Exhibit 99.1 included with this Report on Form 6-K is hereby incorporated by reference into the Company's Registration
Statement on Form F-10 (File No. 333-297311) and shall be deemed to be a part thereof from the date on which this report on Form 6-K is
furnished, to the extent not superseded by documents or reports subsequently filed or furnished.
Exhibit 99.1
|
NASDAQ SGLD
TSXV: SGLD
#750-1095 W. Pender St.
Vancouver, BC V6E2M6
WWW.SCORPIOGOLD.COM
|
SCORPIO GOLD DRILLS 3.02 G/T GOLD OVER
48.92 METRES FROM 118.87 METRES AND 1.19 G/T GOLD OVER 99.94 METRES FROM 98.61 METRES AT THE GOLDWEDGE TARGET AT MANHATTAN
Highlights
| ● | Hole 26MN-115 returned, at Goldwedge: |
| ○ | 3.02 g/t gold over 48.92 metres (“m”) from 118.87 m including 19.29 g/t gold
over 5.24 m from 151.79 m within the Zanzibar Formation. |
| ○ | 5.14 g/t gold over 10.15 m from 173.58 m, at the faulted contact of the Zanzibar Formation
and Manhattan Caldera Volcanics. |
| ○ | 0.46 g/t gold over 16.70 m from 210.92 m within the Manhattan Caldera Volcanics |
| ● | Hole 26MN-118 returned, at Goldwedge: |
| ○ | 1.19 g/t gold over 99.94 m from 98.61 m including 5.13 g/t gold over 4.16 m from 147.82
m within the Zanzibar Formation. |
| ● | Hole 26MN-116 returned, along the Zanzibar Trend: |
| ○ | 0.93 g/t gold over 22.16 m from 95.71 m including 3.72 g/t gold over 3.75 m from 98.66
m, within the Gold Hill Formation. |
| ○ | 0.84 g/t gold over 25.05 m from 205.07 m including 3.63 g/t gold over 3.47 m from 213.33
m, within the Gold Hill Formation. |
September 2, 2026 - Vancouver, British
Columbia – Scorpio Gold Corp. (NASDAQ: SGLD, TSXV: SGLD, OTCQB: SRCRF, FSE: RY9) (“Scorpio Gold”,
or the “Company”) is pleased to announce results from four drill-holes of the Phase Two drill program
at the Manhattan District Project (“Manhattan”), Nevada, USA: 26MN-113, 26MN-115, 26MN-116, and 26MN-118, see
Figure 1. The results are tabulated in Table 1 and discussed below. Scorpio Gold has drilled 114 drill holes to date
from its Phase Two diamond drilling program, 25MN-011 through 25MN-045, 26MN-046 through 26MN-123, for a grand total of 32,585
m. With the results herein, Scorpio Gold has reported assays on 107 of these (25MN-011 through 25MN-045, 26MN-046 through
26MN-116, and 26MN-118, totalling 30,889 m, and assays are pending from 7 holes (26MN-117 and 26MN-119 through 26MN-123),
totalling 1,696 m. The pending results will be reported as they become available.
“Manhattan keeps delivering on
the two things that matter most in this market: scale and grade. Hole 26MN-115 — 19 gram per tonne gold over 5 metres contained
within 3 grams across 48 metres — confirms that high grade feeder zones sit within an expanding bulk tonnage envelope. Just
as importantly, every hole at Goldwedge is sharpening our structural understanding of the system: we can now trace mineralization
along the Reliance Fault, from the Zanzibar sediments in its hanging wall through to the Caldera volcanics at the contact, and
that model is directly guiding where we drill next. Grades like these put a potential underground startup on the table as a nearer-term
path to production, while the broader district — eight and a half kilometres of strike anchored by existing historic resources
— needs modern, systematic drilling to expand toward its true district scale potential. Few juniors can offer that combination
of near-term optionality and district-scale upside, and we intend to keep advancing both,” said Zayn Kalyan, CEO and Director
of Scorpio Gold.
Figure 1. Surface Plan Map of drill
holes.
