PRESENTATION
Norway's Largest Mineral Exploration Company
Total landholding in Norway: 4.092 sqkm
Teako Minerals
Targeting: VMS | Copper | Zinc |
- To build secure supply chains in Europe
January 30, 2026 | CSE: TMIN
CSE: TMIN
www.teakominerals.com
Disclaimer
Disclaimer: Teako Minerals Corp. is a publicly trading company on the Canadian Securities Exchange, or CSE, which is operated by CNSX Markets Inc. Neither the CSE nor its Market Regulator (as that term is defined in the Trading Rules and
policies of the CSE) accepts responsibility for the adequacy or accuracy of information delivered in this presentation. Information Only, No Offer or Solicitation, No Unauthorized Distribution. This presentation does not constitute an offer to sell or solicitation of an offer to buy any of the securities described herein. The sole purpose of this presentation in verbal, paper or electronic form is strictly for information. Forward Looking Statements: Certain statements and/or graphics in the Company’s press releases, web site information and corporate displays, among others, constitute “forward-looking statements”. These statements are based on information currently available to the Company
and the Company provides no assurance that actual results will meet management’s expectations. Forward-looking statements include estimates and statements that describe the Company’s future plans, objectives or goals, including words to the
effect that the Company or management expects a stated condition or result to occur. Forward-looking statements may be identified by terms such as “believes”, “anticipates”, “expects”, “estimates”, “may”, “could”, “would”, “will”, or “plan”, or their
conditional or future forms. Since forward-looking statements are based on assumptions and address future events and conditions, by their very nature they involve inherent risks and uncertainties. Actual results relating to, among other things,
results of exploration, project development, reclamation and capital costs of the Company’s mineral properties, and the Company’s financial condition and prospects, could differ materially from those currently anticipated in such statements for many
reasons such as: changes in general economic conditions and conditions in the financial markets; changes in demand and prices for minerals; litigation, legislative, environmental and other judicial, regulatory, political and competitive developments;
technological and operational difficulties encountered in connection with the activities of the Company; and other matters discussed in this presentation. This list is not exhaustive of the factors that may affect any of the Company’s forward-looking
statements. The Company does not undertake to update any forward-looking statement that may be made from time to time by the Company or on its behalf, except if required to do so by applicable securities laws. These and other factors should be
considered carefully, and recipients should not place undue reliance on the Company’s forward-looking statements. Forward Looking Statements and/or Information Related to Exploration: Relating to exploration, the identification of exploration targets and any implied future investigation of such targets on the basis of specific geological, geochemical and geophysical evidence or trends are future-looking and subject to a variety of
possible outcomes which may or may not include the discovery, or extension, or termination of mineralization. Further, areas around known mineralized intersections or surface showings may be marked by wording such as “open”, “untested”,
“possible extension” or “exploration potential” or by symbols such as “?”. Such wording or symbols should not be construed as a certainty that mineralization continues or that the character of mineralization (e.g. grade or thickness) will remain
consistent from a known and measured data point. The key risks related to exploration in general are that chances of identifying economical reserves are extremely small. Third-party Information: Certain statements and/or graphics may contain third-party historical data and other information that have not been verified by Teako Minerals Corp. and may not be accurate or complete, therefore the information should not be relied upon. Qualified Person (QP) StatementThe technical information in this presentation relating to Teako Mineral Corp’s Scandinavian projects has been prepared in accordance with Canadian regulatory requirements set out in National Instrument 43-101 (“NI 43-101”) and approved by Dr. Eric Roth, F.AusIMM, a non-executive Director and Qualified Person as defined by NI 43-101.
CSE: TMIN
www.teakominerals.com
The Team
Sven Gollan
CEO & Director
Mark Steeltoft
Freddie Duncalf
Eric Roth
Vic Fitch
Non Executive Director & QP
CFO
VP Corp Dev & Director
VP Exploration
Jerker Tuominen
Engebret Lønnum
Carla Bennett
Independent Director
Corporate Secretary
Independent Director
Business & Geological Advisors
Alf Broeng
Desiree Roerdink
Hege Tunstad
Geological Advisor
Project & Mine Planning Advisor
Business Advisor
Visit www.teakominerals.com for detailed biographies of our team members
CSE: TMIN
www.teakominerals.com
Corporate Strategy
The Overall Strategy
The Approach to the Strategy
To drive forth and be at the forefront of exploration in Norway To secure supply of critical minerals and metals for Europe To make a significant base metal discovery To search for alternative non-dilutive financing options and ways for cashflow To have all-year-round exploration programmes between the assets & work around the clock with a diversified team to have continuous progress and newsflow To use the latest innovative technology within exploration to maximize potential for discoveries. To work with and establish partnerships with likeminded corporations and local communities to drive the exploration value chain in Norway
Data driven exploration and leveraging historical and ongoing work by third-parties Fully focused on Norway as a jurisdiction Target metals; VMS Copper-Zinc as a primary target Ability to drill all-year-round
Exploration Strategy
Nationwide Project Hub (+50 projects) Transforming Project Hub into cash flow and upside Exposure to various commodities
Strategic partnerships for projects and business Mineral Network - collaboration between municipalities & exploration companies Business development avenues with the counties
Cashflow & Upside
Collaboration & Partnerships
CSE: TMIN
www.teakominerals.com
Cash Flow Vision
Teako has a vision to incorporate various revenue streams to support main projects and corporate objectives, aiming for less dilution through:An active Pursuit of Project Deals: Seeking transactions within Teako's extensive project hub to fund main projects. • Outright sales & free carried interests • Earn-in Agreements • Option Agreements • Royalties • Other Economic Interests Completed project hub deals referenced in table 1 Year-Round Operations: Leveraging in-house geologists for operational roles, either as part of project deals or independent initiatives. Third-Party Work Programs: Conducting external work programs when resources allow, generating additional revenue streams. Funding Opportunities: Exploring soft funding and strategic partnerships to further enhance financial flexibility.
