NRED Links Soil Samples with Airborne Resistivity to Refine Model
NRED LINKS 926 SOIL SAMPLES WITH AIRBORNE RESISTIVITY TO
REFINE WILMAC COVER MODEL
40 kHz DATA AND SOIL CLASSIFICATION STRENGTHEN PROPERTY-SCALE MAPPING OF
PRINCETON GROUP COVER AND NICOLA GROUP BASEMENT
Vancouver, British Columbia – August 25, 2026 – NRED Intelligent Mining Inc . (CSE: NRED) (OTCQB:
NREDF) ("NRED" or the "Company") is pleased to report results of an integrated review of shallow airborne
resistivity data and 926 classified soil samples from the Wilmac Copper-Gold Project (the "Project"),
located in British Columbia’s Quesnel porphyry belt, approximately 10 kilometres west of Hudbay Minerals
Inc.’s producing Copper Mountain Mine.
The review strengthens NRED’s working model suggesting that younger Princeton Group rocks may cover
and obscure the older Nicola Group and intrusive rocks considered more favourable for exploration. The 40
kilohertz ("40 kHz") airborne apparent -resistivity data identify a broad, more conductive eastern domain
interpreted to be influenced by Princeton Group cover, while the soil classifications provide much
shallower, local-scale information that helps refine the transition toward more resistive basement ground.
“This analysis provides us with a clearer picture of where prospective basement rock may be exposed and
where it may be hidden beneath younger cover,” said Brian Goss, Chief Executive Officer of NRED Intelligent
Mining Inc. “The airborne data provide the property -scale view, while the soils add local detail. Together,
they give us a stronger framework for mapping, follow-up, and future drill targeting.”
Key Results
• 926 soil samples were compared with the property-scale 40 kHz airborne resistivity dataset;
• A 211 ohm-metre empirical screening division, representing the 30th percentile of the property -scale 40
kHz data, was used to distinguish relatively conductive from relatively resistive responses;
• SED and QUAT soil groups returned median apparent resistivities of 288 and 311 ohm -metres
respectively, with approximately 33% and 27% of sites below the 211 ohm-metre screening division;
• The REG group, interpreted to retain a stronger Nicola -derived component, returned a higher median
apparent resistivity of 383 ohm-metres, with only 11% of sites below the screening division; and
• A detailed 2.5 by 1.8 -kilometre North Lamont comparison containing 96 classified soil samples shows
the expected broad relationship between cover -influenced soils, the conductive eastern domain , and the
transition toward more resistive ground.
40 kHz Data Define a Broad Cover-Screening Pattern
The 40 kHz data are part of the 2008 Fugro RESOLVE helicopter survey (Rockel 2009; Saleken 2009) and
principally reflect shallow electrical properties. Across the Project, lower apparent resistivity forms a
coherent eastern domain that broadly corresponds with younger Princeton Group cover, while more
resistive responses are more common over Nicola Group and intrusive ground to the west (Fig. 1).
For this review, 211 ohm -metres was selected as an empirical screening division. Values at or below this
level are relatively conductive and potentially cover -influenced; values above it are relatively resistive and
potentially more basement -influenced. Th e threshold is specific to the Wilmac dataset and is not a
universal geological cutoff or a direct definition of the unconformity.
The contrast is expected to be strongest where Princeton Group rocks are thick and conductive enough to
influence the airborne measurement. Thin, discontinuous, dry , or relatively resistive cover may produce a
basement-like response. Conversely, conductive Quaternary material, clay, groundwater or conductive
Nicola Group rocks may also produce low resistivity. The interpretation is therefore a cover -screening
model, not a direct geological map.
926 Soil Samples Add Shallow, Local-Scale Control
NRED’s 2025 review classified 926 soil samples into eight geochemical groups. Unlike the airborne system,
which averages a broader shallow volume, each soil sample records material at a specific near -surface
location. Lamont Ridge B-horizon soils were generally collected 15 to 30 centimetres below surface. This
means soil chemistry can preserve useful local information even where remaining Princeton Group cover is
too thin to dominate the airborne response.