Goldwedge: Drill holes 26MN-115
and 26MN-118 are both approximately 50 m step-outs along the projected Reliance Fault from high grade gold intercepted in drill
hole 26MN-091, within the Manhattan Caldera Volcanics. Recent drilling at Goldwedge, including the results herein, has demonstrated
consistently strong mineralization, especially in the Paleozoic sediments of the Ordovician Zanzibar Formation, located
in the hanging wall of the Reliance Fault. The Reliance Fault is considered one of many feeders to mineralization. Additionally,
recent results have proven that the Manhattan Caldera Volcanics can likewise host lower grade envelopes around high grade feeder
structures, as demonstrated by the following previously reported intercepts:
| ● | 1.69 g/t gold over 55.70
m from 118.90 m (24MN-009) |
| ● | 0.59 g/t gold over 49.23
m from 31.69 m (26MN-048) |
| ● | 11.84 g/t gold over 8.39
m from 106.21 m (26MN-075) |
| ● | 1.27 g/t gold over 45.23
m from 137.95 m (26MN-086) |
| ● | 1.17 g/t gold over 21.58
m from 111.71 m (26MN-089) |
| ● | 2.04 g/t gold over 11.83
m from 115.67 m (26MN-091) |
| ● | 1.60 g/t gold over 33.53
m from 6.70 m (26MN-101) |
| ● | 3.38 g/t gold over 33.31
m from 138.90 m (26MN-109) |
2.05 g/t gold over 97.99
m from 64.16 m (26MN-110)
The Gap Zone: The Gap Zone is the
previously undrilled area that connects Goldwedge to the Reliance Trend and ultimately, the historic West Pit. Mineralization is
hosted entirely within the meta-sediments of the Gold Hill Formation and is dominantly controlled by veins and structures related
to the steeply dipping Reliance Fault. First tested in early 2025, significant mineralization at the Gap Zone includes:
| ● | 1.24 g/t gold over 92.81
m from 3.05 m (25MN-011) |
| ● | 1.27 g/t gold over 14.75
m from 194.95 m (25MN-013) |
| ● | 0.80 g/t gold over 33.13
m from 118.38 m (25MN-017) |
| ● | 0.94 g/t gold over 36.97
m from 162.95 m (25MN-020) |
| ● | 2.21 g/t gold over 7.38
m from 222.14 m (25MN-030) |
Zanzibar Trend: The Zanzibar Trend
is the previously underexplored area between Mustang Hill and Goldwedge along the faulted contact of the Paleozoic meta-sediments
and the Oligocene aged volcanics of the Manhattan Caldera. High grade gold mineralization is encountered along two main controlling
features: sub-vertical structures parallel to the main contact fault, and along gently to moderately dipping bedding planes primarily
in the Cambrian Gold Hill Formation. Drill hole 26MN-116 steps out approximately 50 m to multiple drill holes along the trend,
including 26MN-067, 25MN-045, and 26MN-087. The results reported herein add to the significant mineralization encountered
along the Zanzibar Trend, including:
| ● | 3.14 g/t gold over 49.62
m from 59.95 m (25MN-044) |
| ● | 0.66 g/t gold over 57.64
m from 29.59 m (25MN-045) |
| ● | 2.10 g/t gold over 22.25
m from 34.14 m (26MN-063) |
| ● | 2.74 g/t gold over 16.49
m from 45.45 m (26MN-066) |
| ● | 12.78 g/t gold over 5.91
m from 134.51 m (26MN-067) |
| ● | 0.69 g/t gold over 23.23
m from 4.05 m (26MN-070) |
| ● | 2.68 g/t gold over 11.34
m from 0.76 m (26MN-071) |
| ● | 2.77 g/t gold over 12.68
m from 58.64 m (26MN-080) |
| ● | 0.98 g/t gold over 23.20
m from 112.13 m (26MN-114) |
Black Mammoth: Black Mammoth is
a ~200+ m step-out from Goldwedge. Strong gold mineralization can be found within the Ordovician Zanzibar sediments along structures
related to the Black Mammoth Fault, and on both sides of the major fault defining the contact between the Paleozoic sediments and
the Oligocene aged volcanics of the Manhattan Caldera. Results at Black Mammoth will be reported as they become available. Significant
mineralization includes:
| ● | 0.75 g/t gold over 24.69
m from 230.12 m (26MN-053) |
| ● | 1.02 g/t gold over 40.23
m from 195.69 m (26MN-057) |
| ● | 0.62 g/t gold over 62.21
m from 230.43 m (26MN-069) |
| ● | 6.04 g/t gold over 4.86
m from 308.23 m (26MN-072) |
| ● | 0.58 g/t gold over 18.04
m from 311.05 m (26MN-078) |
| ● | 0.83 g/t gold over 18.01
m from 277.68 m (26MN-092) |
| ● | 2.56 g/t gold over 13.38
m from 293.28 m (26MN-096) |
All 2026 drill holes tested within and
beyond the Inferred Resource Constraining Pit (“IRCP”), targeting new mineralization outside of the
2025 MRE block model, see Figure 2. For further details see “Mineral Resource Estimate and NI 43-101 Technical Report,
Manhattan Property, Nye County, Nevada” with an effective date of June 4, 2025, on Scorpio Gold’s website at Technical
Report.
