Copper Lake Provides Update and Priorities FOR 2021 Exploration ON Its Marshall Lake Copper-Zinc-Silver Project
News Release No: 21-04
COPPER LAKE PROVIDES UPDATE AND PRIORITIES FOR
2021 EXPLORATION ON ITS MARSHALL LAKE
COPPER-ZINC-SILVER PROJECT
March 18, 2021, - Toronto, ON - Copper Lake Resources Ltd. (TSX -V: CPL, Frankfurt: WOI ,
OTC: WTCZF) (“Copper Lake” or the “Company”) is pleased to provide an update on its plans and
priorities for the 2021 exploration program on the Company’s Marshall Lake copper -zinc-silver
property (the “Property). A budget of $1,500,000 has been allocated to explore Marshall Lake in
2021. The Property is located approximately 252 km north-northeast of the City of Thunder Bay and
30 km west of the Town of Nakina, in the Thunder Bay Mines and Minerals Division, norther n
Ontario. Access to the Property is by all -weather gravel road leading from Highway 11 (Trans -
Canada Highway), providing excellent access year-round.
There are over 112 known occurrences of base -metal mineralization outcrop over an extensive area
across the Property. A systematic review and compilation of historical data at Marshall Lake which
is currently ongoing, identified high-priority targets characterized by high base -metal and precious-
metal grades that warrant immediate follow-up work.
Billiton Zone:
The Billiton Zone consists of 8 lenses of heavily disseminated to massive sulphide, traced by drilling
over a 500- metre strike length. The lenses dip to the north at 45 to 65 degrees and strike WSW to
ENE (064 degrees). Mineralization is hosted within sericite, silica and chlorite -altered laminated
volcaniclastic rocks (dacite) and a cherty tuffaceous unit (possibly exhalite). Mineralization consists
of pyrite, chalcopyrite, sphalerite, silver minerals, galena, pyrrhotite and magnetite. Sulphide lenses
range from 1 to 6 metres in true thickness.
The Billiton Zone has been the target of significant historical drilling, yielding numerous high-grade
intercepts in copper, zinc and silver as tabulated below:
Hole No.1
From (m) To (m) Length
(m)
Cu (%) Zn (%) Ag (g/t) CuEq
(%)2
Au
(g/t)3
GGM-78-230
Imperial Oil Ltd. 1978
50.85
Incl. 50.85
58.23
52.50
7.38
1.65
2.97
5.50
10.98
31.50
219.73
320.18
7.86
17.29
0.34
0.34
GGM-77-154
Imperial Oil Ltd. 1977
83.99
Incl. 83.99
90.09
85.52
6.10
1.53
1.89
1.67
4.03
10.30
145.69
311.26
4.16
7.03
0.34
0.34
NWT-81
NWT Copper Mines
1981
75.46
Incl. 75.46
79.57
77.74
4.11
2.28
1.49
2.24
4.70
7.50
250.93
423.02
4.73
7.58
n/a
n/a
NWT-68-83
NWT Copper Mines
1968
70.40
Incl. 72.56
75.91
75/91
5.51
3.35
2.28
2.45
9.79
13.64
124.44
158.72
6.13
7.70
n/a
n/a
NWT-68-84
NWT Copper Mines
1968
156.77
Incl.
156.77
159.76
158.02
2.99
1.25
2.56
3.44
10.26
18.65
181.34
313.66
6.96
12.62
n/a
n/a
ML-82-05
Falconbridge Copper
1982
295.85
Incl.
298.20
299.66
299.66
3.81
1.46
2.46
4.24
2.00
2.61
179.63
204.65
4.37
6.51
n/a
n/a
ML-82-07
Falconbridge Copper
1982
19.05
Incl. 21.98
22.65
22.65
3.60
0.67
1.81
5.45
9.35
22.26
164.20
436.04
5.82
15.31
n/a
n/a
Mar-18-07
Copper Lake Res. 2018
207.30
Incl.
209.30
212.35
210.30
5.05
1.00
0.68
3.20
2.14
8.35
78.51
367.00
1.89
8.39
1.63
8.01
1Historic information is sourced from drill logs; it predates 43-101 and has not been verified by a QP and should not be
relied upon.