Operator Agreements
Third Party Work
Economic Interests in projects
Cash Flow
Project Deals
Table 1: Project hub deals secured
CSE: TMIN
www.teakominerals.com
Write your title here
Write your title here
Share Structure
Share Structure
Options: 4.700.000
Outstanding Shares: 111.746.161
Warrants: 964.000
Fully Dilluted: 117.410.161
Allocation
Known Ownership by Location
CSE: TMIN
www.teakominerals.com
Write your title here
Write your title here
Top 4 Largest Shareholders & Management
76.094.168 ( 68.10% )
16.023.447 ( 14.34 % )
24.820.668 (22.31 % )
18.581.923 ( 16.62 % )
11.183.577 ( 10.01.% )
5.484.553( 4.91.% )
CSE: TMIN
www.teakominerals.com
Why Norway
First-mover advantage in a jurisdiction with extensive mining history, poised for a resurgence in the industry backed by excellent infrastructure The mineral exploration industry and Government are keen on reviving the mining and exploration sector which became dormant in the 1980s due to low commodity prices and the discovery of oil and gas Positive government support with various initiatives to strengthen the industry A rich history of mining copper, nickel, and cobalt with multiple major copper and REE mines are about to open/reopen Vast amounts of historical geological data are stored publicly in an open-source database at the Geological Survey of Norway (NGU) and the Directorate of Mineral Management (DMF) Access to 800,000 meters of drill core at the NGU Various innovation programs and critical metals initiatives in Norway and the European Union allow the opportunity for non-repayable financial support or grants Geological features comparable to those found in Eastern Canada and comparable mineral wealth Availability of diverse mineralization types. Untapped economic potential in mineral resources
Excerpt's from the Norwegian Governments Mineral Strategy 2023 Read the full strategy by clicking here
CSE: TMIN
www.teakominerals.com
The Project Hub
Overview & Strategy
Teako’s Project Hub, including the Løkken and Venna main projects, now consists of 58 projects covering a total area of 4,092 sq. km. 4 projects wherein Teako holds a 10% economic interest and 5 projects wherein Teako holds a 10% Free Carried Interest Realized through staking and acquisition of prospective for copper, cobalt, zinc, gold, platinum group elements (or “PGE”), uranium, antimony, molybdenum and rare-earth-elements The Project Hub secures prospective projects on a national scale to meet the Company’s ambitions of contributing to the European supply of critical metals and maximizing the first-mover advantage in Norway Serves as a potential catalyst to pursue non-dilutive financing options through project deals and retain upside - without compromising the integrity of our core projects or the shareholder structure Functions as a de-risking mechanism by providing flexibility in project development within the Company Core assets such as the Løkken-Venna district remain integral to the Company’s self-funded exploration programs going forward, whereas the Company aims to retain exposure to exploration success on non-core assets through securing deals with strong partners. These deals, if secured, are intended to potentially bring in capital and/or ongoing cash flow, retain upside exposure, and reduce overall risk, thereby strengthening Teako’s foundation
Figure 1: Overview over Strategic Project Hub including Løkken & Venna main projects
CSE: TMIN
www.teakominerals.com
The Løkken & Venna Projects
Overview
Two separate main VMS projects (Venna and Løkken) measuring in total 697 sq. km with majority of the projects 100% owned by Teako Løkken and Venna are located contigous to and surrounds Norway’s foremost historical past-producing copper mining district at Løkken, Trøndelag Province Løkken and Venna boast well-developed public road networks and covers all prospective bedrock for Løkken-type VMS mineralization in Sør-Trøndelag The yellow Løkken concessions, which include the Løkken mine itself and 5 targets, are 90% owned by Teako, with Capella Minerals holding a 10% interest. The Venna concessions extend a significant strike of similarly prospective stratigraphy to the northeast of Løkken with 3 high priority targets The primary target types at Løkken and Venna are high-grade copper-cobalt-zinc massive sulfide Løkken-type deposits The Løkken and Venna projects are located approximately 50km SW and 30km SE, respectively, of the regional administrative centre of Trondheim, Trøndelag Province, central Norway Work on the Venna and Løkken projects will focus on identifying and prioritizing drill targets containing the potential for discovering new Løkken-type VMS systems
Figure 1: Løkken & Venna exploration Claims
CSE: TMIN
10
www.teakominerals.com
The Løkken & Venna Projects
What are we looking for?