| Drill Hole ID |
Target
Azimuth / Dip |
From (m) |
To (m) |
Intercept¹ (m) |
Gold (g/t) |
| 26MN-115 |
Goldwedge |
118.87 |
167.79 |
48.92 |
3.02 |
| 388 m |
342° / -45° |
| |
including |
151.79 |
157.03 |
5.24 |
19.29 |
| |
|
173.58 |
183.73 |
10.15 |
5.14 |
| |
|
210.92 |
227.62 |
16.70 |
0.46 |
| 26MN-116 |
Zanzibar Trend |
95.71 |
117.87 |
22.16 |
0.93 |
| 285 m |
056° / -50° |
| |
including |
98.66 |
102.41 |
3.75 |
3.72 |
| |
|
166.33 |
170.38 |
4.05 |
0.87 |
| |
|
205.07 |
230.12 |
25.05 |
0.84 |
| |
including |
213.33 |
216.80 |
3.47 |
3.63 |
| 26MN-118 |
Goldwedge |
59.28 |
68.88 |
9.60 |
0.58 |
| 344 m |
344° / -62° |
98.61 |
198.55 |
99.94 |
1.19 |
| |
including |
126.95 |
139.75 |
12.80 |
1.86 |
| |
and |
147.82 |
152.00 |
4.18 |
5.13 |
| |
|
227.38 |
235.52 |
8.14 |
0.25 |
| 26MN-113 |
Moriah |
51.79 |
53.95 |
2.16 |
0.35 |
| 716 m |
135° / -45° |
| ¹ Intervals contain no more than 3 continuous metres grading less than 0.1 g/t gold. |
Table 1. Results from the current batch of drill holes. Note:
There is insufficient geological information to estimate a true width for the drill intercepts reported.
Goldwedge Results:
26MN-115: This drill hole contains three significant
intercepts hosted in both the Ordovician Zanzibar Formation and the Oligocene Volcanics of the Manhattan Caldera (See cross-section
A-A’ in Figure 2 and cross-section B-B’ in Figure 3). The gold mineralization is focused into a structurally
complex zone of faulted and brecciated limestones and limey mudstones of the Ordovician Zanzibar Formation on the hanging wall
of the main contact fault separating the Paleozoic sediment package from the Manhattan Caldera Volcanics (See cross-section B-B’
in Figure 3). The first and longest interval averages 3.02 g/t gold over 48.92 m from 118.87 m and is typical of
the Goldwedge area in that it is generally composed of brecciated Zanzibar limestone and mudstone, with multiple small gouge zones
as well as sulfide and quartz healed breccias that can be well mineralized with gold (See annotated core photos in Figure 5).
The Goldwedge target zone is interpreted as a flower structure associated with the dextral strike/slip fault zone that juxtaposes
the Paleozoic sediments of the Zanzibar and Gold Hill Formations against the much younger volcanic rocks of the Manhattan Caldera.
