VANCOUVER, BC, April 11,
2023 /CNW/ - Silver Valley Metals Corp. (TSXV:
SILV) (OTCQB: SVMFF) ("Silver Valley" or the "Company"), a
brownfield exploration Company with two potential high impact
projects that comprise silver-zinc-lead located in north
Idaho, USA and lithium - potassium
(sulphate of potash) located in Zacatecas and San
Luis Potosi, Mexico respectively, is pleased to provide
strong exploration results from the Ranger-Wyoming target, related to an
under-developed complex of historical mine workings, at the
Ranger-Page Project, Silver
Valley, Idaho.
To view the Ranger-Wyoming Target in a 3-D
multi-media audio-video click: https://tinyurl.com/yc7327fs
Highlights:
- Largest anomalous target area defined at the project.
- Significant coincident induced polarization and resistivity
geophysical anomalies measuring approximately 1,200 metres
in strike length and up to 600 metres depth along the
prominent 96 Fault structure that projects into the Bunker
Hill mine hosting significant high-grade mineralization adjacent to
the project area.
- High values of silver, zinc, lead, and copper in soil and
located coincident with the geophysics anomalies and on top of the
96 Fault with silver values as high as 21.9 g/t, lead values
up to 7,640 ppm, copper values up to 339 ppm and zinc
values up to 274 ppm. Cadmium, arsenic, and antimony are
also elevated which are strong indicators of silver and lead
mineralization found in the District.
- Related to the Ranger-Wyoming
complex historical mine workings.
- The Ranger-Wyoming target is
situated parallel approximately 200 metres south of the East Curlew
and Blackhawk targets.
- First assessment of the Ranger-Wyoming target and '96 Fault' with modern
exploration technologies.
Dale Moore, Exploration
Director for Silver Valley Metals, comments," We are excited
about the target rich environment we have developed at the
Ranger-Page project over the past year. This latest target at the
Ranger-Wyoming complex is located
along the 96 Fault, an important fault on our project, and at
the Bunker Hill Mine located next door. The Ranger-Wyoming complex of underground workings mined
mineralization related to the 96 fault and now, nearly 100 years
later, we think we've located its extension. "
To view exploration results in Presentation
format, click: https://tinyurl.com/2duxbskr
Brandon Rook, CEO,
stated, "Our exploration efforts at Ranger-Page Project have
paid off nicely with the addition of the Ranger-Wyoming target added to the list of high
priority drill-ready targets. The potential extension of
mineralization to surface, and along strike is very exciting for
the Company, and we look forward to getting the drills turning in
this area in 2023. We are using modern exploration techniques
for the first time in the project's history, and it is allowing us
to gain a stronger understanding for the potential of these
zones."
Silver Valley Metals' Ranger – Wyoming target is closely related to the
Ranger-Wyoming complex of mine
workings, which extracted near surface high-grade silver, zinc, and
lead ores. The Ranger and Wyoming
deposits are associated with the 96 Fault which is a
significant project scale structure traced across much of the
Company's property. The 96 Fault merges with the Buckeye
Fault (also a prominent fault) on the eastern edge of the property
boundary, immediately east of the target area, where it projects
into the Bunker Hill mine. This fault structure has been
identified as a strong contributor to silver, zinc, and lead
mineralization that has been mined on Bunker Hill's project.
To view an enhanced version of the
Ranger-Wyoming Target Area, please click:
https://tinyurl.com/33etaw5d
The exploration team identified a potential extension of the
Ranger-Wyoming complex
mineralization along strike, and up-plunge of the historic mine
workings. Coincident ground induced polarization geophysics and
soil geochemical results have constrained a target area with
approximate dimensions of 1,200 metres of strike length and 600
metres of dip length. The anomaly is situated in the hanging wall
of the 96 Fault representing a significant expansion beyond the
known mineralization extent.
The ground induced polarization geophysics results are more than
twice the observed background of the host rock and the high values
of the resistivity ground geophysics also indicate the possible
presence of silicic alteration, which is a strong indicator of
mineralization in the Coeur d'Alene mining district.