The former Løkken mine is a stratiform massive sulfide deposit characterized by its impressive dimensions – approximately 4 km in length, a maximum depth of 1 km, and an average thicknessof 60 meters The main Løkken deposit is the largest known Cyprus-type VMS deposit known. Historical production is estimated to have been 24MT @ 2.3% Cu + 1.9% Cu Its rich mineral composition predominantly consisted of chalcopyrite, sphalerite, pyrite, and pyrrhotite Massive sulfide deposits typically occur in clusters within the same favourable stratigraphy. When compared to other VMS districts globally, we should expect to see more 10+MT deposits discovered in the broader Løkken-Venna district The Løkken deposit was discovered from a subtle massive sulfide outcrop, which measured less than 1m in width. Other potential new discoveries in the Løkken-Venna district may also have subtle (or even non-existent) surface expressions
Note: Historic production values quoted for Løkken are from Grenne T, Ihlen PM, Vokes FM (1999) Scandinavian Caledonide metallogeny in a plate-tectonic perspective.
Mineral Deposita 34:422–471, TMIN has not performed sufficient work to verify the published data reported above, but the Company believes this information to be
considered reliable and relevant.
Figure 1: 3D model of the Løkken deposit & the massive sulfide discovery outcrop (<1 m width)
CSE: TMIN
11
www.teakominerals.com
The Løkken & Venna Projects
On the Hunt for The Next Løkken Deposit
The former Løkken VMS mining district is located 50 km SW of the regional administrative centre of Trondheim, Trøndelag, in an area with excellent infrastructure (including a nearby deep water port at Orkanger) The Løkken-Venna district lies within the Caledonian orogeny of Norway The Caledonian orogeny of Norway is interpreted to have extended from the productive VMS districts in NE Canada (Bathurst Mining Camp, New Brunswick; Buchans District, Newfoundland) and the Appalachian US to northern Norway Mineralization at Løkken is massive sulfide-type and hosted by a sequence of Ordovician-age metabasalts (mixed pillow and massive basalts) within an overturned ophiolite (ancient sea floor crust) sequence The main Løkken deposit is the largest known Cyprus-type VMS deposit known. Historical production is estimated to have been 24MT @ 2.3% Cu + 1.9% Cu. Recent studies confirm that cobalt is also associated with copper-zinc mineralization in the Løkken district
Note: Historic production values quoted for Løkken are from Grenne T, Ihlen PM, Vokes FM (1999) Scandinavian Caledonide metallogeny in a plate-tectonic perspective.
Mineral Deposita 34:422–471, TMIN has not performed sufficient work to verify the published data reported above, but the Company believes this information to be
considered reliable and relevant.
Figure 1: Location of the Løkken deposit in the caledonian orogeny (bottom) and mine-scale geology (top).
CSE: TMIN
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www.teakominerals.com
The Løkken & Venna Projects
On the Hunt for The Next Løkken Deposit
High-resolution airborne geophysics data from a surveycompleted in the Venna area by the Norwegian Geological Survey, released in early 2024 Similarities between the magnetic anomalies found in Løkken and Venna illustrate the possibility of a relationship or shared geological feature between the two properties and the historical Løkken mine The intensity and morphology of the magnetic signature is comparable and expected for areas with such similar mapped geology and provides a strong tool for targeting.
Figure 1. Magnetics data for Løkken and Venna over Teako's license areas - hot colours indicating magnetic highs, cooler colours indicating lows
CSE: TMIN
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www.teakominerals.com
The Løkken & Venna Projects
On the Hunt for The Next Løkken Deposit
The geology of these two regions is dominated by a package of basalts, gabbros, and metasedimentary units of varying types. The similarities in the geology confirm the potential for further mineralization similar to that identified at the Løkken mine. There is a strong correlation between lithology types and geological conditions observed at Løkken mine and on the Løkken and Venna properties. The host rocks at Løkken (basalts and gabbros) form part of a so-called ophiolite sequence, which is former Atlantic ocean floor crust that is now exposed on mainland Norway. There is a strong correlation between lithology types and geological conditions observed at the Løkken mine and on the Løkken and Venna properties. Iron formation enriched in graphite has been historically identified within the Mostadmarka Formation of the Venna project (ref: Gasser et al 2021). This may suggest it formed in anoxic or low oxygen environments, a condition some believe helpful in the formation of VMS style mineralisation.
