Thanks mac. Not tempered one bit, since my expectations are in alignment with what the outcomes are likely to be.
The aquifer can be pressure tested and the costs involved (where hard rock can not be compared) are relatively minor, additionally the resource estimate require less time to determine.
What we may have here in the red valley is a large aquifer which is fed into it by smaller ones created by the faults systems.
I do not exclude a "Clayton valley" look a like. The prehistoric paradox basin is a very enormous. We are sitting on the edge of it.
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