Metals Creek and Benton Announce Anomalous Concentrations of Hydrogen- Helium Soil Gas at Smoking Gun and Parson's Pond Projects in Newfoundland
Metals Creek and Benton Announce
Anomalous Concentrations of Hydrogen-
Helium Soil Gas at Smoking Gun and Parson's
Pond Projects in Newfoundland
Thunder Bay, Ontario--(Newsfile Corp. - September 9, 2026) - Metals Creek Resources Corp. (TSXV:
MEK) (OTC Pink: MCREF) (FSE: M1C1) (the "Companies" or "Metals Creek") and Benton Resources
Inc. (TSXV: BEX) (the "Companies" or "Benton") are pleased to announce preliminary results of
anomalous concentrations of hydrogen and helium from the recently completed soil gas program (see
news release dated August 18, 2026). This program involved two regional soil gas programs at
Parson's Pond and Smoking Gun Hydrogen-Helium projects. Rudy Willick of Rudiger Re-Chem from
Neuanlage, Saskatchewan oversaw the execution and implementation of these programs.
This soil sampling program saw the collection of 710 samples over a period of approximately two weeks
and included the analysis for Hydrogen, Helium, Neon, CO2, and C1-C4 Hydrocarbons. Results include
the identification of four new highly prospective soil gas anomalies with two anomalies from each project.
Even though these results are early stage, the presence of these anomalies further validates the potential
of both projects to potentially host subsurface hydrogen and helium. Of note, several hydrogen sample
clusters point to a historic well (Finnegan Well) which encountered high pressure gas within the Parson's
Pond project.
Smoking Gun Project
The
Smoking Gun Project
is located in Western Newfoundland within the highly prospective Deer Lake
sedimentary basin. Deep sedimentary units within the Deer Lake Basin consist of shales, sandstones
and conglomerates. These units, particularly the sandstones, contain fragments of serpentine and
chrome. When these assemblages are paired together, they create an environment which is considered
essential for the creation of natural hydrogen, with the interaction of water (serpentinization). The Deer
Lake Basin contains several historic drill holes which have encountered high pressure gas. These holes
include the Mills No.1 drill hole in the Southwest portion of the property in addition to the Claybar No. 3
drill hole (see Figure 1) to the NE. Between these two holes is drill hole 79-67, which produced highly
elevated helium values from water sampling with results up to 8,900 parts per billion (ppb). Hole 79-67 is
located approximately 11.8 km from drill hole (Mills No. 1) which encountered high pressure gas that
flowed for a minimum of 12 months. Hole Claybar No. 3 located NE of drill hole 79-67 also produced
several intersections of high-pressure gas indicating a potential expansive system prospective for the
production of hydrogen and helium. Geological conditions for the generation and entrapment of hydrogen
are highly favorable with the presence of highly porous sandstone and conglomerates with associated
glauconite and ground water interaction. The close proximity to the Cabot Fault Zone provides deep
structural pathways required for hydrogen or helium generated either in the basement rock or the
sedimentary basin itself, to migrate upward into porous sandstones and conglomerates. The shales,
which overly the porous sandstone and conglomerate, act as a seal to the system, which is essential for
the entrapment of both hydrogen and helium. Active surface venting of gases and historic well logs
showing high methane levels, point to an energetic multi-gas system potentially capable of trapping
hydrogen and helium.
Ref:
https://gis.gov.nl.ca/mods/ModsCard.asp?NMINOString?temp=n&NMINOString=012H/03/Btm002
Soil Gas Results for Smoking Gun
Results from the recently completed soil gas program on the Smoking Gun property has identified two
highly prospective hydrogen and helium anomalies (see Figure 1) within the Deer Lake Basin. These
initial results delineate two broad anomalies, highlighting a potential robust active gas system with
hydrogen values up to 600 parts per million (ppm) and helium values up to 7.7ppm.
Highlights
:
Both hydrogen and helium soil gas anomalies
within highly favorable geological environment
are conducive for the generation and entrapment of gas. Values up to 600ppm hydrogen (H) and
7.7ppm helium (He) demonstrate the potential of the underexplored Deer Lake Basin.
Anomalous helium values at Smoking Gun
with many samples exhibiting a strong spatial
association with hydrogen, potentially suggests the possibility of a common source for both
hydrogen and helium.
Hydrogen concentrations above 100ppm at Smoking Gun
are interpreted to be significant
with values up to 600ppm being achieved.
