THOUGHTS How i envision Northern Colombia.
Long ago flat region.
Hard rock, sediment ocean floor.
Some under water, some above.
Coal bed region, was the center isle.
Aclower region from east snd west.
Historical records show, coal beds seen a burn off.
( colombia geological records )
Seismic activity began to raise portions of eastern
developing small knolls.
Hardrocks parts that remained underwater ( eastern )
dev coral reefs.
Orgsnisms were attracted to the minerals in hardrock
which remained under shallow water - digesting several
minerals, especially, copper + carbon from the carbonic acid
waters created from coal beds + ocean water.
Overtime, the hardrock copper transitioned to carbonate
copper ( malachite )
More siesmic activity raised the northern ranges
Massive carbonate copper reefs raised with ranges
Overtime, reefs became diseminated, creating patchy
high grade malachite zones, while other areas as shown,
remained intact.
If copper converted to carbonate = reefs
If copper converted to oxide = this hardrock never saw
submersion in ocean.
Max performed, mag surveys + charge surveys.
Mag survey would detect the iron copper far better
iron and copper are oxide.
While the charge survey would pick up on the
carbonate iton and copper conversion.
In my best estimation,
carbonate copper is the high grade due to reef
organims creating a concentrate upon the reef,
versus, hardrock is moreso, original grades from
sediment ocean floors.
Spotting the vegatation coloration indufferences, looking
for the vegatation, that absorbed the aqua malachite,
might ( prove ) more positive than, any survey.
Question -
Since the Endeavor deal happened ( prior ) to URU
would this mean URU has Endeavor percentage interest ?
Cheers.
p.s.
has Max checked the area i pointed out ?
I'd say, that's a significant former reef body.
Iif malachite green - high odds of, high grade copper.
Thick reef, that did not seen siesmic upheaval.
Remained intact.
Moreso a deposit, versus - chasing patchwork.