This allows for many fluid pathways to the surface, resulting in high grade intercepts along the individual fault planes, enveloped
by moderate grades in the surrounding breccia (See cross-section B-B’ in Figure 3). The second interval averages
5.14 g/t gold over 10.15 m from 173.58 m and represents the main fault structure. Lenses of multiple rock types are entrained
within the fault damage zone, including limestones and mudstones of the Zanzibar Formation, as well as ash tuff and lapilli tuff
from the Manhattan Caldera volcanics. The third intercept lies entirely within the Manhattan Caldera Volcanics and averages 0.46
g/t gold over 16.70 m from 210.92 m downhole. This interval is structurally continuous with the neighboring drillhole 26MN-091
which contained 6.95 g/t gold over 11.98 m (see press release dated June 9, 2026) and represents a secondary structure
running parallel to the main fault zone.
26MN-118: Drillhole 26MN-118 contains three notable gold
intercepts hosted in both the Paleozoic meta-sediments of the Zanzibar and Gold Hill Formations, as well as the Volcanics of the
Manhattan Caldera. The geology of this drillhole is very similar to the neighboring drillhole 26MN-115 discussed above, encountering
the complex upward flaring structures that cut through the Goldwedge zone proximal to the main fault separating the sedimentary
rocks southwest of the fault from the volcanic rocks to the northeast (Figure 3 and Figure 4). The first significant gold
mineralization encountered in this drillhole averages 0.58 g/t gold over 9.60 m from 59.28 m with the highest grades in
this interval being found in gouge zones in otherwise brecciated limestones and mudstones of the Ordovician Zanzibar Formation.
The second interval is the most continuous and averages 1.19 g/t gold over 99.94 m from 98.61 m within brecciated limestones
and mudstones of the Zanzibar formation, as well as altered siliciclastic sediments of the Cambrian Gold Hill Formation. Near the
bottom of the interval there are clasts of Oligocene aged volcanics that have been entrained in the larger structural zone from
the footwall country rock of the Manhattan Caldera. Throughout the interval, discrete structural zones are defined by stronger
alteration and gouge, as well as elevated gold grades. In some cases, the breccias have been fully healed by a quartz/sulfide matrix
and can contain high grade gold values (Figure 6). The final notable intercept occurs fully within the volcanic rocks of
the Manhattan Caldera, along a subsidiary structure that is sub-parallel to the main contact fault. It averages 0.25 g/t gold
over 8.14 m from 227.38 m downhole and appears to be continuous with both drillhole 26MN-115 and other neighboring drillholes
at approximately 50m step outs from each other.
Figure 2. Cross-section A-A’, showing
gold grades with reported intervals highlighted.

Figure 3. Cross-section B-B’, showing
gold grades with reported intervals highlighted and schematic of flower structure interpretation.

Figure 4. Plan view of Goldwedge target
area and interpreted geology.

Figure 5. Drill hole 26MN-115, interval
151.79 m to 158.50 m, displaying brecciated and altered meta-mudstones locally healed by quartz/adularia and fine-grained sulfide
matrix.

Figure 6. Drill hole 26MN-118, interval
178.00 m to 184.65 m, displaying brecciated and altered meta-mudstones and marbles locally healed by quartz/adularia and fine-grained
sulfide matrix.
Zanzibar Trend Results:
26MN-116: This drill hole contains three significant
gold intercepts, all hosted within the Cambrian Gold Hill Formation. The first interval contained an average grade of 0.93 g/t
gold over 22.16 m m from 95.71 m downhole. It is a hosted within alternating beds of meta-mudstones and dolomitic marbles crosscut
by small scale structures that typically have moderate clay alteration along them. Proximal to the clay altered zones the host
rocks are strongly silicified, containing dissolution vugs as well as drusy epithermal quartz veins. The second notable interval
in this drillhole contained an average grade of 0.87 g/t gold over 4.05 m from 166.33 m downhole, and is geologically similar
to the first intercept. The third significant intercept in drillhole 26MN-116 contained an average of 0.84 g/t gold over 25.05
m from 205.07 m and is notable for containing the same characteristics as the first two intercepts, with the addition of some
quartz/sulfide healed breccia zones correlating to the higher grades in this drillhole. Results from this drillhole confirm that
there are multiple controls on the gold mineralization at the Zanzibar Trend, specifically sub-vertical structures that are related
to and generally parallel with the main fault separating the Paleozoic sediments and the Oligocene-aged Volcanics of the Manhattan
Caldera, and the gently to moderately north-dipping bedding within the Zanzibar and Gold Hill Formations. Where these two controls
intersect, strong gold mineralization can be found.