The strongest relationship appears at the scale of broader soil groups and domains. SED and QUAT, which
show weaker local bedrock control, returned median 40 kHz apparent resistivities of 288 and 311 ohm -
metres, respectively. Approximately 33% of SED and 2 7% of QUAT sites occur below the 211 ohm -metre
screening division. In comparison, REG, interpreted to retain a stronger Nicola-derived component, returned
a median of 383 ohm-metres, with only 11% of sites below the division.
Other soil groups are consistent with the same broad framework. BVOL occurs farther inside the resistive
domain, while AVOL, CUVOL and PXGB cluster closer to the regional geophysical transition. The PRGP
classification remains provisional because its chemistry may reflect an organic-rich soil horizon rather than
Princeton Group provenance. The results support a broad cover -versus-basement framework but do not
make individual soil classes direct bedrock maps.
Figure 1 — Property-scale 40 kHz apparent resistivity. Blue areas are more resistive and red areas are more
conductive. Green outlines distinguish values at or above the empirical 211 ohm-metre screening division.
The outlines approximate the Nicola/Prince ton Group transition for screening purposes and do not define
geological boundaries.
North Lamont Example Shows the Relationship
A 2.5 by 1.8-kilometre North Lamont window was selected because both datasets have sufficient coverage
for a useful comparison. The window contains 96 classified soil samples. AVOL, CUVOL and PXGB, which
regionally cluster near the interpreted cover margin, follow the local resistivity transition, while SED and
QUAT extend into the more conductive eastern portion of the window.
Figure 2 — North Lamont comparison of the 40 kHz apparent-resistivity field and 96 classified soil samples.
SED and QUAT are grouped as cover- or transport-influenced; BVOL and REG as Nicola-associated; AVOL,
CUVOL and PXGB as cover -margin classes; and PRG P as an ambiguous organic -rich class. The window
illustrates the relationship where both datasets have useful coverage and is not presented as a blind
validation test.
Why the Datasets Do Not Match Point-for-Point
The airborne survey and soil sampling measure different physical volumes and operate at different spatial
resolutions. The 40 kHz system averages a broader shallow electrical response and requires sufficient
thickness and conductivity contrast to recognize cover. A soil sample represents a much smaller and
shallower location and may be affected by residual weathering, transported material, soil horizon and
drainage.
The resistivity data were interpolated to a 60 -metre grid from airborne survey lines, while soils were
collected along field traverses and roads rather than a continuous grid. Local mismatches are therefore
expected. The important result is the broader agreement in the position and character of the conductive
cover domain, the resistive basement domain and the transition between them.
Interpretation and Next Steps
NRED considers the combined interpretation partially supported. The data support the use of 40 kHz
apparent resistivity as a property -scale screen for areas where Princeton Group cover is sufficiently
developed to generate a conductive response, with soil clas sification providing complementary shallow
control. The data do not yet establish the exact unconformity position, cover thickness or bedrock identity
at every location.
The Company plans to test the model using pre -selected field transects across the interpreted transition,
incorporating geological mapping, shallow pits or auger holes, documented soil horizons and, where
practical, ground conductivity or resistivity measu rements. The 211 ohm -metre screening division will be
tested against field observations rather than adjusted to fit them.
The refined cover model will be used to condition other exploration datasets. Geochemical, radiometric or
magnetic responses occurring on interpreted Princeton Group ground will require geological evidence that
they are developed in, or sourced from, under lying Nicola Group or intrusive rocks before being advanced.
Neither the 40 kHz response nor any soil class identifies mineralization or predicts copper grade.
References
Rockel, E.R. (2009). Report on a Fugro Airborne Geophysical Survey, Tulameen Project, Assessment Report
31,585C, prepared for Goldcliff Resource Corporation by Interprex Resources Ltd., dated November 20,
2009, 60 p.
Saleken, L. (2009). Exploration Report on the Tulameen Project Property, Princeton Area, Similkameen
Mining Division, British Columbia, Assessment Report 30899 for Goldcliff Resource Corporation, dated
February 19, 2009, 254 p.
