Reading your description of Langmuir property

The drilling consistently encountered 3 distinct zones of high-grade nickel mineralization surrounded by lower-grade haloes. The low-grade mineralization haloes have an averaged true width of 22m to 44m. The zone widens at depth (approx. 100m to 125m below the surface) to 75m to 117 m true widths. The overall strike length of the North Zone is approximately 350m. The low-grade mineralized haloes range up to 0.769% nickel while narrow high-grade mineralization sections from 1m up to 10.5m true widths typically assaying between 1% and 4% nickel.

Are you saying there are 3 high grade pods each 75m to 117m wide?

How did your nickel form.? Where is your iron ore source and where is the nearby sulphur source for the magma flow? Is this part of an intrusion?

The diamond drilling at the Langmuir No 2 mine - North Zone has indicated a long and broad nickel bearing mineralization zone containing 3 possible distinct komatiitic extrusive flows in a paleotographic depression ...

You certainly are talking about alot of magma flow. Hopefully your komatiitic flow yields the results your flyers describe. What is the dimensions of this broad nickel bearing mineralization that you see as being open pittable. What is contained in the overburden and how much overburden is going to have to be cleared to the resource. At what point do you see putting a ramp to - to getting the higher grade mineralization? How is the existing structure going to be utilized. What caused the collapse of some of the underground structures?