SPAR LAKE - STUDY - north of Scad - sweet spot SPAR LAKE - sweet spot -
where ( ithink ) i saw lots of white rocks or outcrops on google .
Keep in mind the pdf report belwo speaks of, testing away from outcrops..
Now.. if the outcrops that were avoided - were carbonates - they should have been first focus.
Not lolly doggin it elsewhere.. .wink ( enjoying Spar Lake - tease )
https://www.google.com/maps/place/Spar+Lake/@46.6687106,-80.6587861,14z/data=!4m5!3m4!1s0x4d2f116693cd993b:0x2ffe65bc6c3a41e2!8m2!3d46.6691183!4d-80.6408158
MAIN PREMISE OF THE MAPPING PROGRAM
The main thrust of the mapping programme was to locate additional chlorite breccia zones similar to those of the known ore zones.
The pdf reports the intrusion of, Espanola ( serpentine ) carbonates.
( Carbonates and Chlorites )
What's serpentine rock ?
Carbonate minerals = limes + Chlorites
Serpentine = green - named after coloration of snakes.
A heinz 57 assemblage of any sort of rocks, with carbonate that lend a green hue.
Limes act as the glue - limes = cement.
Where is the gold ususally found in this Scadding area ?
In the carbonate serpentines ( chlorites )
Did they chck in the right area of Sapr Lake...
In my opinion yes.
They ( got it right ) checking for the dips AWAY from oiutcrops...
Why ids this better ?
Because the serpentine carbonate intrusion would fill the dips and valleys.
Thus at a later date solidify into carbonate rock - which even may appear to
fool a miner and look like a dyke.. .wink.
Where they got it wrong ?
Only kept to surfical testing - humus and plants.
The carbonate connection to gold = 51 feet down.
Where could the Serpentine intrusion eminate form - oither than Espanoloa ?
Georgian bay... in mining distances - spit throw away for a large intrusion.
Even factoring the Grenville fault - could have been a causway fault aiding the intrusion into,
Scadding area... even as much as, Geargian bay was once connected to - Wanapitei Lake.
CARBONATES CHLORITES = ALKAI
Alkai gold depsoit - not - sulphide.
What, was the 1981 report focusing on ?
( checking humus and plants for the identificant of, gold )
Weeee little bit of a problem - in my opinion.
The carbonate intrusion now has ( several year classes of overburden )
Checking humus and plants for gold - would do di-ck...the plant root systems
don't run 51 feet down.
Why 51 ft or 15.5 m is the sweert spot ?
The johnston occurence reported gold ( rich grade gold ) was found at 51 ft down.
What sort of rock was it found in ?
Nonother than - carbonate breccia - angular.
WHAT'S UP WITH THE ANGULAR ?
My hunch says... the carbonate limes ( CRUSTED ) in a baked heat sun.
Or, cracked with overburden atop it.
Result = fractured carbonates = angular / jagged / shattered / hardened carbonates.
.
Where do serpentine rocks originate - know to be elesewhere ?
Bottom of ocean floor... salt carbonates.
Known to crust and form a sedimnetry floor.
Carbonates are also clay based... fine platletes of, SILICA.
Superb for keeping water from penetrating- near impermiable.
BIGGEST QUESTION OF ALL ?
How can an alkai intrusion of carbonates deposit gold ?
Perhaps quite easily.
Gold can dissolve in alkai solutions. ( chloride )
If carried in by way of, ocean water in high concentrations of, carbonates
then... is could be rewritten how the gold deposited in this region with in a blanketed
carbonate bed - solidifying appearing as dykes, but rather, channel pocket lows
where the caerbonates eventually solidified trapping the gold.
NANO CARBONATE DISSOLVED GOLD = DOESN'T PRODUCE CHUNKY GOLD
NOT TH AT MOST OULD THINK....
ONE must keep in mind - minerals are constantly evoloving and metaphoring.
NO ROCK stays the same - decay overrides and soon basdown onlly to reassemble.
HOW COULD NANO GOLD REASEMBLE ?
In a carbonate alkai solution it only needs to solidify, and as most know,
minerals do attract to eachothjer.. .or repel.
Nano gold perhaps attracterd to othr nanao god and reassebld - even grown in crystal form.
MOST MINERS STUDY SULPHIDE GOLD
Which is a breakdown of ores in suphur.
While it is my beleif.... minerals in Alkais form and crystalize.
HOW COULD THEY FORM AND RECONSOLODATE ?
Salts - hold electrical ions - electreical charge.
It might be as simple as - an area which holds a good earth electrical charge -
Or, carbonates in an area of heightened electrical charge - might assist the fusion of
gold nano particles to reaassemble threough - electrolysis. ( wink )
AND...THERE MIGHT BE ANOTHER WAY
Not going ot hear this in mainstream - minerology classes ... wink.
There was a vidoe i came across few years back - i can'y find it on youtube...
They must have taken it down.. the documentry was coverign the topic of
gold - growing - on rocks - either Scotland or Ireland - gold actually growing in a crystal form.
Researches barracaded the rocks location to perform more studies...
Now.. if i recall.. . the large rock was near the ocean.
What's in the ocean ?
That's right... salt caegonates...salts charged with electrical ions..
Most likley .,... performing a low grade electrolysis on hte nanao gold with in the salt water
splashing up on the rocks....
SPAR LAKE - PDF REPORT - 1981
https://www.google.com/url?sa=t&rct=j&q=&esrc=s&source=web&cd=&cad=rja&uact=8&ved=2ahUKEwj21caMiKDvAhUTQ80KHX2PDZEQFjAAegQIARAD&url=http%3A%2F%2Fwww.geologyontario.mndm.gov.on.ca%2Fmndmfiles%2Fafri%2Fdata%2Fimaging%2F41I10NE0188%2F41I10NE0188.pdf&usg=AOvVaw0OxtxZnxIsULEBTAX4qPs4
Lastly...
When i opened google maps and scannedthe areas of Spar Lake the other eve,
It appeared to look like numerous white ourtcrops or rocks... scattered atop the syrface.
All around the south east bay and Spar Lake... in the V section between Johnston road and Kukugami.... Was it rocks or was it snow...?
The map i opened appeared to be a summer arial view - and as most know - sometimes google will patch a snaow zone with summer... thuis map appeared to be all summer...
Which points to... rocks could verywel lbe scattered thorughout this forested area.
Keep in mind - the pdf report - chose to trst areas around Spar lake - away for moutcrops.
They should have checked ot see if thr outcrops werre of, carebonate nature and really
studied - especially if thery know the gold is found in - serpentine carbonates.
Check those dips and valleys all arounf hte iron formations.
0m to 100m.
Let the iron formations on the surveys - red resistivity zones -
be the guide inwhich points to - the outside areas as alkai lows loands now filled in.
Filled in with... serpentine carbonates... crusted and jagged angulars just like
jonhston occurence - 52 ft down.
Cheers....