Figure 1. Bedrock data for Løkken and Venna over Teako's license areas
CSE: TMIN
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www.teakominerals.com
The Venna VMS Project
On the Hunt for The Next Løkken Deposit
The Venna Project covers 292 km2 of prospective ground in the Norwegian Caledonides, within 30 km of Trondheim City Centre and boasts 3 high-priority targets within the broader Mostadmarka target area (yellow trend) Geology is similar to Løkken mining district with the formation within the Caledonian Orogeny. Venna hosts the historical Mostadmarka ironworks trend with a series of over 200 near surface workings, targeting hematite- and magnetite-rich Iron Formations, thought to have formed through the action of hydrothermal fluids at or below the sea floor Limited exploration for VMS Cu-Zn mineralization has been recorded in this district, rendering it one of the most exciting greenfields opportunities in the Norwegian Caledonides
Figure 1. Venna geological map with 1:50k overlap including targets within the Mostadmarka target area
CSE: TMIN
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www.teakominerals.com
The Venna VMS Project
On the Hunt for The Next Løkken Deposit
Teako have completed an initial geochemical assessment of the area to screen for potential of buried massive sulfide deposits The study targeted sampling of the iron formations present alongside the volcanic host rocks. Iron formations can form through the exhalation or replacive-action of hydrothermal fluids at or below the paleo-seafloor, marking them as potentially prospective marker horizons for VMS-style mineralization. The iron formations can therefore hold geochemical indications of Cu-Zn mineralization and indicate proximity to a hydrothermal vent source Iron formations are a key feature of the Løkken district and other global VMS districts including the historical Tverfjellet mine to the south of Venna and the Bathurst Mining Camp in Canada. In a typical VMS model, iron formations can be deposited on the same horizon as massive Cu-Zn sulfide mineralization. The pathfinder elements/ratios identified within the iron formations can be used to vector towards the vent zones, higher the concentrations of these elements the closer to the vent system.Studies of iron formations led to the discovery of the Bathurst 12 and 6 deposit (see inset map and district concept in Figure 1) Further high resolution sampling in addition to other high resolution surveys is expected to lead to refined drill target definition.
Figure 1. Venna project overview map including NGU magnetics and geological model
CSE: TMIN
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www.teakominerals.com
The Venna VMS Project
On the Hunt for The Next Løkken Deposit
Within the southern magnetic trend an electromagnetic conductor (2.2km strike) known as the Storslåtten target was found associated with outcropping pyrite mineralization and has a geochemical signature indicating a hydrothermal origin Literature indicates that graphitic schist is limited in the area, so the conductor at the Storslåtten target is currently interpreted as being more likely sulphide-related Within the northern (~10km strike length) ironworks trend two high-priority targets have currently been identified with compelling geochemical indications of prospectivity; Nævra and Heingruva The Nævra target indicates hydrothermal replacement which from literature is typically linked to higher metal grades The Heingruva target features indicates a pure hydrothermal vent origin
Figure 1. Map of the Mostadmarka target area showing select geochemical laboratory results and geophysical anomalies over high-priority targets
CSE: TMIN
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www.teakominerals.com
The Løkken VMS Project
On the Hunt for The Next Løkken Deposit
Potential of additional undiscovered deposits within the district along a broadly E-W-oriented mineralization trend. In winter 2025 Teako completed a drill program at Åmot (AM-25-001) and Høydal (HOY-25-001)(see Figure 1). The Løkken deposit outcrops on its eastern margin, whereas the western margin (yellow polygon in Figure 1) is interpreted to be truncated by a post-mineralization fault zone, which the Orkla River now occupies. The Orkla River lies at the current known western margin of the Løkken deposit (Astrup Shaft) and is interpreted by Capella Minerals to represent a broadly N-S-trending post-mineralization fault which has dissected the original Løkken VMS deposit. The potential exists for the discovery of displaced blocks of the original Løkken deposit on the western side of the Orkla River valley. Given the depth of mineralization at the nearby Astrup Shaft (approximately 900m vertically below the surface), the Company anticipates that any displaced blocks of mineralization at Løkken West would lie at similar depths to Astrup and, therefore, be beyond detection for the standard geophysical and geochemical techniques currently being applied at Løkken.
Figure 1. The Løkken Target Area
CSE: TMIN
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www.teakominerals.com
The Løkken VMS Project
On the Hunt for The Next Løkken Deposit
The Høydal Cu-Co-Zn target lies immediately to the East of the former Løkken mining operations and within the highly prospective Løkken-Høydal-Åmot corridor. The primary target at Høydal is a 3 km-long corridor containing Cu-Zn-rich VMS-style mineralization (see Figure 1), with approximately 1km of this corridor having been tested by historical core drilling. A total of 20,846m of core drilling (see Figure 2) is reported to have been completed at Høydal by Orkla Grube AB between 1910 and 1976 (Grammelvedt, 1986); future exploration is expected to focus on extending higher grade (+2% Cu and +2% Zn) zones. Geological work completed by predecessors has also identified a potential new corridor of mineralization located approximately 500m South of the primary Høydal trend. Høydal represents a priority target for further drill testing based on its favourable geology / known mineralization and its proximity to the former mineral processing facilities at the old Løkken mine.
Figure 2. Overview of Høydal Target Showing Ground Magnetics and Soil Geochemistry
Figure 1. Høydal Historical Drilling and Model of Historical Mineralization Envelope
Caveat: The 3D model shown in Figure 1 was generated using LeapfrogTM software using a copper cut-off grade of 1% and with the explicit purpose of understanding the geological context of the historic Høydal mineralization with respect to the newly defined surface geophysical and geochemical anomalies. The historic mineralization envelope does not constitute a mineral resource estimate, and the Company does not treat the historic mineralization as a current resource.
