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Message: Hog,s post of yesterday

I would like to post a link to Hog,s post of Dynacors Acari Property. There is in that post important information that may be linked to the Tesoro property and what Greaser was trying to tell us awhile back. If these 800m HIGH veins that contain a grade of 16g/t gold lead up the canyon walls on the south side, guess where they lead to. I didn,t see or know this before, I was under the impression that Dynacors gold bearing veins ran from their surface to 800m below, NOT ABOVE!

http://agoracom.com/ir/steliasmines/forums/discussion/topics/475386-interesting-info-from-our-neighbor-dyn-further-to-bow-s-post/messages/1532902#message

Dynacor is sitting at 500m above sea level in the canyon, we are at roughly 2300m above sea level. The high hill in the link below at 2500m is what I beleive to be the ancient volcano and the C-1 workings is on the flat, hence the 2300m level.

http://www.steliasmines.com/properties/PeruFig5.pdf

If Dynacor has traced those veins UP 800m, that puts them at least at the 1500 meter level below the A-4 workings. Look at Primeds picture with the depth of the ovoid and look where it is still open at the 1500m level. Keep also in mind that the strong signature from the responses from the Titan above THE 1000M LEVEL may have blocked out whats below, hence the narrowing of the anomaly at depth.

http://agoracom.com/ir/steliasmines/forums/discussion/topics/471157-this-one-is-worth-2000-words/messages/1521004#message

Now, imagine if you will, a volcano, with the heart being the giant anomaly and the Dynacor veins I speak of, being part of the lava flow after an eruption. The lava would contain lower mineralization the further you got away from the source and higher mineralization down inside of it where the eruption originated from. This may be a bad example I am using (the volcano event) to try to explain what I am saying, but I hope most of you get it. So, we got Dynacor veins on the outreaches of the lava flow grading 16 g/t and we have near the mouth of the volcano, the A-4 vein grading average 24 g/t, it should be reasonable to expect higher grades yet in the heart of the volcano.

It has been suggested several times by management,that the Acari veins are part of the same system that formed the Tesoro. It is in my opinion that they are connected, because of probably a couple km,s away and their strike that points right to the Tesoro. The major structure responsible for the area deposition IS the main corridor, a rip in the Earth that extends NW AND SW, IMO. There is conclusive evidence of this in the fact we have andesite dykes and pegmatic material present directly above this fault. IMO.

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