Moriah Results:
26MN-113: This was the first known drillhole at the Moriah
Target, which is notable for the extensive historic workings in the area including large adits and deep shafts. Field mapping had
identified the same prospective Zanzibar Limestones that are preferred gold hosts at Goldwedge and the Zanzibar Trend, as well
as extensional faults and veining associated with the epithermal system seen elsewhere on the property. The drillhole did intersect
prospective units and structure near the top of the hole, and moderate silicification and veining near the bottom, however significant
gold mineralization was not encountered. Further work will be undertaken to interpret the geological information gathered from
this drillhole to refine the targeting strategy at the Moriah target.
QA/QC
HQ sized diamond drill core samples were
cut in halves, then bagged and secured with security tags to ensure integrity during transportation to the Elko, NV, MSALABS facility
for preparation. For quality assurance (“QA”), unmarked coarse blanks, unmarked certified reference materials,
and requested laboratory duplicates were inserted into the sampling sequence. QA samples were systematically inserted into each
batch of samples, amounting to approximately 10% of the run of samples. Samples were analyzed for gold using a two-cycle PhotonAssayTM
analysis method (~500 g) of crushed material (70% passing 2 mm). All MSALABS facilities comply with ISO 17025:2017.
About the Manhattan District
Manhattan, located in the Walker Lane
Trend of Nevada, USA, is road accessible and lies approximately 20 kilometers south of the operating Round Mountain Gold Mine
(https://www.kinross.com/operations/default.aspx#americas-roundmountain), which has produced more than 15 million ounces
of gold. For the first time, the Company has consolidated Manhattan’s past-producing mines under a single entity that holds
valuable permitting and water rights. Historically, Manhattan has produced approximately 700,000 ounces of gold from high-grade
placer and lode operations dating from the late 1890s through to the mid-2000s.¹ The maiden mineral resource estimate (the
“Maiden MRE”) covering the Goldwedge and Manhattan Pit areas of Manhattan is comprised of 18,343,000 tonnes
grading 1.26 g/t gold for a total of 740,000 oz contained gold in the inferred category.²
A historical mineral resource estimate
(the “Historical MRE”) covers the Black Mammoth, April Fool, Hooligan, Keystone, and Jumbo areas of Manhattan
and comprises 1,652,325 tonnes grading 5.89 g/t gold for a total of 303,949 oz contained gold.³ The deposit is interpreted
as a low-sulfidation, epithermal, gold-rich system situated adjacent to the Tertiary-aged Manhattan caldera in the Southern Toquima
Range of Nevada. A “Qualified Person” as defined in National Instrument 43-101 - Standards of Disclosure for Mineral
Projects (“NI 43-101”) has not done sufficient work to make the Historical MRE current, and the Company
is not treating the Historical MRE as current.
Notes
| ● | Adjacent Properties: The Company has no interest in, or rights to, any of the
adjacent properties mentioned, including the Round Mountain Gold Mine, and exploration results on adjacent properties are not necessarily
indicative of mineralization on the Company’s properties. Any references to exploration results on adjacent properties are
provided for information only and do not imply any certainty of achieving similar results on the Company’s properties. |
| ● | Historical Data: This news release includes historical information that has been
reviewed by the Company’s qualified person. The Company’s review of the historical records and information reasonably
substantiate the validity of the information presented in this presentation. The Company encourages readers to exercise appropriate
caution when evaluating these data and/or results. |
| ● | Third-Party Mineral Projects: These deposits are cited solely for geological context.