CSE: TMIN
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www.teakominerals.com
The Løkken VMS Project
On the Hunt for The Next Løkken Deposit
The Åmot Cu-Co-Zn target is located 5km East of the former Løkken mining operations. Åmot is hosted within stratigraphy considered favourable for the discovery of further Løkken-type massive sulfide (VMS) deposits. The primary target is a large (up to 2km in length) coincident electromagnetic (EM), ground magnetic, and geochemical anomaly, which together represent a highly favourable combination for a buried VMS deposit. The Åmot target is interpreted from geophysical data to lie approximately 150 m below the surface
Figure 1. Overview of Åmot Target Showing Ground Magnetics and Soil Geochemistry
CSE: TMIN
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www.teakominerals.com
The Løkken VMS Project
On the Hunt for The Next Løkken Deposit
The Dragset-Halsetasen target hosts the former Dragset open pit and underground mining operation located approximately 5km West of the former Løkken mine. High-grade Cu-Co-Zn mineralization at Dragset is interpreted from both geological and geophysical data to be hosted within a fold nose, with the southern mineralized limb of the fold zone interpreted to extend eastwards towards the Halsetasen sector (see Figure 1). Further work is recommended in this Dragset-Halsetasen target to determine high-grade resource potential.
Figure 1. Overview of the Dragset-Halsetasen Target Showing Ground Magnetics and Soil Geochemistry
CSE: TMIN
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www.teakominerals.com
The Løkken VMS Project
On the Hunt for The Next Løkken Deposit
The Fjellslett Cu-Co-Zn target lies on the western margin of the Løkken property It contains outcropping high-grade Cu-Co +/- Zn mineralization hosted within a broadly ENE-WSW-trending corridor as defined by both geology and ground magnetic survey data (see Figure 1). Additional exploration work, including ground-loop EM surveys and preliminary drilling, has been proposed by for the Fjellslett target area.
Figure 1. Overview of Fjellslett Target Showing Ground Magnetics
CSE: TMIN
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www.teakominerals.com
Teako Minerals Corp.
400-601 West Broadway, Vancouver, BC V5Z 4C2 +1 (604)-871-4301 Contact us: Sven Gollan, CEO
sven.gollan@teakominerals.com Mark Steeltoft, VP Corporate Development & IR
mark.steeltoft@teakominerals.com
CSE: TMIN
www.teakominerals.com
Teako Minerals January 30, 2026
Mark Steeltoft
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Transcript
PRESENTATION
Norway's Largest Mineral Exploration Company
Total landholding in Norway: 4.092 sqkm
Teako Minerals
Targeting: VMS | Copper | Zinc |
- To build secure supply chains in Europe
January 30, 2026 | CSE: TMIN
CSE: TMIN
www.teakominerals.com
Disclaimer
Disclaimer: Teako Minerals Corp. is a publicly trading company on the Canadian Securities Exchange, or CSE, which is operated by CNSX Markets Inc. Neither the CSE nor its Market Regulator (as that term is defined in the Trading Rules and policies of the CSE) accepts responsibility for the adequacy or accuracy of information delivered in this presentation. Information Only, No Offer or Solicitation, No Unauthorized Distribution. This presentation does not constitute an offer to sell or solicitation of an offer to buy any of the securities described herein. The sole purpose of this presentation in verbal, paper or electronic form is strictly for information. Forward Looking Statements: Certain statements and/or graphics in the Company’s press releases, web site information and corporate displays, among others, constitute “forward-looking statements”. These statements are based on information currently available to the Company and the Company provides no assurance that actual results will meet management’s expectations. Forward-looking statements include estimates and statements that describe the Company’s future plans, objectives or goals, including words to the effect that the Company or management expects a stated condition or result to occur. Forward-looking statements may be identified by terms such as “believes”, “anticipates”, “expects”, “estimates”, “may”, “could”, “would”, “will”, or “plan”, or their conditional or future forms. Since forward-looking statements are based on assumptions and address future events and conditions, by their very nature they involve inherent risks and uncertainties. Actual results relating to, among other things, results of exploration, project development, reclamation and capital costs of the Company’s mineral properties, and the Company’s financial condition and prospects, could differ materially from those currently anticipated in such statements for many reasons such as: changes in general economic conditions and conditions in the financial markets; changes in demand and prices for minerals; litigation, legislative, environmental and other judicial, regulatory, political and competitive developments; technological and operational difficulties encountered in connection with the activities of the Company; and other matters discussed in this presentation. This list is not exhaustive of the factors that may affect any of the Company’s forward-looking statements. The Company does not undertake to update any forward-looking statement that may be made from time to time by the Company or on its behalf, except if required to do so by applicable securities laws. These and other factors should be considered carefully, and recipients should not place undue reliance on the Company’s forward-looking statements. Forward Looking Statements and/or Information Related to Exploration: Relating to exploration, the identification of exploration targets and any implied future investigation of such targets on the basis of specific geological, geochemical and geophysical evidence or trends are future-looking and subject to a variety of possible outcomes which may or may not include the discovery, or extension, or termination of mineralization. Further, areas around known mineralized intersections or surface showings may be marked by wording such as “open”, “untested”, “possible extension” or “exploration potential” or by symbols such as “?”. Such wording or symbols should not be construed as a certainty that mineralization continues or that the character of mineralization (e.g. grade or thickness) will remain consistent from a known and measured data point. The key risks related to exploration in general are that chances of identifying economical reserves are extremely small. Third-party Information: Certain statements and/or graphics may contain third-party historical data and other information that have not been verified by Teako Minerals Corp. and may not be accurate or complete, therefore the information should not be relied upon. Qualified Person (QP) StatementThe technical information in this presentation relating to Teako Mineral Corp’s Scandinavian projects has been prepared in accordance with Canadian regulatory requirements set out in National Instrument 43-101 (“NI 43-101”) and approved by Dr. Eric Roth, F.AusIMM, a non-executive Director and Qualified Person as defined by NI 43-101.