Qualified Person
The scientific and technical information in this news release, including the geological interpretations
described herein, has been reviewed and approved by Rick Walker, P.Geo., a Qualified Person as defined
by National Instrument 43 -101 ("NI 43 -101"). Mr. Walker is not independent of the Company within the
meaning of NI 43 -101. The interpretations described above are conceptual and rely in part on historical,
third-party data that the Company has not independently verified. No mineral resources or mineral reserves
have been identified on the Project.
About NRED Intelligent Mining Inc.
NRED Intelligent Mining Inc. (CSE: NRED) (OTCQB: NREDF) is a mineral exploration company focused on
the identification, acquisition, exploration and development of copper -gold porphyry projects in British
Columbia, leveraging an artificial intelligence-enhanced geospatial technology platform that it developed to
identify and evaluate prospective mineral properties. The Company’s optioned Wilmac copper-gold project
comprises 16,078 hectares located within the Quesnel porphyry belt in the Similkameen Mining Division,
southwest of Princeton and approximately 10 kilometres west of Hudbay Minerals Inc.’s producing Copper
Mountain Mine.
Readers are cautioned that the discussion of mineralization, alteration or grades on adjacent, similar or
analogous properties , including the Copper Mountain Mine , is not necessarily indicative of the
mineralization or potential of the Wilmac Copper-Gold Project. The Company has no interest in, or right to
acquire any interest in, any such properties.
ON BEHALF OF NRED INTELLIGENT MINING INC.
Brian Goss
Chief Executive Officer
FORWARD-LOOKING INFORMATION
This news release contains "forward-looking information" within the meaning of applicable Canadian securities legislation.
Forward-looking information includes, but is not limited to, statements regarding: the interpretation of geological,
geochemical and geophysical data , which were used to identify future exploration targets on the Wilmac Project; the
inference that the combination of airborne survey resistivity data and soil sample results, as interpreted, suggest that the
Wilmac Project may potentially host mineralized copper zones; the completion of additional analysis of past results and
the completion of anticipated exploration on the Wilmac Project in the future, including exploration to test the Company’s
revised property model ; and the Company’s intention and ability to satisfy the cash payment, share issuance , and
exploration expenditure milestones required to exercise the option agreements respecting the Wilmac Project.
Forward-looking information is based on a number of assumptions that, while considered reasonable by the Company at
the date of this news release, are inherently subject to significant business, economic and competitive uncertainties and
contingencies. Such assumptions include, without limitation: the accuracy of current geological interpretations, including
the identified anomalies and structural corridors described in this news release; the accuracy and completeness of the
third-party historical data on which the interpretation rests; the availability of adequate funding to complete the proposed
exploration; the ability of the Company’s geophysical contractors and geological consultants to complete contemplated
exploration on schedule; favourable weather, terrain and field conditions; access to the Project area; the availability of
qualified personnel; the receipt of all necessary permits and authorizations for planned exploration; and the continued
cooperation of the optionors under the terms of the relevant option agreements.
Forward-looking information is subject to known and unknown risks, uncertainties and other factors that may cause actual
results, performance or achievements to differ materially from those expressed or implied by such forward -looking
information. Important risk factors include, but are not limited to: the possibility that the interpretations described are
not ultimately accurate; additional exploration and drilling do not support the interpretation described; the continued
availability of capital and financing; the ability to satisfy option earn-in requirements on the timelines contemplated; risks
inherent in mineral exploration; adverse weather or terrain conditions ; tenure grant, renewal and permitting outcomes,
including under British Columbia’s revised mineral tenure system; Indigenous and community consultation requirements;
changes in applicable laws and regulations; the ability to retain key personnel and contr actors; litigation; failure of
counterparties to perform their contractual obligations; and general economic, market or business conditions. Readers
are cautioned not to place undue reliance on forward -looking information. The Company undertakes no obligat ion to
update or revise any forward-looking information, except as required by applicable securities laws.
Neither the CSE nor its Market Regulator (as that term is defined in CSE policies) accepts responsibility for the adequacy
or accuracy of this news release.