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2.2.4 Permanent water and groundwater flow<br />

The flooded landscape and very high water flows of the wet season are counterbalanced by<br />

the long dry season, where temporary water sources dry out. A poor wet season and long<br />

dry season can make the <strong>pre</strong>sence of permanent water sources vital <strong>to</strong> life in the area. Big<br />

lagoons such as Oriners and Mosqui<strong>to</strong> are very important at such times, and the following<br />

conversations are about how their levels are maintained.<br />

Marcus Bar<strong>be</strong>r: Those big lagoons, like the one next <strong>to</strong> Oriners and Mosqui<strong>to</strong> and<br />

Horseshoe. How come they stay there? Is it really deep or is there still water coming up<br />

from underneath? 19<br />

Ro<strong>be</strong>rt Burns: Must <strong>be</strong>. They don‟t go down much at all.<br />

Fred Coleman: Must <strong>be</strong><br />

Michael Ross: That‟s all s<strong>to</strong>ry places. Horseshoe [Lagoon] he‟s s<strong>to</strong>ry place. Horseshoe.<br />

Oriners is Moon s<strong>to</strong>ry, [and] around the corner, Crocodile s<strong>to</strong>ry. They all s<strong>to</strong>ry places. Big<br />

[important] water.<br />

Marcus Bar<strong>be</strong>r: So is there water under the ground coming up <strong>to</strong> keep them going?<br />

Ro<strong>be</strong>rt Burns: Yeah.<br />

Michael Ross: Because if it was just rain water, it would dry up like a dam, go away. Even<br />

last year the water was still the same, it was full.<br />

Fred Coleman: Even in my time working, I‟ve never seen it go dry. It always had water.<br />

Even if you go down <strong>to</strong> the junction, I‟ve never seen that go dry. And you get big fish there.<br />

Ro<strong>be</strong>rt Burns: Big water and big fish <strong>to</strong>o.<br />

Fred Coleman: Yeah, jewfish.<br />

---------------------------------------<br />

Oriners Lagoon, I don‟t think it would ever go dry, <strong>be</strong>cause it makes water. It makes water.<br />

Soaks. And Horseshoe Lagoon and Crocodile, and that other one over near Goose<br />

Swamp, that actually makes water there. You can see the bluey film in them, that‟s where<br />

that water comes in. You have a look on the edges of the water, you know when you see a<br />

spring and you can see that bluey tinge through it? Cloudy I suppose you could call it. I<br />

<strong>be</strong>lieve that is [water] coming in from the sides. Jewfish Lagoon I‟ve seen low. I reckon<br />

Jewfish would go dry. I don‟t know about Mosqui<strong>to</strong>, it‟s a bit more protected from<br />

evaporation. Emu Lagoon, that‟s one of the biggest lagoons. It nearly went dry, back in the<br />

sixties. George Murray <strong>to</strong>ld me that. He said it got so low the fish were dying. In Emu, and<br />

that‟s a big hole. You need a continuation of <strong>not</strong> much water flow [<strong>to</strong> dry out big holes]. You<br />

can get wet seasons <strong>with</strong> a fair bit of rain, but no big water flowing rain, like heavy stuff.<br />

Emu [Lagoon] is an overflow out of the Alice, that‟s what fills Emu up, and if the Alice does<br />

<strong>not</strong> run high enough [it does <strong>not</strong> fill]. And what can happen <strong>with</strong> those rivers <strong>to</strong>o is that if<br />

they don‟t get a good high flow, they‟ll actually build up sand along the anabranches. And<br />

the next year will run high, but <strong>be</strong>cause of the [increased] sand bank up there, it won‟t go<br />

in. So you need a<strong>not</strong>her big flush <strong>to</strong> take it out again.<br />

David Hughes<br />

Cecil Hughes commented that the creeks in the area s<strong>to</strong>pped every year, but that he had<br />

never seen Oriners waterhole dried out. He did <strong>not</strong> <strong>be</strong>lieve they were fed by groundwater,<br />

but rather were deep enough and held water well through the dry period. He had seen<br />

19 This conversation (and others on the same <strong>to</strong>pic) may have <strong>be</strong>nefitted from greater <strong>pre</strong>cision about<br />

water flowing from deeper underground via springs and rock fissures, and water seeping in<strong>to</strong> the sides<br />

of permanent holes from the surrounding water table.<br />

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

64

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