CSE: TMIN
www.teakominerals.com
The Team
Sven Gollan
CEO & Director
Mark Steeltoft
Freddie Duncalf
Eric Roth
Vic Fitch
Non Executive Director & QP
CFO
VP Corp Dev & Director
VP Exploration
Jerker Tuominen
Engebret Lønnum
Carla Bennett
Independent Director
Corporate Secretary
Independent Director
Business & Geological Advisors
Alf Broeng
Desiree Roerdink
Hege Tunstad
Geological Advisor
Project & Mine Planning Advisor
Business Advisor
Visit www.teakominerals.com for detailed biographies of our team members
CSE: TMIN
www.teakominerals.com
Corporate Strategy
The Overall Strategy
The Approach to the Strategy
To drive forth and be at the forefront of exploration in Norway To secure supply of critical minerals and metals for Europe To make a significant base metal discovery To search for alternative non-dilutive financing options and ways for cashflow To have all-year-round exploration programmes between the assets & work around the clock with a diversified team to have continuous progress and newsflow To use the latest innovative technology within exploration to maximize potential for discoveries. To work with and establish partnerships with likeminded corporations and local communities to drive the exploration value chain in Norway
Data driven exploration and leveraging historical and ongoing work by third-parties Fully focused on Norway as a jurisdiction Target metals; VMS Copper-Zinc as a primary target Ability to drill all-year-round
Exploration Strategy
Nationwide Project Hub (+50 projects) Transforming Project Hub into cash flow and upside Exposure to various commodities
Strategic partnerships for projects and business Mineral Network - collaboration between municipalities & exploration companies Business development avenues with the counties
Cashflow & Upside
Collaboration & Partnerships
CSE: TMIN
www.teakominerals.com
Cash Flow Vision
Teako has a vision to incorporate various revenue streams to support main projects and corporate objectives, aiming for less dilution through:An active Pursuit of Project Deals: Seeking transactions within Teako's extensive project hub to fund main projects. • Outright sales & free carried interests • Earn-in Agreements • Option Agreements • Royalties • Other Economic Interests Completed project hub deals referenced in table 1 Year-Round Operations: Leveraging in-house geologists for operational roles, either as part of project deals or independent initiatives. Third-Party Work Programs: Conducting external work programs when resources allow, generating additional revenue streams. Funding Opportunities: Exploring soft funding and strategic partnerships to further enhance financial flexibility.
Operator Agreements
Third Party Work
Economic Interests in projects
Cash Flow
Project Deals
Table 1: Project hub deals secured
CSE: TMIN
www.teakominerals.com
Write your title here
Write your title here
Share Structure
Share Structure
Options: 4.700.000
Outstanding Shares: 111.746.161
Warrants: 964.000
Fully Dilluted: 117.410.161
Allocation
Known Ownership by Location
CSE: TMIN
www.teakominerals.com
Write your title here
Write your title here
Top 4 Largest Shareholders & Management
76.094.168 ( 68.10% )
16.023.447 ( 14.34 % )
24.820.668 (22.31 % )
18.581.923 ( 16.62 % )
11.183.577 ( 10.01.% )
5.484.553( 4.91.% )
CSE: TMIN
www.teakominerals.com
Why Norway
First-mover advantage in a jurisdiction with extensive mining history, poised for a resurgence in the industry backed by excellent infrastructure The mineral exploration industry and Government are keen on reviving the mining and exploration sector which became dormant in the 1980s due to low commodity prices and the discovery of oil and gas Positive government support with various initiatives to strengthen the industry A rich history of mining copper, nickel, and cobalt with multiple major copper and REE mines are about to open/reopen Vast amounts of historical geological data are stored publicly in an open-source database at the Geological Survey of Norway (NGU) and the Directorate of Mineral Management (DMF) Access to 800,000 meters of drill core at the NGU Various innovation programs and critical metals initiatives in Norway and the European Union allow the opportunity for non-repayable financial support or grants Geological features comparable to those found in Eastern Canada and comparable mineral wealth Availability of diverse mineralization types. Untapped economic potential in mineral resources
Excerpt's from the Norwegian Governments Mineral Strategy 2023 Read the full strategy by clicking here
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The Project Hub
Overview & Strategy