The Company cautions that these properties are not necessarily adjacent to, nor does the Company or have any interest in or control
over them. Although certain geological features may be similar, there is no assurance that mineralization comparable to these deposits
will be discovered on any of the Company’s properties. Information regarding the aforementioned deposits is taken from publicly
available sources and technical reports believed to be reliable but has not been independently verified by the Company. The Company
encourages readers to exercise appropriate caution when evaluating these data and/or results. |
| ● | Mineral Resource Estimate (MRE): All scientific and technical information relating
to Manhattan pertaining to Maiden MRE contained in this news release is derived from the Technical Report dated April 23, 2026
(with an effective date of June 4, 2025) titled “Mineral Resource Estimate and NI 43-101 Technical Report” (the “Technical
Report”) prepared by Matthew R. Dumala, P.Eng (BC) of Archer Cathro Geological (US) Ltd., Patrick Loury, M.Sc., CPG (AIPG)
of Daniel Kunz & Associates, Annaliese Miller, LG (WA) of Geosyntec Consultants, Inc. and Art Ibrado, PhD, PE (AZ) of Fort
Lowell Consulting PPLC. The information contained herein in respect of the Maiden MRE is subject to all of the assumptions, qualifications
and procedures set out in the Technical Report and reference should be made to the full text of the Technical Report, a copy of
which has been filed with the applicable securities regulators and is available under the Company’s profile on www.sedarplus.ca. |
| ● | Historical MRE: A Qualified Person has not done sufficient work to make the Historical
MRE current, and the Company is not treating the Historical MRE as current. |
The Company considers the
Historical MRE relevant as it demonstrates the presence of significant gold mineralization across multiple zones within Manhattan;
however, its reliability is uncertain because it was prepared prior to the adoption of the current CIM Definition Standards and
current QA/QC practices. The Historical MRE provides limited disclosure of assumptions, parameters, estimation methods, cutoff
grades, and QA/QC protocols, and therefore these cannot be fully verified by the Company. The categories used in the historical
estimate predate, and are not directly comparable to, current CIM Definition Standards, and the Company is not treating the Historical
MRE as a current Mineral Resource Estimate. To upgrade and verify the Historical MRE in order to make it a current Mineral Resource
Estimate, the Company would be required to undertake confirmatory drilling, modern QA/QC sampling, validation and digitization
of historical datasets and updated geological modeling followed by the preparation of a new Mineral Resource Estimate in accordance
with CIM Definition Standards and NI 43-101. The Company encourages readers to exercise appropriate caution when evaluating the
Historical MRE.
All scientific and technical
information relating to Manhattan pertaining to the Historical MRE contained in this news release is derived from the Technical
Report dated May 1997 titled “Exploration and Pre-Production Mine Development, Manhattan District Project, Nye County”
(the “Historical Technical Report”) prepared by New Concept Mining, Inc. The information contained herein in
respect of the Historical MRE is subject to all the assumptions, qualifications and procedures set out in the Historical Technical
Report and reference should be made to the full text of the Historical Technical Report.
| ● | References: (1) Strachan, D. G., and Master, T. D., 2005: Update and Revision
of the Gold Wedge Project Development, Nye County. Report prepared for Nevada; Royal Standard Minerals, Inc. and dated March 31,
2005; (2) Dumala, M. R., and Lowry, P., 2025: Mineral Resource Estimate and NI 43-101 Technical Report, Manhattan Property, Nye
County, Nevada. Report prepared for Scorpio Gold Corporation and dated October 23, 2025 (with an effective date of June 4, 2025);
and (3) Berry, A., and Willard, P., 1997: "Exploration and Pre-Production Mine Development, Manhattan District Project, Nye
County". Report prepared for New Concept Mining, Inc. and dated May 1997. |
Qualified Person
The scientific and technical information in this news release has been reviewed, verified and approved by Leo Hathaway, P. Geo.,
Executive Technical Director of Scorpio Gold, a "Qualified Person", as defined under National Instrument 43-101 Standards
of Disclosure for Mineral Projects. Verification included review of laboratory certificates, review of field logs and chain-of-custody
records, inspection of blank/standard/duplicate performance, and review of collar and down-hole survey data. No limitations or
failures to verify were identified.
About Scorpio Gold Corp.
Scorpio Gold holds a 100% interest in
the Manhattan District located in the Walker Lane Trend of Nevada, USA. Scorpio Gold's Manhattan District is ~4,780-hectares and
comprises the advanced exploration-stage Goldwedge Mine, and four past-producing pits that were acquired from Kinross in 2021
(see news release dated March 25, 2021 https://scorpiogold.com/news/scorpio-gold-closes-purchase-of-kinross-manhattan-property-nye-county-nevada/).