To view an enhanced version of the
Ranger-Wyoming target figure -
Geophysics: Induced Polarization Anomaly, please
click: https://tinyurl.com/5ysky2yu
To view an enhanced version of the
Ranger-Wyoming target figure –
Geophysics: Resistivity Anomaly, please click:
https://tinyurl.com/bdfubnu7
A comprehensive surface geochemical program was
undertaken and was positioned along and on top of the 96 Fault and
on and near the geophysics anomalies. Results were
significant with silver values as high as 21.9 g/t, lead
values up to 7,640 ppm and copper values as much as 339
ppm, and zinc values up to 274 ppm.
Cadmium, arsenic, and antimony are also elevated, which are
strong indicators of lead and silver mineralization found in the
Coeur d'Alene mining district.
Lastly, the historic Ranger-Wyoming complex; positioned closely to the
former producing Blackhawk and Crown Point mines,
200 metres north and 500 metres north respectively - were
only partially developed, to less than 70
metres in depth. The Ranger-Wyoming target shows great
potential for further expansion,
laterally and vertically, and the fact that many of the
region's current and historic mines are developed to 1200 metres,
2,500 metres and beyond, the Ranger-Wyoming target is a top priority for
the Company's upcoming drilling program in 2023.
Geophysics: Induced
Polarization
Background induced polarization observed in the host rock at the
Ranger-Wyoming complex and
surrounding area in the western end of the Silver Valley is typically between 0 and 4
msec, as compared to the +20 msec background observed in the
Prichard formation to the north of
the Osburn Fault. The Ranger-Wyoming induced polarization anomaly are
locally as high as 10msec, more than twice the observed background
polarization of the host rock. The strike length of this
anomaly is approximately 1200 metres. The depth is approximately
600 meters. High overlapping resistivity data at the
Ranger-Wyoming target is
interpreted to be silicic alteration associated with a potential
mineralized system. This is a strong indicator of
mineralization in the Coeur d'Alene mining district and complements
both the induced polarization response in addition to anomalous
geochemistry on surface.
Geochemical Program:
A follow up geochemical program was implemented to further
validate the target, and results show the presence of anomalous
silver, lead, and copper along the trace of the '96 Fault' in the
target area. Soil geochemistry sampling over the induced
polarization anomaly shows silver values up to 21.9 g/t
compared to a background of <0.1. Lead, and Copper anomalies are
as high as 7,640 ppm and 339 ppm respectively. Background
levels of lead, copper and zinc in the project area are
typically 10 ppm, 6 ppm and 40 ppm
respectively based on all 2022 Silver Valley Metals
geochemical data. Trace element vector analysis is ongoing, and we
expect that will further validate the Ranger-Wyoming target.
Field Program
description:
A north-south soil grid oriented over the Induced
Polarization anomaly was used to guide sample locations. Samples of
the B and C soil horizons were collected on a 30-metre spacing. At
each location, a pit was dug until refusal (could not dig
deeper). The C and B soil horizons were sampled separately,
described, photographed, staked and location data collected via
GPS. Results were loaded into Leapfrog Geo and displayed via a
proportional grade plot to highlight high values.
