Landscape setting
The Dampier Archipelago is on the Indian Ocean coast of the Pilbara of Western Australia. It is made up of 42 islands and islets of which Dampier Island is the largest. As a result of industrial development, Dampier Island is now an artificial peninsula known as the 'Burrup Peninsula'. The rugged landscape with its massive boulder-strewn ridges, plateaus and steep-sided valleys contrasts markedly with the broad low-lying plain of the mainland.
A series of ridges and rocky hills made up of massive boulders dominates the landscape of the Archipelago. These result from ancient weathering and erosion of the pre-Cambrian volcanic lava flows. The dominant rock type is granophyre, particularly on the western side, though gabbro, granite and dolerite also occur. Steep-sided valleys provide access corridors through the rugged terrain and are important sources of water and shelter. The coastline offers a complex array of different environments including rocky shores, sandy beaches, tidal mudflats and mangroves.
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Soils in the area are generally shallow and plant cover sparse. The dominant vegetation of the area is spinifex grassland. However, the complex topography has created a range of micro-habitats which support a variety of specialised plant and animal communities. These include a high number of plant species normally only found much further north in the Kimberley region. Many of these are edible and provided important food resources for Aboriginal people.
Water is scarce in the Archipelago and there are no permanent surface sources. The climate is characterised by high summer temperatures and erratic rainfall affected both by southern winter rainfall pattern and northern tropical cyclones. The valley systems carry ephemeral creeks with rock pools which act as natural cisterns. Freshwater soaks are also found. These would have been of critical importance to the people of the area.
The first settlement of Australia occurred by about 50,000 years ago during the last major glacial period, or Ice Age, when global climates were generally cooler than today, the polar ice caps were much larger and sea levels were up to 130m lower. At this period the 'Dampier Ranges' would have been a series of low rocky hills and ridges rising out of a flat plain and the sea would have been more than 100km distant. The Dampier Archipelago in its present form is a drowned landscape. It formed over several thousand years as the polar ice caps melted and sea levels rose at the end of the last Ice Age. The shoreline stabilised about 6000 years ago, forming rock platforms and boulder beaches with gradual accumulation of sand and silt in more sheltered bays. The complex terrestrial and marine ecosystems of the Archipelago and the resulting abundance and diversity of animals and plants would have provided particularly rich resources for Aboriginal people. However, the sheltered valleys and relatively reliable water sources of the rugged landscape would also have provided an important focus for people at times of lowered sea level.
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