Resource Management and Geography - Theses
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ItemThe physiography of coastal dunes, East Gippsland, Victoria( 1978)Coastal Dunes – East Gippsland. Coastal dunes occur extensively in south-east and East Gippsland, Victoria (Fig 1.1). Bird (1965, 1978) and Jenkin (1968) discuss the geomorphology and Quaternary history of the Gippsland Lakes region, outlining several stages of barrier and dune formation. The outermost barrier extends from Corner Inlet to Red Bluff as the gently curving Ninety Mile Beach, interrupted only by intermittent stream outlets and the artificial opening at Lakes Entrance. Along its entire length the barrier is surmounted by dunes behind which lie elongated lagoons and salt marsh. Landward of these are earlier formed barriers. The coastal hinterland is a lowland with relict coastal terraces mantled by fluvial and Aeolian deposits. Active dunes are confined to the narrow outer barrier but older stabilized dune systems occur on the earlier barriers and the coastal terraces. The East Gippsland coast is here considered to extend from Lake Tyers to Cape Howe at the New South Wales border. East of Lake Tyers, the foothill ranges of the Eastern Highlands are closer to the coast and Palaeozoic and Tertiary rocks form bluffs and bold headlands. The sequence of parallel barriers and lagoons is less well defined and the zone of Quaternary coastal deposits less continuous. Sandy shoreline however is dominant – of the 185 kilometres of ocean coast between Lake Tyers and Cape Howe, approximately 145 kilometres (78%) is backed by sand deposits that range from a mere fringe to a broad zone up to 7 kilometres wide. (From Introduction)
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ItemSquatters, merchants and mariners: an historical geography of Gipps' Land 1841-1851( 1975)This thesis is a study of some of the processes which created a new geography in a particular region of Australia. Though localised in space it has a wider relevance for the study of its time, for this regional settlement was not an isolated, unique expansion but part of a nation-wide and world-wide movement. And though localised in time, it has a wider relevance for the study of this particular region because the patterns established in these few years set a framework which endures in many respects to the present. The study presents a reconstruction of the geography of a region for the first decade of its settlement, its pioneering phase, by tracing the establishment, growth and change in themes which created the regional character. By looking at the region as an open system, the influence of external forces is studied to see what effect these had on regional development.