B-Horizon Geochemical Sample
data:
LDL
|
<5 ppm
|
<1 ppm
|
<2 ppm
|
<5 ppm
|
<5 ppm
|
<2 ppm
|
<3.4 ppm
|
Sample ID
|
Easting
|
Northing
|
Elevation
(m)
|
As (ppm)
|
Cd (ppm)
|
Cu (ppm)
|
Pb (ppm)
|
Sb (ppm)
|
Zn (ppm)
|
Ag (g/t)
|
GCE-2-2B
|
561287
|
5263834
|
889
|
Trace
|
2.2
|
10.8
|
24.6
|
19.5
|
144.0
|
Trace
|
GCE-2-3B
|
561313
|
5263863
|
890
|
6.8
|
2.4
|
16.1
|
219.0
|
19.8
|
169.0
|
Trace
|
GCE-2-4B
|
561336
|
5263895
|
888
|
Trace
|
1.2
|
11.8
|
27.2
|
17.1
|
100.0
|
Trace
|
GCE-2-5B
|
561366
|
5263928
|
887
|
Trace
|
2.8
|
15.8
|
24.1
|
14.4
|
274.0
|
Trace
|
GCE-2-6B
|
561387
|
5263942
|
885
|
Trace
|
1.1
|
13.2
|
232.0
|
21.0
|
106.0
|
Trace
|
GCE-2-7B
|
561412
|
5263970
|
883
|
7.4
|
2.4
|
17.2
|
24.0
|
16.3
|
144.0
|
Trace
|
GCE-2-8B
|
561424
|
5263998
|
884
|
19.4
|
1.5
|
19.0
|
33.2
|
23.0
|
86.6
|
Trace
|
GCE-2-9B
|
561444
|
5264023
|
883
|
6.2
|
Trace
|
9.2
|
140.0
|
16.0
|
74.6
|
Trace
|
GCE-3-4B
|
561518
|
5264043
|
917
|
23.9
|
Trace
|
17.1
|
145.0
|
26.4
|
65.2
|
Trace
|
GCE-3-10B
|
561506
|
5264017
|
894
|
28.6
|
Trace
|
28.5
|
57.5
|
21.4
|
54.1
|
Trace
|
GCE-3-11B
|
561490
|
5263985
|
909
|
29.3
|
Trace
|
16.7
|
Trace
|
16.0
|
62.7
|
Trace
|
GCE-3-12B
|
561470
|
5263961
|
912
|
43.5
|
Trace
|
17.4
|
7.2
|
17.3
|
41.8
|
Trace
|
GCE-3-13B
|
561453
|
5263938
|
916
|
12.8
|
Trace
|
21.1
|
15.9
|
19.6
|
53.4
|
Trace
|
GCE-3-14B
|
561431
|
5263915
|
915
|
10.6
|
Trace
|
21.5
|
Trace
|
21.6
|
41.0
|
Trace
|
GCE-3-15B
|
561405
|
5263892
|
919
|
Trace
|
Trace
|
4.4
|
Trace
|
17.7
|
45.0
|
Trace
|
GCE-3-16B
|
561382
|
5263869
|
918
|
Trace
|
Trace
|
5.7
|
15.3
|
20.1
|
64.3
|
Trace
|
GCW-1-7B
|
561251
|
5264028
|
895
|
Trace
|
Trace
|
6.7
|
31.1
|
18.8
|
87.8
|
Trace
|
GCW-1-8B
|
561242
|
5263997
|
893
|
6.1
|
1.4
|
15.6
|
72.8
|
17.7
|
114.0
|
Trace
|
GCW-1-9B
|
561236
|
5263965
|
894
|
Trace
|
Trace
|
11.4
|
107.0
|
16.8
|
33.8
|
Trace
|
GCW-1-10B
|
561228
|
5263934
|
896
|
Trace
|
1.9
|
16.7
|
231.0
|
18.7
|
127.0
|
Trace
|
GCW-1-11B
|
561213
|
5263903
|
897
|
Trace
|
Trace
|
12.3
|
125.0
|
19.9
|
59.9
|
9.5
|
GCW-2-1B
|
561169
|
5263934
|
938
|
Trace
|
1.6
|
16.6
|
177.0
|
19.2
|
114.0
|
9.3
|
GCW-2-2B
|
561177
|
5263972
|
941
|
Trace
|
Trace
|
9.0
|
23.5
|
17.5
|
71.2
|
Trace
|
GCW-2-3B
|
561189
|
5264008
|
946
|
Trace
|
Trace
|
10.7
|
110.0
|
17.6
|
69.9
|
Trace
|
GCW-2-4B
|
561199
|
5264045
|
950
|
Trace
|
Trace
|
12.2
|
97.0
|
18.0
|
79.8
|
Trace
