Here is the link to the Reed Lake map (it is on Wildcat's website):

http://wildcat.ca/openwindow.php?PAT...

This concludes my survey on WEL's Reed Lake property.

It is clear that there is significant mineralization on neighbouring properties to the south as well as to the west and north of the Wildcat property. That alone suggests that the same mineralization should exist on Wildcat's land as the rock is of the same type. As Wildcat continues doing exploration on it's own property, there is a high probablility that they will discover economically viable deposits that will then lead to a joint venture with a producer. The proximity of the smelter in Flin Flon also adds to the viability of future production.

NL

P.S. In case you were wondering what VMS stands for (as I was):

Volcanogenic massive sulfide ore deposits or VMS are a type of metal sulfide ore deposit, mainly Cu-Zn-Pb which are associated with and created by volcanic-associated hydrothermal events in submarine environments.

These deposits are also sometimes called volcanic-hosted massive sulfide (VHMS) deposits. They are predominantly stratiform accumulations of sulfide minerals that precipitate from hydrothermal fluids on or below the seafloor in a wide range of ancient and modern geological settings.