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Figure 56. Land use map of the Mitchell catchment showing a) operating mines, abandoned<br />

mines, mine claims, proposed mines, b) distribution of major alluvial gullies, c) major paved<br />

and unpaved roads, d) existing and proposed water resource development, e) agricultural<br />

development near Dimbulah (green outline). Note the relatively sparse development in and<br />

around Oriners and Sef<strong>to</strong>n Stations.<br />

3.2.8 Surface hydrology<br />

The surface hydrology of water flow and discharge (magnitude, frequency, duration, timing,<br />

rate change) down creeks and de<strong>pre</strong>ssions around the forest country of Oriners and Sef<strong>to</strong>n<br />

has <strong>not</strong> <strong>be</strong>en studied in detail in the field „on country‟. This is also the case for small, shallow,<br />

oval wetlands (pans) and drainage de<strong>pre</strong>ssions (dambos) on the Holroyd Plain and larger<br />

lagoons in Quaternary alluvium, which are common in the area. It is likely that the timing and<br />

volume of runoff and water s<strong>to</strong>rage along these drainage networks are closely linked <strong>to</strong> the<br />

monsoon rainfall at the daily, seasonal and decadal scales (Figure 44; Figure 45; Figure 46).<br />

Horn (1995) reviewed the surface water hydrology of the Cape York Peninsula, but there are<br />

few data applicable <strong>to</strong> the Oriners area. No his<strong>to</strong>ric or current stream gauge stations exist in<br />

the Oriners region or Alice River catchment. <strong>CSIRO</strong> has developed water budgets (rainfallrunoff<br />

modelling) for the entire Mitchell-Alice catchment (Commonwealth Scientific and<br />

Industrial Research Organization (<strong>CSIRO</strong>) 2009) and well as sediment budgets (Rus<strong>to</strong>mji,<br />

Shell<strong>be</strong>rg et al. 2010). However, these modelling efforts are also hampered by a lack local<br />

gauge data and specific detail in the Alice catchment that are needed <strong>to</strong> validate and drive<br />

model efforts. Modelling results are also <strong>not</strong> detailed enough <strong>to</strong> infer local hydrological<br />

processes from, <strong>be</strong>yond basic climate data reviewed in Section 3.2.1.<br />

Due <strong>to</strong> the remoteness of the area and lack of local field data, satellite images and remote<br />

sensing have <strong>be</strong>en <strong>used</strong> <strong>to</strong> understand the seasonal flood inundation patterns of the area<br />

(Ward, Pusey et al. 2011). Ward et al. (2012) analysed Moderate Resolution Imaging<br />

Spectroradiometer (MODIS) satellite imagery (2003-2009) <strong>to</strong> estimate the visual inundation<br />

patterns and frequency of different parts of the Mitchell-Alice fluvial megafan. These data<br />

<strong>cover</strong>ed over a dozen flood events <strong>not</strong> obstructed by cloud <strong>cover</strong>. They provide minimum<br />

Working Knowledge at Oriners Station, Cape York<br />

148

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