|
GCW-2-5B
|
561210
|
5264086
|
950
|
7.0
|
Trace
|
17.2
|
140.0
|
17.7
|
96.5
|
Trace
|
GCW-3-5B
|
561162
|
5264100
|
979
|
10.1
|
Trace
|
14.4
|
205.0
|
15.4
|
38.9
|
Trace
|
GCW-3-6B
|
561153
|
5264072
|
977
|
8.1
|
Trace
|
11.8
|
84.4
|
18.8
|
63.4
|
Trace
|
GCW-3-7B
|
561144
|
5264034
|
972
|
Trace
|
Trace
|
8.6
|
42.0
|
17.1
|
56.2
|
Trace
|
GCW-3-8B
|
561132
|
5263996
|
976
|
Trace
|
Trace
|
11.4
|
28.2
|
18.6
|
90.4
|
Trace
|
GCW-3-9B
|
561117
|
5263962
|
974
|
Trace
|
Trace
|
11.8
|
127.0
|
18.1
|
55.4
|
Trace
|
GCW-3-10B
|
561105
|
5263936
|
970
|
Trace
|
Trace
|
5.5
|
31.8
|
24.1
|
45.1
|
Trace
|
GCW-4-2B
|
561061
|
5263953
|
1001
|
Trace
|
Trace
|
23.5
|
222.0
|
27.0
|
48.4
|
Trace
|
GCW-4-3B
|
561082
|
5263975
|
1004
|
11.6
|
Trace
|
25.4
|
269.0
|
31.6
|
71.1
|
Trace
|
GCW-4-4B
|
561091
|
5264005
|
1007
|
9.7
|
Trace
|
22.2
|
51.0
|
20.9
|
97.4
|
Trace
|
GCW-4-5B
|
561106
|
5264044
|
1008
|
Trace
|
Trace
|
27.9
|
472.0
|
19.1
|
68.2
|
Trace
|
GCW-4-6B
|
561117
|
5264076
|
1010
|
Trace
|
Trace
|
9.7
|
79.7
|
17.8
|
51.8
|
Trace
|
GCW-4-7B
|
561124
|
5264113
|
1010
|
Trace
|
Trace
|
9.6
|
110.0
|
19.0
|
58.2
|
Trace
|
GCW-4-8B
|
561122
|
5264145
|
1014
|
9.3
|
Trace
|
5.9
|
133.0
|
17.8
|
30.1
|
Trace
|
GCW-5-3B
|
561065
|
5264160
|
1049
|
Trace
|
Trace
|
8.1
|
12.5
|
15.5
|
94.9
|
Trace
|
GCW-5-4B
|
561059
|
5264133
|
1057
|
Trace
|
1.1
|
8.6
|
32.6
|
15.9
|
69.8
|
Trace
|
GCW-5-9B
|
561020
|
5263993
|
1053
|
6.7
|
Trace
|
24.4
|
192.0
|
19.1
|
95.2
|
Trace
|
GCW-6-1B
|
560978
|
5263988
|
1042
|
Trace
|
Trace
|
12.9
|
26.2
|
16.0
|
107.0
|
Trace
|
GCW-6-2B
|
560994
|
5264016
|
1039
|
31.0
|
1.2
|
52.3
|
1050.0
|
83.4
|
124.0
|
Trace
|
GCW-6-3B
|
561001
|
5264048
|
1036
|
6.6
|
Trace
|
17.7
|
31.4
|
16.3
|
87.5
|
Trace
|
GCW-6-6B
|
561015
|
5264141
|
1036
|
Trace
|
Trace
|
12.3
|
92.9
|
16.0
|
102.0
|
Trace
|
C-Horizon Geochemical Sample
data:
LDL
|
<5 ppm
|
<1 ppm
|
<2 ppm
|
<5 ppm
|
<5 ppm
|
<2 ppm
|
<3.4 ppm
|
Sample ID
|
Easting
|
Northing
|
Elevation
(m)
|
As
(ppm)
|
Cd
(ppm)
|
Cu
(ppm)
|
Pb
(ppm)
|
Sb
(ppm)
|
Zn
(ppm)
|
Ag (g/t)
|
GCE-2-2C
|
561287
|
5263834
|
889
|
Trace
|
4.6
|
5.0
|
12.6
|
16.8
|
116.0
|
Trace
|
GCE-2-3C
|
561313
|
5263863
|
890
|
Trace
|
Trace
|
4.8
|
7.5
|
17.8
|
51.0
|
Trace
|
GCE-2-4C
|
561336
|
5263895
|
888
|
Trace
|
1.2
|
10.6
|
17.7
|
19.5
|
105.0
|
Trace
|
GCE-2-5C
|
561366
|
5263928
|
887
|
Trace
|
Trace
|
7.0
|
8.7
|
15.9
