Australian provisions with those of other federations (Chapter Three). The first Victorian electoral distribution is evaluated by comparing it with two alternative distributions prepared at about the same time, both of which were eventually rejected (Chapter Five). The three distributions are compared by applying a range of techniques which together provide a method of evaluating any electoral distribution, or at least any where political parties may readily be identified. This study is limited to the period 1890 to 1901. Its implications are not. The mechanism for allocating representation to the States and Territories was to apply to future apportionments as well as to that of 1900. The questions that were raised by the first federal electoral distribution in Victoria have been echoed time and again in Australia; previously, subsequently and elsewhere.
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ItemA study of some of the relationships between geography and policy in the Australian dairy industry( 1973)No abstract available
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ItemThe development of the Port of Melbourne 1877-1971( 1974)The main purpose of this study is to describe and explain the physical and commercial development of the Port of Melbourne in the period 1877-1971. The year 1877 has been selected for the beginning of the study because it was the year in which the Melbourne Harbor Trust was established. The port has been modified in several ways since then and is now one of the most modern and best-equipped in the world. In tracing the port's evolution for nearly a century, the writer has tried to examine those factors, both human and physical, which have influenced its growth - world economic and political conditions, economic activities in its hinterland, policy decisions of the port authority and the national government and site conditions. The study does not encompass merely the physical development of the port, but also changes and trends in its trade and shipping. In addition, an attempt has been made to investigate those problems connected with the port's development. The growth and expansion of the manufacturing industries in the port district have also been considered. As well as these, the physical setting of the port, the discovery of Port Phillip Bay, Hobson's Bay and the River Yarra, the geology of the Yarra Delta, the condition of the port before 1877 and the genesis of the Melbourne Harbor Trust have been briefly referred to.
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ItemThe geomorphology of Mallacoota Inlet, East Gippsland( 1977)Mallacoota Inlet is an estuary located 537 kilometres by road east of Melbourne (Fig. 1.1). The estuary occupies a drowned river valley cut by the Genoa and Wallagaraugh Rivers at lower sea levels during the Pleistocene era. Mallacoota Inlet has a total shoreline length of 85 kilometres, a surface area of 25 x 106 square metres and a volume at low water of approximately 73 x 10 cubic metres, and is consequently the largest estuary or estuarine lagoon occurring east of the Gippsland Lakes. Two major hydrographic provinces may be differentiated within the Mallacoota system: (1) the basins, and (2) the linear channels. Three major basins comprise Mallacoota Inlet; the Upper Lake, the Lower Lake, and the North East Arm. A further, smaller basinal area is Double Creek Arm (Fig. 1.2). These basins differ in depth and sediment characteristics, and both these characteristics are related to the proximity to, and the source of, sediment within the Mallacoota system. The Upper Lake is a broad, shallow (less than three metres), and relatively flat bottomed basin with margins which are for the most part relatively gently sloping (Figs. 1.3 and 1.4). This basin, being closest to the point of river discharge, receives the greatest amount of fluvial sediment. On the other hand, the North East Arm is a relatively deep (up to six metres) flat bottomed basin with steeply sloping margins