Teako’s Project Hub, including the Løkken and Venna main projects, now consists of 58 projects covering a total area of 4,092 sq. km. 4 projects wherein Teako holds a 10% economic interest and 5 projects wherein Teako holds a 10% Free Carried Interest Realized through staking and acquisition of prospective for copper, cobalt, zinc, gold, platinum group elements (or “PGE”), uranium, antimony, molybdenum and rare-earth-elements The Project Hub secures prospective projects on a national scale to meet the Company’s ambitions of contributing to the European supply of critical metals and maximizing the first-mover advantage in Norway Serves as a potential catalyst to pursue non-dilutive financing options through project deals and retain upside - without compromising the integrity of our core projects or the shareholder structure Functions as a de-risking mechanism by providing flexibility in project development within the Company Core assets such as the Løkken-Venna district remain integral to the Company’s self-funded exploration programs going forward, whereas the Company aims to retain exposure to exploration success on non-core assets through securing deals with strong partners. These deals, if secured, are intended to potentially bring in capital and/or ongoing cash flow, retain upside exposure, and reduce overall risk, thereby strengthening Teako’s foundation
Figure 1: Overview over Strategic Project Hub including Løkken & Venna main projects
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The Løkken & Venna Projects
Overview
Two separate main VMS projects (Venna and Løkken) measuring in total 697 sq. km with majority of the projects 100% owned by Teako Løkken and Venna are located contigous to and surrounds Norway’s foremost historical past-producing copper mining district at Løkken, Trøndelag Province Løkken and Venna boast well-developed public road networks and covers all prospective bedrock for Løkken-type VMS mineralization in Sør-Trøndelag The yellow Løkken concessions, which include the Løkken mine itself and 5 targets, are 90% owned by Teako, with Capella Minerals holding a 10% interest. The Venna concessions extend a significant strike of similarly prospective stratigraphy to the northeast of Løkken with 3 high priority targets The primary target types at Løkken and Venna are high-grade copper-cobalt-zinc massive sulfide Løkken-type deposits The Løkken and Venna projects are located approximately 50km SW and 30km SE, respectively, of the regional administrative centre of Trondheim, Trøndelag Province, central Norway Work on the Venna and Løkken projects will focus on identifying and prioritizing drill targets containing the potential for discovering new Løkken-type VMS systems
Figure 1: Løkken & Venna exploration Claims
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The Løkken & Venna Projects
What are we looking for?
The former Løkken mine is a stratiform massive sulfide deposit characterized by its impressive dimensions – approximately 4 km in length, a maximum depth of 1 km, and an average thicknessof 60 meters The main Løkken deposit is the largest known Cyprus-type VMS deposit known. Historical production is estimated to have been 24MT @ 2.3% Cu + 1.9% Cu Its rich mineral composition predominantly consisted of chalcopyrite, sphalerite, pyrite, and pyrrhotite Massive sulfide deposits typically occur in clusters within the same favourable stratigraphy. When compared to other VMS districts globally, we should expect to see more 10+MT deposits discovered in the broader Løkken-Venna district The Løkken deposit was discovered from a subtle massive sulfide outcrop, which measured less than 1m in width. Other potential new discoveries in the Løkken-Venna district may also have subtle (or even non-existent) surface expressions
Note: Historic production values quoted for Løkken are from Grenne T, Ihlen PM, Vokes FM (1999) Scandinavian Caledonide metallogeny in a plate-tectonic perspective. Mineral Deposita 34:422–471, TMIN has not performed sufficient work to verify the published data reported above, but the Company believes this information to be considered reliable and relevant.
Figure 1: 3D model of the Løkken deposit & the massive sulfide discovery outcrop (<1 m width)
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The Løkken & Venna Projects
On the Hunt for The Next Løkken Deposit
The former Løkken VMS mining district is located 50 km SW of the regional administrative centre of Trondheim, Trøndelag, in an area with excellent infrastructure (including a nearby deep water port at Orkanger) The Løkken-Venna district lies within the Caledonian orogeny of Norway The Caledonian orogeny of Norway is interpreted to have extended from the productive VMS districts in NE Canada (Bathurst Mining Camp, New Brunswick; Buchans District, Newfoundland) and the Appalachian US to northern Norway Mineralization at Løkken is massive sulfide-type and hosted by a sequence of Ordovician-age metabasalts (mixed pillow and massive basalts) within an overturned ophiolite (ancient sea floor crust) sequence The main Løkken deposit is the largest known Cyprus-type VMS deposit known. Historical production is estimated to have been 24MT @ 2.3% Cu + 1.9% Cu. Recent studies confirm that cobalt is also associated with copper-zinc mineralization in the Løkken district
Note: Historic production values quoted for Løkken are from Grenne T, Ihlen PM, Vokes FM (1999) Scandinavian Caledonide metallogeny in a plate-tectonic perspective. Mineral Deposita 34:422–471, TMIN has not performed sufficient work to verify the published data reported above, but the Company believes this information to be considered reliable and relevant.