|
33.3
|
Trace
|
GCE-2-6C
|
561387
|
5263942
|
885
|
Trace
|
Trace
|
5.7
|
11.9
|
16.5
|
36.3
|
Trace
|
GCE-2-7C
|
561412
|
5263970
|
883
|
7.7
|
Trace
|
24.4
|
21.1
|
16.0
|
115.0
|
Trace
|
GCE-2-8C
|
561424
|
5263998
|
884
|
25.9
|
Trace
|
18.5
|
9.7
|
20.5
|
32.0
|
Trace
|
GCE-2-9C
|
561444
|
5264023
|
883
|
22.6
|
Trace
|
13.2
|
33.4
|
15.7
|
33.8
|
Trace
|
GCE-3-4C
|
561518
|
5264043
|
917
|
31.4
|
Trace
|
14.8
|
75.8
|
29.1
|
25.9
|
Trace
|
GCE-3-10C
|
561506
|
5264017
|
894
|
24.8
|
Trace
|
10.8
|
6.3
|
23.5
|
56.7
|
Trace
|
GCE-3-11C
|
561490
|
5263985
|
909
|
19.6
|
Trace
|
9.2
|
Trace
|
20.9
|
30.6
|
Trace
|
GCE-3-12C
|
561470
|
5263961
|
912
|
11.2
|
Trace
|
4.5
|
Trace
|
16.5
|
27.3
|
Trace
|
GCE-3-13C
|
561453
|
5263938
|
916
|
20.2
|
Trace
|
34.5
|
13.9
|
22.6
|
47.8
|
Trace
|
GCE-3-14C
|
561431
|
5263915
|
915
|
7.8
|
Trace
|
9.9
|
Trace
|
19.9
|
26.8
|
Trace
|
GCE-3-15C
|
561405
|
5263892
|
919
|
Trace
|
Trace
|
12.5
|
Trace
|
25.2
|
33.4
|
Trace
|
GCE-3-16C
|
561382
|
5263869
|
918
|
Trace
|
Trace
|
Trace
|
7.6
|
18.9
|
25.8
|
Trace
|
GCE-4-8C
|
561567
|
5264048
|
937
|
26.7
|
Trace
|
7.8
|
5.3
|
18.4
|
44.4
|
Trace
|
GCE-4-9C
|
561549
|
5264028
|
938
|
17.3
|
Trace
|
4.4
|
19.2
|
17.2
|
28.4
|
Trace
|
GCE-4-10C
|
561533
|
5264002
|
940
|
20.4
|
Trace
|
15.8
|
Trace
|
14.5
|
14.2
|
Trace
|
GCE-4-11C
|
561513
|
5263975
|
944
|
54.8
|
Trace
|
10.6
|
Trace
|
15.0
|
21.5
|
Trace
|
GCE-4-12C
|
561494
|
5263953
|
942
|
20.2
|
Trace
|
8.3
|
Trace
|
12.4
|
39.6
|
Trace
|
GCE-4-13C
|
561481
|
5263933
|
941
|
14.3
|
Trace
|
104.0
|
26.0
|
39.2
|
49.3
|
Trace
|
GCE-4-14C
|
561462
|
5263901
|
944
|
Trace
|
Trace
|
2.9
|
Trace
|
13.1
|
20.5
|
Trace
|
GCE-4-15C
|
561442
|
5263886
|
940
|
Trace
|
Trace
|
5.0
|
7.8
|
17.3
|
70.6
|
Trace
|
GCE-5-2R
|
561493
|
5263918
|
951
|
Trace
|
Trace
|
Trace
|
Trace
|
16.9
|
22.3
|
Trace
|
GCE-5-3R
|
561514
|
5263929
|
959
|
19
|
Trace
|
6.7
|
6.6
|
12.4
|
20.0
|
Trace
|
GCE-5-4R
|
561524
|
5263944
|
960
|
Trace
|
Trace
|
3.0
|
6.0
|
14.0
|
18.3
|
Trace
|
GCE-5-5R
|
561535
|
5263957
|
946
|
8.1
|
Trace
|
2.5
|
Trace
|
14.4
|
20.5
|
Trace
|
GCE-5-6R
|
561531
|
5263964
|
948
|
13.0
|
Trace
|
2.5
|
Trace
|
9.4
|
11.8
|
Trace
|
GCE-5-7R
|
561548
|
5263990
|
958
|
53.2
|
Trace
|
19.6
|
Trace
|
19.3
|
22.6
|
Trace
|
GCE-5-8R
|
561567
|
5264018
|
950
|
31.5
|
Trace
|
4.8
|
Trace
|
16.7
|
25.5
|
Trace
|
GCW-1-7C
|
561251
|
5264028
|
895
|
Trace
