Renforth Grab Samples 0.71% Ni from Unexplored Area of ~20km Victoria Mineralized Structure
September 26, 2022 CSE: RFR
For Immediate Release OTCQB: RFHRF
Renforth Grab Samples 0.71% Ni from Unexplored Area of ~20km Victoria Mineralized Structure
• New outcrop mineralization discovered east of road, near centre of ~20km Victoria structure, highest
grab sample result 0.71% Ni in albitized ultramafic with sulfides
• Discovery of second band of mineralization north of previous drilling at Victor ia
• Lalonde delivered consistent elevated values including 0.33% Ni in grab samples from mineralized
horizon currently being stripped
Renforth Resources Inc. (CSE – RFR) (OTCQB– RFHRF) (FSE-9RR) (“Renforth” or the “Company”) is pleased to
deliver to shareholders results from prospecting targeting the polymetallic intrusive mineralization at Surimeau
during May-July 2022. These results include 0.71% Ni in a grab sample from a previously unexplored area of
central Victoria (east of the Rapide 7 road) and two assay results of 0.32% Ni in two separate grab samples
obtained within the current stripping area at Lalonde west (west of the Rapide 7 road).
Grab samples are preferentially selected and not representative of the entirety of a structure. In the case of
Lalonde west follow up work consisting of stripping a wide band perpendicular (north/south) to the mineralized
Lalonde structure (which runs east/west), followed by channel sampling, is ongoing as previously announced. In
the case of central Victoria additional prospecting will be undertaken this fall.
"These initial results validate the extent of surface mineralization on our Surimeau District Property. Our current
interpretation is two separate polymetallic mineralized systems essentially running east/west, outcropping on
surface, with lengths of ~20kms at Victoria and currently ~9km at Lalonde, the latter is still open on strike and
unexplored. West of the Rapide 7 road the two horizons are separated north/south by ~3.7km. Copper and Zinc
mineralization is hosted in a thick sequence of greywacke with graphitic mudstone interlayers while Nickel and
Cobalt mineralization is hosted within ultramafic flows. The best mineralization is often found within and
around sheared, albite altered, and calc-silicate altered ultramafics the sedimentary contact. We continue to
learn more about this property with ongoing exploration to determine the extent and sur face grade of the
mineralization. We intend to drill at Victoria west this winter, building on the drilled mineralized package as
deep as 180m with an ~125m package width over the ~2.2km we have drill ed. We will also likely drill Lalonde
west of the road for the first time. Our grab samples reflect the consistent presence of polymetallic
mineralization with a wide range of grades, clearly there is with more work required, which we will do" states
Nicole Brewster, President and CEO of Renforth.
2022 Prospecting Results Summarized
This press release reports on prospecting results obtained from the Victoria and Lalonde trends during the 2022
season, prior to trenching. Work to date leads Renforth to conclude that the Victoria and Lalonde are of similar
mineralization environments, interpreting the geological setting as being a type of hybrid volcanogenic massive
sulfide (VMS) and mono-sulfide solid solution (MMS) system where there was interaction between intruding
Nickel enriched ultramafic magmas and sulfide-enriched sedimentary material leading to the formation of
nickel mineralization alongside anomalous zinc and copper from any assimilated VMS systems. Following this
prospecting work, a channel cutting program was carried out (results pending). Currently, the property has
Unit 1B 955 Brock Road
Pickering ON L1W 2X9
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been chipped and stripped with channel cutting ongoing at Lalonde. Renforth's geologists will map and sample
the newly stripped areas subsequent to a field break allowing the local community uninterrupted access for
hunting. The results of the prospecting work highlighted below demonstrated to Renforth the consistent
presence of some amount of polymetallic (Nickel, Cobalt, Copper and Zinc) mineralization throughout each
system and support the continued exploration of the property in order to determine the size and extent of the
occurrences.