An historical well (# DDH 79-67)
is locatedbetween the two soil gas anomalies, documented
helium at 8.9ppm. The location of the well aligns with the hydrogen and helium anomalies in this
area and may connect the soil gas anomalies on each side. Lineaments were also noted in the
area that are parallel to the trajectory of the soil gas anomalies and the well, which may suggest the
possible influence of a fault in the migration of the gases to the surface.
Multiple geological systems
capable of producing hydrogen and helium within the Deer Lake
Basin.
1
.
Serpentine & Chrome (Hydrogen): Ultramafic mineral fragments react directly with circulating
groundwater (serpentinization), while chromium acts as a solid-state catalyst to speed up
water-splitting and release hydrogen gas.
2
.
Glauconite (Hydrogen): An entirely separate, shallow sedimentary process, where iron-rich
marine clay alters via reverse weathering, producing redox reactions that generate hydrogen.
3
.
Radiogenic (Helium): Heavy radioactive elements (Uranium and Thorium) locked inside the
basin's sandstones and conglomerates constantly shed alpha particles, which capture
electrons to turn into stable Helium-4 gas.
4
.
Regional structures present serving as a pathway for the migration of H & He Gas.
5
.
Mudstones and shales overlying sandstones and conglomerates acting as a trap.
Figure 1: Smoking Gun Project Location Map
To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/943/313536_37010a8034025ac5_002full.jpg
Parson's Pond Property
The
Parson's Pond Property
, also located in Western Newfoundland, covers a large portion of a
prospective large sedimentary basin (Parson's Pond Basin) (see Figure 2).
This area is underlain by
thrust faulted rocks of the Humber Arm Supergroup. Drill logs indicate sedimentary units composed of
shales along with sandstones, containing fragments of glauconite. The presence of the mineral
glauconite, which, combined with these geological indicators and the presence of oxygen poor fluids or
ground water, suggests a highly prospective environment for the generation of white hydrogen (natural
hydrogen) within the basin. As in the case of the Deer Lake Basin, mudstones and shales are also
present within the Parson's Pond basin and are essential for the entrapement of both hydrogen and
helium. Gas in several historical drill logs located 14.2 km apart reported signifacant gas hits which
noted C1 methane gas levels reaching 72%. The presence of such high concentrations of methane
alongside hydrogen indicators suggests a potentially prospective active gas system within the basin. In
addition, surface areas have been noted to vent gas within the project boundaries, further indicating that
Parson's Pond is a part of an active gas system. With gas being reported in two historic holes 14.2 km
apart, suggests a potential expansive system prospective for the formation of gas potentially including
hydrogen.
(Ref. NALCOR ENERGY - OIL AND GAS INC FINAL WELL REPORT For Nalcor Energy et al SEAMUS #1
https://www.gov.nl.ca/em/files/publications-
energy-nalcorseamusfwr.pdf
and
NALCOR ENERGY - OIL AND GAS INC FINAL WELL REPORT For Nalcor Energy et al Finnegan #1
https://www.gov.nl.ca/em/files/FinniganFWR.pdf
).
Soil Gas Results for Parson's Pond
Results from the recently completed soil gas program has identified two significant hydrogen soil gas
anomalies within the central portion of the Parson's Pond property (see Figure 2). Highly anomalous
hydrogen values have been retutned with values up to 900 ppm, which is considered highly significant.
Highlights
:
Two hdrogen soil gas anomalies
with values up to 900ppm hydrogen. Max Power Mining
Corp.'s ("Max") Rider Project returned highly anomalous soil values upto 914ppm hydrogen (see
Max news release dated November 24, 2024). With results exceeding 900ppm, this current
program illustrates a potentially active migration of hydrogen from underlying source rock, which is
actively generating and moving gas.
Two highly anomalous hydrogen anomalies
from inaugual program with large portions of
project yet to be evaluated.
Parsons Pond area
revealed a higher overall concentration of hydrogen compared to the
Smoking Gun, but with lower helium concentrations overall.
Sampling in the Parson's Pond Lake
area was challenging due to wet and shallow bedrock
conditions, with only 20 samples able to be collected. A significant percentage of those samples
contained anomalous hydrogen concentrations. This is significant because of historical notes in
the region reporting gas emanating from the subsurface. It was noted that on the island in the lake,
gases were "bubbling" from the subsurface. No gas analysis was conducted at the time, but the
Rudiger Re-Chem soil gas survey highlighted a location on the island with hydrogen above
400ppm in the soils.
Sampling at Parson's Pond Central
area certain groupings of hydrogen anomalies that appear
to follow fault lines and different subsurface trends. The Central area also had the highest
concentrations of hydrogen out of the 4 areas of interest discussed. Hydrogen concentrations
exceeded 600ppm in several locations with the highest up to 900ppm.