|
Trace
|
Trace
|
Trace
|
16.0
|
51.3
|
Trace
|
GCW-1-8C
|
561242
|
5263997
|
893
|
Trace
|
Trace
|
8.9
|
Trace
|
13.9
|
80.2
|
Trace
|
GCW-1-9C
|
561236
|
5263965
|
894
|
Trace
|
Trace
|
8.5
|
122.0
|
15.2
|
27.6
|
Trace
|
GCW-1-10C
|
561228
|
5263934
|
896
|
8.68
|
Trace
|
12.3
|
57.4
|
23.4
|
41.7
|
Trace
|
GCW-1-11C
|
561213
|
5263903
|
897
|
Trace
|
Trace
|
8.3
|
17.3
|
11.0
|
34.0
|
Trace
|
GCW-2-1C
|
561169
|
5263934
|
938
|
21.0
|
Trace
|
13.1
|
13.2
|
17.6
|
51.6
|
Trace
|
GCW-2-2C
|
561177
|
5263972
|
941
|
6.2
|
Trace
|
8.5
|
35.2
|
14.6
|
30.6
|
Trace
|
GCW-2-3C
|
561189
|
5264008
|
946
|
Trace
|
Trace
|
7.2
|
Trace
|
14.1
|
38.9
|
Trace
|
GCW-2-4C
|
561199
|
5264045
|
950
|
Trace
|
Trace
|
5.0
|
23.1
|
16.5
|
33.7
|
Trace
|
GCW-2-5C
|
561210
|
5264086
|
950
|
Trace
|
Trace
|
6.6
|
11.0
|
37.2
|
72.9
|
Trace
|
GCW-3-5C
|
561162
|
5264100
|
979
|
8.68
|
Trace
|
16.8
|
303.0
|
12.0
|
25.2
|
4.1
|
GCW-3-6C
|
561153
|
5264072
|
977
|
7.4
|
Trace
|
5.5
|
9.1
|
18.4
|
40.2
|
Trace
|
GCW-3-7C
|
561144
|
5264034
|
972
|
8.0
|
Trace
|
14.3
|
24.5
|
17.4
|
50.8
|
Trace
|
GCW-3-8C
|
561132
|
5263996
|
976
|
6.7
|
Trace
|
7.5
|
5.1
|
18.8
|
60.8
|
Trace
|
GCW-3-9C
|
561117
|
5263962
|
974
|
Trace
|
Trace
|
3.2
|
6.7
|
36.5
|
100.0
|
Trace
|
GCW-3-10C
|
561105
|
5263936
|
970
|
Trace
|
Trace
|
6.9
|
83.1
|
33.1
|
62.9
|
Trace
|
GCW-4-2C
|
561061
|
5263953
|
1001
|
Trace
|
Trace
|
34.9
|
86.0
|
22.1
|
132.0
|
Trace
|
GCW-4-3C
|
561082
|
5263975
|
1004
|
13.0
|
Trace
|
23.1
|
69.2
|
16.7
|
45.6
|
Trace
|
GCW-4-4C
|
561091
|
5264005
|
1007
|
10.3
|
Trace
|
18.4
|
10.2
|
19.9
|
55.1
|
Trace
|
GCW-4-5C
|
561106
|
5264044
|
1008
|
Trace
|
Trace
|
8.5
|
40.4
|
16.8
|
39.8
|
Trace
|
GCW-4-6C
|
561117
|
5264076
|
1010
|
8.2
|
Trace
|
7.8
|
81.4
|
33.6
|
57.4
|
Trace
|
GCW-4-7C
|
561124
|
5264113
|
1010
|
Trace
|
Trace
|
11.6
|
74.7
|
30.1
|
61.0
|
Trace
|
GCW-4-8C
|
561122
|
5264145
|
1014
|
Trace
|
Trace
|
4.3
|
55.5
|
29.6
|
49.8
|
Trace
|
GCW-5-3C
|
561065
|
5264160
|
1049
|
Trace
|
Trace
|
2.9
|
12.5
|
40.3
|
86.9
|
Trace
|
GCW-5-4C
|
561059
|
5264133
|
1057
|
Trace
|
Trace
|
4.9
|
7.9
|
30.3
|
62.6
|
Trace
|
GCW-5-5R
|
561050
|
5264102
|
1058
|
35.0
|
Trace
|
339.0
|
7640.0
|
42.9
|
52.8
|
21.9
|
GCW-5-6R
|
561043
|
5264074
|
1055
|
27.2
|
1
|
113.0
|
4950.0
|
53.4
|
134.0
|
6.2
|
GCW-5-7R
|
561038
|
5264054
|
1059
|
8.8
|
Trace
|
102.0
|
27.9
|
37.2
|
115.0
|
Trace
|
GCW-5-8R