2Copper equivalent is based on prices of $4.00/lb for copper, $1.20/lb for zinc and $20/oz. for silver 3Many analyses for
gold are not available, particularly in the older historic logs
Given the high-grade and polymetallic nature of the Billiton zone, this target is clearly the number
one priority. Notably, there has been a lack of deep historic drilling completed on the Billiton Zone,
with only 6 known drill holes testing the zone deeper than 150 metres bel ow surface, over its 500 -
metre strike length. ( See the Billiton Zone, Longitudinal Section on page 11 of the Corporate
Presentation at www.copperlakeresources.com)
Excellent potential exists for extending high -grade mineralization at Billiton to depths greater than
that completed by historical drilling. Large-loop ground electromagnetic surveys (TDEM) and bore-
hole electromagnetic surveys (BHEM,) prime exploration tools utilized in the search for deep massive
sulphide deposits, were not utilized in historical work completed at Billiton and are strongly
recommended for immediate, upcoming work. In addition, a deep Induced Polarization (IP)
orientation survey (400-metre depth capability) will be completed at Billiton to test the suitability of
this technique to help guide deeper drilling and to supplement the ground TDEM and BHEM surveys.
Shallow historical IP surveys (to 100 metres depth) completed at Billiton, reveale d discrete
chargeability and resistivity anomalies, closely associated with sulphide mineralization.
A contractor has been engaged to complete the deep geophysical surveys at Billiton; the surveys will
commence as soon as field conditions permit. Follow-up diamond drilling to extend the Billiton zone
to depth is anticipated for June or July of this year.
Gazooma North and RM Zones:
Collectively, the Gazooma North and RM Zones have been tested by diamond drilling over a
minimum 300-metre strike length and may comprise the same mineralized zone. Drilling has largely
been completed at shallow depths, almost all within 150 metres of surface; the deepest hole was
completed on the RM Zone to a depth of 460 metres (at a shallow dip of -45 degrees).
Mineralization o ccurs as stringers, heavy disseminations and narrow bands of semi -massive
chalcopyrite, hosted within a high-silica or silica-altered, dacitic volcaniclastic rock unit. Significant
copper drill intercepts from both zones are summarized below.
Hole No.
Zone From (m) To (m) Length
(m)
Cu (%) Ag (g/t) Au (g/t)
GAZN-08-06
East West
Gazooma
North
70.00
incl. 81.50
& incl.
85.00
94.00
83.50
90.00
24.00
2.00
5.00
1.74
3.67
3.36
8.90
18.10
17.10
0.32
0.61
0.68
GAZN-10-11
White Tiger
Gazooma
North
110.40
incl. 117.00
that incl.
120.00
143.00
122.00
121.00
32.60
5.00
1.00
1.04
3.53
9.32
5.10
18.20
49.80
0.15
0.52
1.20
GAZN-10-15
White Tiger
Gazooma
North
149.00
incl. 155.00
that incl.
157.00
172.00
160.00
159.00
23.00
5.00
2.00
1.34
4.08
7.25
6.70
20.60
35.9
0.29
1.17
2.03
RMZ-11-21
White Tiger
RM Zone 149.00
incl. 155.00
that incl.
158.00
182.00
160.00
160.00
33.00
5.00
2.00
1.53
3.73
6.25
6.80
16.40
28.60
0.13
0.31
0.54
RMZ-11-23 RM Zone 269.00 293.00 24.00 1.01 4.00 0.09
White Tiger incl. 278.00
that incl.
278.00
282.00
279.00
4.00
1.00
2.87
6.71
9.50
18.30
0.24
0.60
RMZ-11-28
White Tiger
RM Zone 28.00
incl. 28.00
& incl.
32.00
35.00
30.00
34.00
7.00
2.00
2.00
2.50
3.38
4.00
8.9
11.8
14.70
0.07
0.15
0.06
RMZ-13-40
White Tiger
RM Zone 144.00
incl. 144.00
that incl.
145.00
187.00
177.00
155.00
43.00
33.00
10.00
1.38
1.66
2.52
5.40
6.17
9.40
0.04
0.05
0.07
The style of copper mineralization and alteration at Gazooma and RM Zone is commonly described
as stringer or stock -work-type. Accordingly, potential exists for the discovery of massive sulphides
at this locale, associated with the stringer -type mineralization. Models for volcanic -hosted massive
sulphide deposits invoke an underlying or flanking zone of stringer, stock- work mineralization,
largely copper-rich, that feed or lead to overlying or adjacent Cu-Zn-Ag-Au bearing massive sulphide
lenses.