Several hydrogen sample clusters
point to a historic well (Finnigan) which encountered high
pressure gas.
Hydrogen concentrations above 150ppm at Parson's Pond
are interpreted to be significant
with values up to 900ppm being achieved.
Parson's Basin Provides Highly Favorable
geological environment conducive for the
generation and entrapment of gas.
Management is highly encouraged with these initial results from both projects, with values up to
900pmm
hydrogen.
Even though these highly encouraging results are early stage, the near surface results
potentially indicate a direct pathway to a deeper source. This same model was performed by Max Power
Mining Corp., returning soil gas results up to 914ppm at surface. These results also ultimately proved
that hydrogen was also being produced within Max Power's projects. Historic holes on Max Power's
projects also had historic holes producing unexplained gas shows that, ultimately led them to refine their
model and successfully intercept hydrogen and helium in other locations. Parson's Pond and Smoking
Gun also have unexplained gas shows that are in close proximity to these highly prospective soil gas
anomalies. It is especially encouraging that one of these historic holes produced gas for in excess of 12
months (Mills No. 1) within the Deer Lake Basin. These highly promising soils appear to demonstrate
that both the Deer Lake and Parson's Pond Basins are productive for hydrogen and Smoking Gun is
also illustrating its potential for helium.
Large portions of both projects remain unsampled. Further exploration may be required to clarify if some
of these anomalous sources are connected, for example, the Parson's Pond lake anomaly may be joined
by a regional fault. There is potential to proceed to the North and South of Parson's Pond area to further
define potential soil gas sources. Further passive sampling for soil gas in these areas may be required
to further expand and delineate these potential zones within areas of swamp and bog.
Figure 2: Parson's Pond Project Location Map
To view an enhanced version of this graphic, please visit:
https://images.newsfilecorp.com/files/943/313536_37010a8034025ac5_003full.jpg
Survey Parameters
The geochemical survey program begins with the preparation of sample vials and replacing the septa in
the probes. The vials are evacuated to an absolute pressure of 20 pascals so that a sample extracted by
a syringe is not contaminated with residual ambient air. A cordless rotary drill is used to drive a hollow
probe of stainless steel to an average depth of about 1 meter to avoid barometric pumping which can
affect gas concentrations in soil. Once the probe is purged of ambient air, a 30cc sample is extracted
and injected through the septum of a 12cc vial. Other operations at the sampling site are the recording of
coordinates by GPS and recording of sample numbers on the box cover. To avoid hydrogen artefacts in
analysis, Rudiger Re-Chem utilizes a proprietary probe as well as detailed field notes for soil-gas
surveys. The samples are shipped to Rudiger Re-Chem's lab in Saskatoon for analysis by a state-of the
art Gas Chromatographs.
Hydrogen and Helium Demand
Hydrogen and helium have seen a significant increase in demand, with more expected in the future.
Hydrogen is used as a fuel and a chemical building block, it helps create fertilizer for food, refines the
gasoline in your car, and is increasingly being used to power clean trucks and ships as well as fuel for
rocket propulsion for the launching of satellites. Helium is the world's ultimate cooler; its super-cold
properties are essential for keeping MRI machines running and making the computer chips found in your
phone and laptop. AI-driven chip manufacturing is the primary growth engine for helium. Helium keeps
our most advanced technology and medical equipment functioning.
In the neighboring province of Nova Scotia, companies such as Quebec Innovative Metals Corp are
having success in the search for natural hydrogen. This success has generated further exploration in
similar geological environments to that of the projects mentioned above.
Please note that the presence of gas or methane on these staked projects or gas discovered on
adjacent properties does not guarantee the presence of hydrogen or helium. Further studies are
required to validate their presence.
About Metals Creek Resources Corp.
Metals Creek Resources Corp. is a junior exploration company incorporated under the laws of the
Province of Ontario, is a reporting issuer in Alberta, British Columbia and Ontario, and has its common
shares listed for trading on the Exchange under the symbol "MEK". Metals Creek has earned a 50%
interest in the Ogden Gold Property including the former Naybob Gold mine, located 6 km south of
Timmins, Ontario and has an 8 km strike length of the prolific Porcupine-Destor Fault (P-DF).
Additional information concerning the Company is contained in documents filed by the Company with
securities regulators, available under its profile at
www.sedarplus.ca
.
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.
Alexander (Sandy) Stares, President and CEO
709-424-1141
Metals Creek Resources Corp
MetalsCreek.com
Twitter.com/MetalsCreekRes
Facebook.com/MetalsCreek
To view the source version of this press release, please visit
https://www.newsfilecorp.com/release/313536