|
561031
|
5264024
|
1057
|
23.7
|
Trace
|
32.0
|
59.1
|
29.3
|
50.1
|
Trace
|
GCW-5-9C
|
561020
|
5263993
|
1053
|
Trace
|
Trace
|
7.9
|
9.1
|
30.4
|
53.9
|
Trace
|
GCW-6-1C
|
560978
|
5263988
|
1042
|
Trace
|
Trace
|
2.0
|
Trace
|
17.5
|
29.6
|
Trace
|
GCW-6-2C
|
560994
|
5264016
|
1039
|
5.2
|
Trace
|
17.9
|
69.3
|
30.7
|
38.2
|
Trace
|
GCW-6-3C
|
561001
|
5264048
|
1036
|
21.5
|
Trace
|
14.4
|
11.7
|
29.3
|
93.9
|
Trace
|
GCW-6-4R
|
561005
|
5264075
|
1035
|
Trace
|
Trace
|
18.9
|
41.5
|
32.6
|
155.0
|
Trace
|
GCW-6-5R
|
561004
|
5264110
|
1033
|
5.2
|
Trace
|
58.6
|
856.0
|
23.4
|
71.7
|
Trace
|
GCW-6-6C
|
561015
|
5264141
|
1036
|
13.2
|
Trace
|
20.1
|
11.4
|
28.5
|
59.8
|
Trace
|
Lab Analysis – QA-QC:
Atomic absorption analysis for Silver:
American Analytical Services, Inc ("AAS") is an ISO/IEC 17025
accredited laboratory, located in Osburn,
Idaho. All analysis includes quality control measures to
ensure an acceptance standard established within AAS methods. All
samples sent to AAS were checked for accuracy between the chain of
custody and the samples with the client present. Samples are dried
before starting the prep process. The prep process includes
crushing the sample in its entirety to 80% passing a 10 mesh, split
in a riffle box to make a 250g sub-sample and pulverized to 85%
passing a 140 mesh. Analysis for AA-Ag is done by 2 or 4 acid
digestion. Detection limit for AA-Ag is 0.100 Oz/ton - 15.0 Oz/ton.
Any results over the detection limit are sent to fire assay to do
Ag gravimetric finish.
ICP-OES analysis for 35 element analysis:
All samples are subjected to a 4-acid digestion. Digestion QC
consists of a reagent blank, control standard and for every 20
samples there is a duplicate of a sample pulp to check RPD. To
begin ICP-OES analysis, the instrument is standardized with the
five working standard solutions (multi-point linear fitting).
Samples are then measured with the reagent blank, control standard
and a CCV (continuous calibration verification). Once samples are
analyzed, all QC is checked, and results are sent to LIMS system to
be made into the client's report.
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Qualified person
Timothy Mosey, BSc, MSc, SME, is
the qualified person for the company and qualified person as
defined by National Instrument 43-101. Mr. Mosey supervised the
preparation of the technical information in this news release.
