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To: peter snowdon who wrote (20382)9/14/2003 11:11:13 AM
From: jpthoma1  Respond to of 39344
 
I was a shareholder of Loki Resources, the company that is 4 reversed split old mother company of Mill City.

If the Browns brothers are still involved in that company, I would not touch it with a thousand miles long stick!!!!!

Yes I still own 100 shares (originally, I had 50,000 shares of Loki)

LOLOL

JP



To: peter snowdon who wrote (20382)9/15/2003 3:13:00 AM
From: VAUGHN  Respond to of 39344
 
Hello Peter

I don't know how you found out so much, but good on you mate!

I appreciate all you did.

I'll have to watch and see whether Carl keeps accumulating...

Thanks again.

Vaughn



To: peter snowdon who wrote (20382)9/17/2003 3:46:45 PM
From: VAUGHN  Respond to of 39344
 
Hello Peter

Some news regarding our discussion on Mill City (MC.V):

Mill City's Nevada Holdings Increase to 692 Claims

CALGARY, Sept. 17 /CNW/ - MILL CITY INTERNATIONAL CORPORATION ("MILL
CITY") (TSX.VEN-MC) is pleased to announce the acquisition of a 100% interest
in the Elliott Dome property in north central Nevada. The property is
comprised of 95 claims (795 hectares) and adjoins the Company's previously
acquired Pony Creek property. This latest acquisition brings the Company's
holdings in Nevada to 692 claims (5790 hectares).
Consideration for the acquisition includes the payment of US$30,000, the
issuance of 100,000 common shares of the Company and escalating yearly
property payments to the vendor. A Net Smelter Return Royalty ("NSR") of 4% is
payable to the vendor and Mill City retains the right to purchase 1% of the 4%
NSR on the property for US$1,000,000.
Located in southwestern Elko County about 20 miles south of the town of
Carlin and along the crest of the Pinon Range, the property is within the
southern Carlin Trend 12 to 15 miles south of the Rain and Emigrant Springs
deposits. It is comprised of 95 mineral claims (795 hectares) which extend for
a strike length of three miles from the Company's Pony Creek property on the
south to the Trout Creek property (held by Royal Standard Minerals) on the
north.
Elliott Dome is within the Pinon graben, a regionally extensive
structural feature which trends north/south for at least 20 miles and hosts
deposits and mineral occurrences containing more than 5 million ounces of
gold. A well developed anticline, which occupies the central part of the
graben, has been segmented by west-northwest trending faults into several
south plunging antiforms or domes. One of the south plunging antiforms hosts
the Trout Creek deposit (520,000 ounces of gold) on the north border of the
property. Another antiform within the graben hosts the large mineral system at
Mill City's Pony Creek property south of Elliott Dome. The antiform at Elliott
Dome is well defined in the altered exposures of Mississippian sandstone and
conglomerate, and has been intruded by a recently recognized intrusive about
2,000 feet in diameter. This intrusive is identical to those hosting the
mineral system at Pony Creek a mile to the south.
Alteration and mineralization are extensive within the Mississippian
clastic sediments and the intrusives especially along structures.
Silicification is widespread along with iron oxides (after pyrite) and barite
breccias.
The structural setting, the stratigraphy, and the alteration at Elliott
Dome are the same as seen above and peripheral to the deposits at Rain. The
Mississippian/Devonian contact which is host to the Rain deposit (15.5 million
tons at 0.066 opt Au) and the Saddle deposit (3.99 million tons at 0.37 opt
Au) has not been tested on this property. The nearest exposure of this contact
is at Trout Creek (about one mile north of the property) where a shallow
resource of 520,000 ounces has been outlined.
Excellent potential exists to discover structurally controlled high grade
at the Mississippian/Devonian contact within the Elliott Dome property.
Completion of the property acquisition described above is subject to
regulatory approval.


Seems to be some real potential being pursued by the new management group. I guess that explains why (Carl) somebody has been accummulting it.

Regards

Vaughn