The consolidated Manhattan District presents an exciting late-stage exploration opportunity, with over 140,000 metres of historical
drilling, significant resource potential, and valuable permitting and water rights.
Neither the TSX Venture Exchange nor
its Regulation Services Provider (as that term is defined in the policies of the Exchange) accepts responsibility for the adequacy
or accuracy of this release.
ON BEHALF OF THE BOARD OF SCORPIO GOLD
CORPORATION
Zayn Kalyan, Chief Executive Officer
and Director
Tel: (604)-252-2672
Email: zayn@scorpiogold.com
Investor Relations Contact:
Email: ir@scorpiogold.com
Connect with Scorpio Gold:
Email | Website | Facebook | LinkedIn | X | YouTube
To register for investor updates please
visit: scorpiogold.com
NASDAQ: SGLD | TSXV: SGLD
| FSE: RY9
Forward-Looking
Statements
This news release contains statements
that constitute “forward-looking statements” or "forward-looking information" within the meaning of applicable
securities laws (collectively, "forward-looking statements"). Such forward-looking statements involve known and unknown
risks, uncertainties and other factors that may cause the Company’s actual results, performance or achievements, or developments
to differ materially from the anticipated results, performance or achievements expressed or implied by such forward-looking statements.
Forward-looking statements are statements that are not historical facts and are generally, but not always, identified by the words
“expects,” “plans,” “anticipates,” “believes,” “intends,” “estimates,”
“projects,” “potential” and similar expressions, or that events or conditions “will,” “would,”
“may,” “could” or “should” occur. Forward-looking statements are based on the beliefs, estimates
and opinions of the Company's management as of the date of this news release.
Forward-looking statements in this news
release include, among others, statements relating to: the timing, scope and interpretation of assay results; potential for resource
growth and discovery; the potential continuity, extent, grade and characteristics of mineralization along the Reliance Trend, Black
Mammoth, Gap Zone, Zanzibar Trend and Mustang Hill; the intended follow-up exploration activities and timing thereof; the Company's
exploration plans and objectives; expected future drilling programmes; anticipated timing of future disclosures and announcements;
and other statements that are not historical facts. In making the forward-looking statements in this news release, the Company
has applied several material assumptions, including: that the Company will be able to obtain sufficient financing to complete planned
exploration activities; that the Company will be able to obtain necessary permits and regulatory approvals in a timely manner;
that exploration results will be consistent with management's expectations; that general business and economic conditions will
not change in a materially adverse manner; that equipment and qualified personnel will be available when required; and that the
Company's interpretations of geological data are accurate. By their nature, forward-looking statements involve known and unknown
risks, uncertainties and other factors which may cause our actual results, performance or achievements, or other future events,
to be materially different from any future results, performance or achievements expressed or implied by such forward-looking statements.
Such factors and risks include, among others: the Company may require additional financing from time to time in order to continue
its operations, which may not be available when needed or on acceptable terms and conditions; the inherent risks involved in the
exploration and development of mineral properties, including uncertainties related to the interpretation of drill results and other
geological data; fluctuations in commodity prices; compliance with extensive government regulation and changes in domestic and
foreign laws and regulations that could adversely affect the Company’s business and results of operations; uncertainties
related to obtaining necessary permits and regulatory approvals; risks related to the Company's ability to retain key personnel;
environmental risks and hazards; title matters and surface rights issues; competition in the mining industry; the stock markets
have experienced volatility that often has been unrelated to the performance of companies and these fluctuations may adversely
affect the price of the Company’s securities, regardless of its operating performance; and other risks and uncertainties
disclosed in the Company's public filings.
The forward-looking information contained
in this news release represents the expectations of the Company as of the date of this news release and, accordingly, is subject
to change after such date. Readers should not place undue importance on forward-looking information and should not rely upon this
information as of any other date. The Company undertakes no obligation to update these forward-looking statements in the event
that management's beliefs, estimates or opinions, or other factors, should change.