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Decade Resources Ltd V.DEC

Alternate Symbol(s):  DECXF

Decade Resources Ltd. is a Canadian based mineral exploration company seeking opportunities in the resource sector. The Company holds numerous properties at various stages of development and exploration from basic grass roots to advanced ones. Its properties and projects are all located in the Golden Triangle area of northern British Columbia. Its projects include Grassy, Premier East, Red Cliff, Lord Nelson, Del Norte and Terrace. The Terrace project includes Terrace Gold, Kleanza, Dardanelle, Treasure Mountain and Nobody Knows. The Company owns 100% of Goat property. The Copper River Valley properties are comprised of three main claim blocks; Terrace Gold-Darranelle-Treasure Mountain group of claims located in northern British Columbia. The property consists of 52 contiguous mineral claims. The Grassy property contains approximately 830.20 hectares in two separate claims which are owned 100% by the Company. The Red Cliff project consists of approximately eight mineral claims.


TSXV:DEC - Post by User

Post by Wangotango67on Mar 25, 2021 9:53pm
172 Views
Post# 32883911

DEL NOTRE - i see something interesting

DEL NOTRE - i see something interesting I don't think the silt on Del Notre Mountain is - indigenous.
I think - it's glacial wash - from - elsewhere.
The silts that sugar coat Del...  don't match the color of the host rock.

Before you scream and yell....
Hang on.

Look at the base of the Del, see anything interesting ?
I do... i see something amazing.
I see welded conglomerates.
Round - yes, water washed - round boulders - rewelded into the base of Del Notre.

Now.. look at how high the conglomerate rocks are - yip.. that's pretty high up.
Which proves a glacial or... cough cough, watershed washed these rocks in, aside
of the Del Notre and with alkai salt waters and rhyolites, limes, gypsums = welded.


Let's now ( hypothetically ) power wash the Del.
Rid the Mountain of the sandy silts.
What would we see ?

Would the Del reveal the same hosr rock with a distinct volcanic dark grey that weaves about ?
My hunch says... yes.
All same host rock - cept - the intrusive dyke that runs up into the - LG VEIN

Next... focus solely on the darker sulphides that weave about.
DEC  - is locked on the central zone just east of the LG  zone.
Goos pot... thick dark grey rocks - highly prob containing target minerlas.

Now...follow this dark grey lense.
It runs to the left - westerly.
Coursestill it runsto the next peake - then, as iit cascades down stil lgoing left, hits the
next peake - extreme westerly.

It also looks like it forks out going to the left...
One branch going up the other down and create an oval and then, reattaches.
But.. my hunch says... wash the foreign silts form the Mountain.
Host rockwould most likely - show itself.

The far lone peake - off to the left - looks pretty sweet..
very similar sulphide greys - with, ample room for - drill pads.
I'm thinking - one big system.. but with a nintrusive - dyke - lg.

Not hard to imagine - ocean waters sweeping through these large caverns.
washing major silts and float rocks against and on these - ranges.
Add in snow and ice - preserves it.
As the ice melts.. it's like looking into the past.


https://teuton.com/wp-content/uploads/2019/03/Walus-Moorman-1024x692.jpg


Again, it's my own interpretation.
You can have yours and well, i'll keep working on mine.
Wink.


Cheers...






 
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