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Emberson, Rowan The Speleological Society 1998 Journal of the speleological society of korea Vol.7 No.2
The Bullock Creek Caves are located adjacent to the usually dry river bed of Bullock Creek, which reaches the sea about a kilometer north of Punakaiki. The caves have been comprehensively written up by Rodgers(l972). Under conditions of normal water flow Bullock Creek submerges where the stream meets limestone on the west side of thier Punakaiki syncline. In flood conditions it overflows the first submergence and progressively floods a series of smaller submergences down valley until it comes to the caves shown on the map. All these with the exception of Wazpretti Cave and Dry Valley Cave are probably more or less flooded during and after heavy rain.(omitted)
Emberson, R.,Cody, A.,Kermode, L. The Speleological Society 1998 Journal of the speleological society of korea Vol.8 No.2
The Bullock Creek Caves are located adjacent to the usually dry river bed of Bullock Creek, which reaches the sea about a kilometer north of Punakaiki. The caves have been comprehensively written up by Rodgers(972). Under conditions of normal water flow Bullock Creek submerges where the stream meets limestone on the west side of their Punakaiki syncline. In flood conditions it overflows the first submergence and progressively floods a series of smaller submergences down valley until it comes to the caves shown on the map. All these with the exception of Wazpretti Cave and Dry Valley Cave are probably more or less flooded during and after heavy rain.(omitted)
Cohort Profile: The Korean Cancer Prevention Study-II (KCPS-II) Biobank
Jee, Yon Ho,Emberson, Jonathan,Jung, Keum Ji,Lee, Sun Ju,Lee, Sunmi,Back, Joung Hwan,Hong, Seri,Kimm, Heejin,Sherliker, Paul,Jee, Sun Ha,Lewington, Sarah Oxford University Press 2018 International journal of epidemiology Vol.47 No.2