The basal unit of the Whim Creek Greenstone Belt is the Whim Creek Group consisting of the Warambie Basalt, rhyolite and volcaniclastic rocks of the Mons Cupri Volcanics overlain by conglomerate, sandstone, shale and felsic tuffs of the Bookingarra Group. The Bookingarra Group consists of the Cistern Formation, (conglomerate, tuffaceous sandstone and siltstone) overlain by the Rushall Shale and mafic rocks of the Louden and Mt Negri Volcanics (Huston 2006).
http://www.venturexresources.com/index.php/whim-creek-project/
Look at where they know the conglomerate layer is. Remember that up till recently no one knew to look at the conglomerate.
Remember at Whitswaterand they it is economical to mine 4000m deep.
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