WEST KIMBERLEY PLACE REPORT - Department of Sustainability ...
WEST KIMBERLEY PLACE REPORT - Department of Sustainability ...
WEST KIMBERLEY PLACE REPORT - Department of Sustainability ...
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A NATURAL AND CULTURAL REFUGE<br />
For the people who live here, whether Traditional Owners or more recent arrivals, the<br />
west Kimberley is home; for scientists, it is largely a tantalising unknown. The<br />
Kimberley is vast and remote from southern centres. Travel is difficult during the wet<br />
season, and many parts cannot be reached by ordinary means <strong>of</strong> transport at any time<br />
<strong>of</strong> year. Along the coast, there are saltwater crocodiles and massive, powerful tides.<br />
The west Kimberley coast, particularly at King Sound and Roebuck Bay, has the<br />
greatest tidal range <strong>of</strong> any coastal area in Australia, and one <strong>of</strong> the greatest in the<br />
world. Spring tides can reach up to 12 metres, and there are two tidal cycles each day.<br />
The west Kimberley is also remarkable for having the most convoluted coastline in<br />
Australia: it is comprised <strong>of</strong> an enormous number <strong>of</strong> islands, bays, coves and inlets,<br />
which appear as an impossible tangle <strong>of</strong> lines on a map.<br />
While most <strong>of</strong> the region has not yet been studied in detail, what survey work has<br />
taken place indicates that the Kimberley is home to a highly diverse range <strong>of</strong> plants<br />
and animals, and includes many species that live nowhere else (endemics), as well as<br />
species that are under threat or have now disappeared elsewhere in Australia. Some <strong>of</strong><br />
the factors that make the Kimberley most challenging to study also make it a refuge –<br />
providing greater resilience from introduced species and human actions, from<br />
seasonal scarcity, and from longer term changes in climate – allowing unique<br />
communities <strong>of</strong> species to thrive.<br />
Kimberley country ranges from coastal mangroves and eucalypt woodlands, through<br />
rugged ranges, flat-topped mesas and deep gorges, to rich pockets <strong>of</strong> rainforest and<br />
savanna grasslands. Rainfall, geology, topography, soil types, and associated plants<br />
and animals all vary significantly between the coast and inland, and from north to<br />
south. For descriptive purposes, the west Kimberley mainland is divided into four<br />
regions, reflecting changes in rainfall and geology: the north Kimberley, including the<br />
Mitchell Plateau and the northern and north-western coastline; Yampi Peninsula;<br />
central Kimberley, which includes the King Leopold, Napier, Oscar, Pillara and<br />
Emmanuel ranges; and the south-west, made up <strong>of</strong> Dampier Peninsula and the<br />
catchment <strong>of</strong> the Fitzroy River. The multitude <strong>of</strong> islands and reefs and other<br />
outstanding marine features which lie <strong>of</strong>f the coast are also described.<br />
North Kimberley<br />
The north Kimberley is an extensive area <strong>of</strong> rugged tablelands and distinctive flattopped<br />
mesas stretching from Cape Londonderry in the north to Harding Range in the<br />
south, and includes the Carson Escarpment, Mitchell Plateau (Ngauwudu to its<br />
Wanjina–Wunggurr Traditional Owners) and Gardner Plateau. This is the wettest part<br />
<strong>of</strong> the Kimberley: between 1,100 and 1,500 millimetres <strong>of</strong> rain falls on average each<br />
year, mostly in the summer months. The area has high biodiversity values, including<br />
the richest mammal populations in the west Kimberley, and is home to many endemic<br />
species. The greatest diversity <strong>of</strong> plant and animal species in the Kimberley is found<br />
in the coastal strip from the Mitchell Plateau north-east to Drysdale River.<br />
The geology <strong>of</strong> the north Kimberley is dominated by sandstones, dolerites and other<br />
volcanic rocks. Ancient rocks usually buried deep below Earth's surface are exposed<br />
here. In places, these basement strata have been worn through by rivers, showing both<br />
the long geological stability <strong>of</strong> the region which has allowed such features to be<br />
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