Shallow IP anomalies appear to correlate with the copper mineralization obtained in drilling, but only
yield data to a depth of approximately 100 metres below surface (very shallow). (See pages 13 and
14 of the Corporate P resentation for descriptions of the Mineralization and IP Anomalies at the
Gazooma and RM Zones). A large-loop TDEM survey is warranted at Gazooma North and RM Zone
to test for the presence of massive sulphides at depth and to expand on the limits of very significant
stringer-stock-work copper mineralization present at this locale. This survey will be undertaken
following the completion of the recommended deep EM and IP work, slated for the Billiton zone.
VTEM Anomalies:
A property-wide Versatile Time Domain Electromagnetic (VTEM) survey was flown at Marshall
Lake in 2007 to assist targeting in exploring for volcanic-hosted massive sulphide deposits. Modelling
completed by contractors delineated a total of 31 anomalies (conductors), a few of which have been
followed-up by diamond drilling.
Two strong untested conductors occur stratigraphically above the Billiton zone on the eastern portion
of the property on recently staked claims that are wholly-owned by the Company. These conductors
are underlain by vent-facies, volcanic auto-breccias, characterized by pervasive iron enrichment with
strong garnet -actinolite-magnetite-pyrrhotite alteration. These new target areas may represent a
repetition of the stratigraphy hosting the Billiton deposit through structural imbrication or
alternatively, may mark the location of an additional time horizon hosting base-metal mineralization.
Ground EM surveys will be completed on these targets to more accurately define the conductors,
prior to diamond drilling.
A re-assessment of the EM conductors yielded by the survey will be undertaken, supplemented by
additional output products from such data, to assist in the ongoing goal of generating additional high-
quality exploration targets on the Property.
Continuing Data Compilation:
The review and compilation of the current and historical data should continue with the integration
and interpretation of drilling, geological, geophysical and geochemical data sets. In particular, 3D
modelling of all mineralized zones should be completed and merged with the above data, to gain a
better understanding of controls on base and precious-metal mineralization and to generate additional
targets for continuing exploration.
Donald Hoy, M.Sc., P.Geo., is the Qualified Person under NI 43-101 and has read and approved
the technical content of this News Release.
About Copper Lake Resources
Copper Lake Resources Ltd. is a publicly traded Canadian company currently focused on advancing
its Marshall Lake and Norton Lake properties located in Ontario, Canada.
Marshall Lake Property
The Marshall Lake high -grade VMS copper, zinc, silver and gold property, compris es an area of
approximately 104 square km located 120 km north of Geraldton, Ontario and is accessible by all-
season road from the Trans-Canada Highway and just 22 km north of the main CNR rail line. Copper
Lake has an option to increase its interest to 87.5% from its current 75% interest. The property also
includes 148 claim cells staked in 2018 and 2020 that are 100% owned and not subject to any
royalties, which add approximately 30 square km to the property. The current consolidated land
position has an extensive exploration history including historical resource estimates as documented
and disclosed appropriately in the 43- 101Technical Report on the Marshall Lake Property dated
June 7, 2016 available at www.copperlakeresources.com.
In addition to the original Marshall Lake property above, Marshall Lake also includes the Sollas
Lake and Summit Lake properties, which are 100% ow ned by the Company and are not subject to
any royalties. The Sollas Lake property consists of 20 claim cells comprising an area of 4 square
km on the east side of the Marshall Lake property where historical EM airborne geophysical surveys
have outlined st rong conductors on the property hosted within the same favorable felsic volcanic
units. The Summit Lake property currently consists of 100 claim cells comprising an area of 20.5
square km, is accessible year round, and is located immediately west of the or iginal Marshall Lake
property.
Norton Lake Property
Copper Lake has a 71.41% interest in the Norton Lake nickel, copper, cobalt, and palladium PGM
property, located in the southern Ring of Fire area, is approximately 100 km north of the Marshall
Lake Property. The Norton Lake property has a NI 43 -101 compliant Measured and Indicated
resource of 2.26 million tonnes @ 0.67% Ni, 0.61% Cu, 0.03% Co and 0.46 g/t Pd.
On behalf of the Board of Directors,
Copper Lake Resources Ltd.
Terry MacDonald, CEO
(416) 561-3626
www.copperlakeresources.com
Neither the TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in
the policies of the TSX Venture Exchange) accepts responsibility for the adequacy or accuracy of
this release.