As I have said previously...
In the wash-up, I believe people will refer to this as a "golden Eagle type field".
I think it is already unique...especially the salt "slide" (my terms), which appears to have run down the Salt Valey Anticline, over the top of the Northern fault and effectively encapsulated everything fromn the Pinkerton Trail formation down.
I reckon Alkali Gulch will eventually prove to be significantly bigger than most expect, for the Pinkerton Train to be equally large and an eventual zone somewhere in the Mississippian or Cambrian formations...be they Leadville, McCracken, Lynch or any one of the several other secondary targets!
Cheers!
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