About: MexiCan lithium -
potassium (sulphate of potash) project:
Silver Valley Metals Corp. owns a 100% interest in a lithium and
potassium bearing salar complex comprising 4,056 hectares on three
mineral concessions (the "Mexican Projects") located on the Central
Mexican Plateau in the states of Zacatecas, and San
Luis Potosi, Mexico. The NI 43-101 inferred mineral resource
contains 12.3Mt of Sulfate of Potash (SOP) and 243,000 tonnes of
lithium carbonate equivalent (LCE) and remains open in all
directions for expansion.
About: Ranger-Page
project:
The Ranger-Page Project ("The Project") is in the Silver Valley, northern Idaho, USA, 60 kilometres east of Coeur
d'Alene and 1 kilometre from the I-90 freeway. In 2020 Idaho was
ranked the first in the world in policy perception and 9th best
mining jurisdiction (Fraser Institute Annual Mining Survey). The
Project borders the famous Bunker Hill Mine to the east and for the
first time consolidates the western extent of the prolific
Silver Valley mining
corridor by one operator in the past 100+ years.
The Project comprises 6 historical mines on patented claims,
without royalties. The largest of these, the Page Mine, was a top
ten producer in the Silver Valley
yielding over 1.1 billion pounds of zinc and lead and 14.6 million
ounces of silver. The Page Mine has high grade silver-zinc-lead
historic reserves and remains open at depth and along strike beyond
what has been identified to date.
Historical mining on the properties shared underground
infrastructure which connected the larger Page mine with five
shallow historic mines within the larger Project area. The Company
has underground mining data and surface geological data that
supports high grade silver-zinc-lead mineralization present within
the shallow, undeveloped mines. These mines remain open at depth,
and laterally along strike.
Exploration potential beyond the historic mines is considered
significant as modern systematic exploration is being applied to
the project for the first time.
About: Silver Valley
Metals:
Silver Valley Metals Corp. is a Canadian exploration company
comprised of a group of experienced exploration, mining, and
financing specialists focused on the pursuit of mineral discovery
and development. We are focused on the advancement of strategic and
precious mineral properties including Lithium-Potash in
Mexico and Silver-Zinc-Lead in
northern Idaho,
USA.
Link to
Website: http://www.silvervalleymetals.com
On behalf of the Board of Directors of Silver Valley Metals,
"Brandon Rook"
Brandon Rook, President &
CEO, Director
THE TSX VENTURE EXCHANGE HAS NOT REVIEWED AND DOES NOT ACCEPT
RESPONSIBILITY FOR THE ADEQUACY OR ACCURACY OF THIS RELEASE.
The information contained herein contains "forward-looking
statements" within the meaning of applicable securities
legislation. Forward-looking statements relate to information that
is based on assumptions of management, forecasts of future results,
and estimates of amounts not yet determinable. Any statements that
express predictions, expectations, beliefs, plans, projections,
objectives, assumptions or future events or performance are not
statements of historical fact and may be "forward-looking
statements." Forward-looking statements are subject to a variety of
risks and uncertainties which could cause actual events or results
to differ from those reflected in the forward-looking statements,
including, without limitation: risks related to failure to obtain
adequate financing on a timely basis and on acceptable terms; risks
related to the outcome of legal proceedings; political and
regulatory risks associated with mining and exploration; risks
related to the maintenance of stock exchange listings; risks
related to environmental regulation and liability; the potential
for delays in exploration or development activities or the
completion of feasibility studies; the uncertainty of
profitability; risks and uncertainties relating to the
interpretation of drill results, the geology, grade and continuity
of mineral deposits; risks related to the inherent uncertainty of
production and cost estimates and the potential for unexpected
costs and expenses; results of prefeasibility and feasibility
studies, and the possibility that future exploration, development
or mining results will not be consistent with the Company's
expectations; risks related to commodity price fluctuations; and
other risks and uncertainties related to the Company's prospects,
properties and business detailed elsewhere in the Company's
disclosure record. Should one or more of these risks and
uncertainties materialize, or should underlying assumptions prove
incorrect, actual results may vary materially from those described
in forward-looking statements. Investors are cautioned against
attributing undue certainty to forward-looking statements. These
forward-looking statements are made as of the date hereof and the
Company does not assume any obligation to update or revise them to
reflect new events or circumstances. Actual events or results could
differ materially from the Company's expectations or
projections.
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SOURCE Silver Valley Metals Corp.