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In fact, BOW,s numbers are really based on .35 g/t, not 1 g/t. He uses the 1 g/t after he has scaled the anomaly by 66%.

To get .35 g/t over the whole 600m into the ovoid with one hole is really nothing, but, if that grade is consistant through the entire anomaly of 1800 x 1700 x 1300, you have a huge deposit. If that drill intercept comes back with 1 g/t over 600m, you will have 3 times as much as what BOW,s math says.

People fail to see the tests on the anomalous gold outside the veins, and understand its importance. The main country rock of the Tesoro is the diorite, this diorite has been tested in approx 5 different areas on the property. The tested areas were mostly exposed areas and had grades as high as 2.3 g/t or higher ,in the host rock itself over considerable widths. The diorite has not been tested in the 70% area of the property that is covered with overburden, or at least it has not been reported on yet. The diorite does give off a signature on the Titan, but without some sort of mineralization, we would not be getting the readings we are getting, which are multiples higher than just diorite/granodiorite readings. Its the sulphides that set off the chargeability like it does, and we have been told that by reputable sources.

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