No doubt you are aware that, for suitably homogenous and well-calibrated sources, photomicrographic measurement of the depth of hydration (patination) has proved to be a fair first-order aging technique for flaked obsidian. However, since hydration rate is strongly affected by the surounding soil (pH, etc.) conditions, I have never relied on it.
But this specimen is supposedly andesite, which is so heterogenous that all patination 'bets are off'...
Thanks again!
I've seen this technique used before and the patination was called 'desert varnish.'
You don't have to rely on it for aging, but it's a good indicator that something isn't a newly manufactured hoax.