Victoria East and West Prospecting Result Highlights
Sample # Location Litho Outcrop Sample Ni ppm Co ppm Cu ppm Zn ppm
81094 Victoria East V4
Ultramafic,
massive with
zones of spinifex
texture, non-mag,
dark green, series
of NW-Se trending
dykes
Ultramafic,
massive with
zones of spinifex
texture, non-mag,
dark green, series
of NW-Se trending
dykes
1730 192 60 110
81096 Victoria East V4
Same spot as
above, either
contact or
weathered
differently
because of
blowdown tree,
surface is soft
greasy and talcose,
Ultramafic,
massive, fine to
med grained, blue-
grey colour, clots
of coarse calcite,
trace py
Same spot as
above, either
contact or
weathered
differently
because of
blowdown tree,
surface is soft
greasy and talcose,
Ultramafic,
massive, fine to
med grained, blue-
grey colour, clots
of coarse calcite,
trace py
1690 101 70 60
81131 Victoria East V4
Ultramafic, bands
of mod to strong
albitization,
pyroxene rich
band, rare 2 cm
qz-ab veinlets + 1-
2 mm ab stringers,
patchy weak mag,
2-4 % diss py
throughout, ,
locally up to 7%
py, fol at 94/30N ,
sulphides are
lineated
Ultramafic, bands
of mod to strong
albitization,
pyroxene rich
band, rare 2 cm
qz-ab veinlets + 1-
2 mm ab stringers,
patchy weak mag,
2-4 % diss py
throughout, locally
up to 7% py
7160 257 260 330
81197 Victoria East V3
Mafic volcanic,
aphanitic, dark
grey-black, mod to
strong mag
throughout,
occasional shiny
pyroxene crystals,
trace py, massive
Mafic volcanic,
aphanitic, dark
grey-black, mod to
strong mag
throughout,
occasional shiny
pyroxene crystals,
trace py, massive,
smooth bedrock,
possible large frost
heave boulder
from nearby
1830 131 20 110
81198 Victoria East V3
Same as 81197, 2
m tall 25 m long
ridge in low relief
area, oriented 250
(E-W), possible
pillows visible on
surface
Same as 81197, 2
m tall 25 m long
ridge in low relief
area, oriented 250
(E-W), possible
pillows visible on
surface
1640 120 50 90
81199 Victoria East V3
Same as 81197,
weak fol at
260/30N
Same as 81197,
weak fol at
260/30N
1650 114 50 70
81231 Victoria West V4
Greenish
ultramafic, med
grained, patches /
bands of mod to
strong albitization,
with 1%py/po
locally up to 3%,
flat ridge oriented
86/60N
Greenish
ultramafic, med
grained, patches /
bands of mod to
strong albitization,
with 1%py/po
locally up to 3%
620 110.5 1400 520
81232 Victoria West V4
Main shear like
rock, deeply
weathered thus
micaceous,
strongly albitized,
low ridge striking
230/60N conc to
fol, trace -1 %
sulphides, often
weathered out
Main shear like
rock, deeply
weathered thus
micaceous,
strongly albitized,
low ridge striking
230/60N conc to
fol, trace -1 %
sulphides, often
weathered out
510 100.5 1380 16500
81035 Victoria West V4
Looks identical to
shear zone in
trench, deeply
weathered,
strongly albitized,
strongly foliated at
247/70N, well
mineralized, 15 %
diss + stringers and
clots, py-sph
Looks identical to
shear zone in
trench, deeply
weathered,
strongly albitized,
strongly foliated at
247/70N, well
mineralized, 15 %
diss + stringers and
clots, py-sph
240 83.2 1470 3860
81064 Victoria West V4
North side of same
ridge as sample
81062, E-W
orientation, calc-
silicate v4,
aphanitic, mod
albitization, mod
bt, 5-15% fine
sulfides (py-po),
sulfur odor around
outcrop.
Calc-silicate v4,
aphanitic, mod
albitization, mod
bt, 5-15% fine
sulfides (py-po),
sulfur odor around
outcrop.
1820 196 210 230
81076 Victoria West V4
Same ridge as
above, ultramafic,
aphanitic,
serpentinized, 20
m from 81075,
weak albitization
Ultramafic,
aphanitic,
serpentinized, 20
m from 81075,
weak albitization
1820 91.4 0 70
*Results presented above are grab samples and only represent the material sampled. Additional samples were taken in this
program and are not reported on in this release. Mapped prospecting results are available on the website.
Lalonde East and West Prospecting Result Highlights
Sample Location Litho Outcrop Sample Ni ppm Co ppm Cu ppm Zn ppm
81142 Lalonde
East V4
Strongly
albitized,
deeply
weathered,
sheared rock,
very similar to
main shear in
Victoria
trench, strong
fol at 94/70N,
well
mineralized py
+ sph, stringers
and clots along
foliation, 5-
10% sulphides
overall
Strongly albitized,
deeply weathered,
sheared rock, very
similar to main shear in
Victoria trench, strong
fol at 94/70N, well
mineralized py + sph,
stringers and clots along
foliation, 5-10%
sulphides overall
110 52.8 380 17900
81251 Lalonde
East V3
Boulder sub
angular in
swamp 2x2 m
maf vol, dark grey black
colour, fine-med
grained mod mag
throughout, trace fine
py, rare fine ab blebs
throughout
1520 80 50 60
81118 Lalonde
East V4
Massive
ultramafics,
trace to 1 %
diss py, po,
green colour,
serpentinized
Massive ultramafics,
trace to 1 % diss py, po,
green colour,
serpentinized
1430 106 160 90
81119 Lalonde
West V4
Ultramafic,
dark green,
coarse grained,
massive,
dense, rare 1-3
mm qz-ab
stringers, 2-5
% fine to med
diss py, po
throughout,
locally up to
10%, weak to
mod mag
throughout
Ultramafic, dark green,
coarse grained, massive,
dense, rare 1-3 mm qz-
ab stringers, 2-5 % fine
to med diss py, po
throughout, locally up
to 10%, weak to mod
mag throughout
3220 208 360 390
81123 Lalonde
West V4
Tallish ridge,
Lalonde east
area
powerline,
strongly
foliated
104/44NE,
albitized
ultramafic with
fine stringers
and diss py,
po, up to 10-12
%
Strongly foliated
104/44NE, albitized
ultramafic with fine
stringers and diss py,
po, up to 10-12 %
3220 297 160 240
81085 Lalonde
West V4
Same ridge as
81119,
Ultramafic,
dark green,
coarse
tremolites in
aphanitic
groundmass,
10-20% fine to
med diss py,
po, possible
trace bornite,
presence of
reworked/
broken red
garnets within.
Ultramafic, dark green,
coarse tremolites in
aphanitic groundmass,
10-20% fine to med diss
py, po, possible trace
bornite, presence of
reworked/ broken red
garnets within.
2140 160 410 570
81304 Lalonde
West V3
Sheared maf
vol,
ultramafics,
strongly
foliated, and
actinolized
sediments,
possibly,
amphibolized
maf vol <1mm
ab stringers
conc to fol at
313/steep
slight NE
Sheared maf vol,
ultramafics, strongly
foliated, and actinolized
sediments, possibly,
amphibolized maf vol
<1mm ab stringers conc
to fol at 313/steep
slight NE
1690 110 20 130
*Results presented above are grab samples and only represent the material sampled. Additional samples were taken in this
program and are not reported on in this release. Mapped prospecting results are available on the website.
Samples presented in this press release were selected, bagged, and tagged in the field under the supervision of
Francis R. Newton P. Geo (OGQ#2129) and personally delivered to the facilities of ALS Geochemistry in Val d’Or,
Quebec, for analysis using the ME-MS89L assay methodology (Trace Level Lithium Exploration by Na -Peroxide
Fusion).
Technical disclosure in this press release has been reviewed and approved by Francis R. Newton P.Geo
(OGQ#2129), a “qualified person” pursuant to NI 43-101.
For further information please contact:
Renforth Resources Inc.
Nicole Brewster
President and Chief Executive Officer
C:416-818-1393
#Unit 1B – 955 Brock Road, Pickering ON L1W 2X9
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About Renforth
Renforth is focused on Quebec's newest battery metals district, our wholly owned ~330 km2 Surimeau District
Property, which hosts several known areas of polymetallic "battery metals" mineralization, each with various
levels of exploration, as well as a significant amount of unexplored ground. Victoria West has been drilled over a
strike length of 2.2km, within a 5km long mineralized structure, proving nickel, copper, zinc and cobalt
mineralization, in the western end of a 20km magnetic anomaly. The Huston target, during initial
reconnaissance, resulted in a grab sample grading 1.9% Ni, 1.38% Cu, 1170 ppm Co and 4 g/t Ag. Additionally,
the Lalonde, Surimeau and Colonie Targets are all polymetallic mineralized occurrences which, along with
various gold showings, comprise the areas of potential of this NSR free property.
In addition to the Surimeau District battery metals property Renforth wholly owns the Parbec Gold deposit, a
surface gold deposit contiguous to the Canadian Malartic Mine property in Malarti c, Quebec. In 2020/21
Renforth completed 15,569m of drilling which successfully twinned certain historic holes, filled in gaps in the
resource model with newly discovered gold mineralization and extended mineralization deeper. Based upon the
success of this significant drill program the Company considers the spring 2020 MRE, with a resource estimate
of 104,000 indicated ounces of gold at a grade of 1.78 g/t Au and 177,000 inferred ounces of gold at a grade of
1.78 g/t Au to be out of date. With the new data gained Renforth will undertake to complete the first ever
structural study of the mineralization at Parbec, as well as additional total metallic assay work in order to better
contextualize the nugget effect on the gold mineralization.
Renforth also holds the Nixon-Bartleman property, west of Timmins Ontario, with gold present on surface over
a strike length of ~500m.
No securities regulatory authority has approved or disapproved of the contents of this news release.
Forward Looking Statements
This news release contains forward-looking statements and information under applicable securities laws. All
statements, other than statements of historical fact, are forward looking. Forward -looking statements are
frequently identified by such words as ‘may’, ‘will’, ‘plan’, ‘expect’, ‘believe’, ‘anticipate’, ‘estimate’, ‘intend’
and similar words referring to future events and results. Such statements and information are based on the
current opinions and expectations of management. All forward-looking information is inherently uncertain and
subject to a variety of assumptions, risks and uncertainties, including the speculative nature of mineral
exploration and development, fluctuating commodity prices, the risks of obtaining ne cessary approvals, licenses
and permits and the availability of financing, as described in more detail in the Company’s securities filings
available at www.sedar.com. Actual events or results may differ materially from those projected in the forward -
looking statements and the reader is cautioned against placing undue reliance thereon. Forward -looking
information speaks only as of the date on which it is provided and the Company assumes no obligation to revise
or update these forward-looking statements except as required by applicable law.