Figure 1: Location of the Løkken deposit in the caledonian orogeny (bottom) and mine-scale geology (top).
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The Løkken & Venna Projects
On the Hunt for The Next Løkken Deposit
High-resolution airborne geophysics data from a surveycompleted in the Venna area by the Norwegian Geological Survey, released in early 2024 Similarities between the magnetic anomalies found in Løkken and Venna illustrate the possibility of a relationship or shared geological feature between the two properties and the historical Løkken mine The intensity and morphology of the magnetic signature is comparable and expected for areas with such similar mapped geology and provides a strong tool for targeting.
Figure 1. Magnetics data for Løkken and Venna over Teako's license areas - hot colours indicating magnetic highs, cooler colours indicating lows
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The Løkken & Venna Projects
On the Hunt for The Next Løkken Deposit
The geology of these two regions is dominated by a package of basalts, gabbros, and metasedimentary units of varying types. The similarities in the geology confirm the potential for further mineralization similar to that identified at the Løkken mine. There is a strong correlation between lithology types and geological conditions observed at Løkken mine and on the Løkken and Venna properties. The host rocks at Løkken (basalts and gabbros) form part of a so-called ophiolite sequence, which is former Atlantic ocean floor crust that is now exposed on mainland Norway. There is a strong correlation between lithology types and geological conditions observed at the Løkken mine and on the Løkken and Venna properties. Iron formation enriched in graphite has been historically identified within the Mostadmarka Formation of the Venna project (ref: Gasser et al 2021). This may suggest it formed in anoxic or low oxygen environments, a condition some believe helpful in the formation of VMS style mineralisation.
Figure 1. Bedrock data for Løkken and Venna over Teako's license areas
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The Venna VMS Project
On the Hunt for The Next Løkken Deposit
The Venna Project covers 292 km2 of prospective ground in the Norwegian Caledonides, within 30 km of Trondheim City Centre and boasts 3 high-priority targets within the broader Mostadmarka target area (yellow trend) Geology is similar to Løkken mining district with the formation within the Caledonian Orogeny. Venna hosts the historical Mostadmarka ironworks trend with a series of over 200 near surface workings, targeting hematite- and magnetite-rich Iron Formations, thought to have formed through the action of hydrothermal fluids at or below the sea floor Limited exploration for VMS Cu-Zn mineralization has been recorded in this district, rendering it one of the most exciting greenfields opportunities in the Norwegian Caledonides
Figure 1. Venna geological map with 1:50k overlap including targets within the Mostadmarka target area
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The Venna VMS Project
On the Hunt for The Next Løkken Deposit
Teako have completed an initial geochemical assessment of the area to screen for potential of buried massive sulfide deposits The study targeted sampling of the iron formations present alongside the volcanic host rocks. Iron formations can form through the exhalation or replacive-action of hydrothermal fluids at or below the paleo-seafloor, marking them as potentially prospective marker horizons for VMS-style mineralization. The iron formations can therefore hold geochemical indications of Cu-Zn mineralization and indicate proximity to a hydrothermal vent source Iron formations are a key feature of the Løkken district and other global VMS districts including the historical Tverfjellet mine to the south of Venna and the Bathurst Mining Camp in Canada. In a typical VMS model, iron formations can be deposited on the same horizon as massive Cu-Zn sulfide mineralization. The pathfinder elements/ratios identified within the iron formations can be used to vector towards the vent zones, higher the concentrations of these elements the closer to the vent system.Studies of iron formations led to the discovery of the Bathurst 12 and 6 deposit (see inset map and district concept in Figure 1) Further high resolution sampling in addition to other high resolution surveys is expected to lead to refined drill target definition.
Figure 1. Venna project overview map including NGU magnetics and geological model
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The Venna VMS Project
On the Hunt for The Next Løkken Deposit
Within the southern magnetic trend an electromagnetic conductor (2.2km strike) known as the Storslåtten target was found associated with outcropping pyrite mineralization and has a geochemical signature indicating a hydrothermal origin Literature indicates that graphitic schist is limited in the area, so the conductor at the Storslåtten target is currently interpreted as being more likely sulphide-related Within the northern (~10km strike length) ironworks trend two high-priority targets have currently been identified with compelling geochemical indications of prospectivity; Nævra and Heingruva The Nævra target indicates hydrothermal replacement which from literature is typically linked to higher metal grades The Heingruva target features indicates a pure hydrothermal vent origin
Figure 1. Map of the Mostadmarka target area showing select geochemical laboratory results and geophysical anomalies over high-priority targets
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The Løkken VMS Project
On the Hunt for The Next Løkken Deposit
Potential of additional undiscovered deposits within the district along a broadly E-W-oriented mineralization trend. In winter 2025 Teako completed a drill program at Åmot (AM-25-001) and Høydal (HOY-25-001)(see Figure 1). The Løkken deposit outcrops on its eastern margin, whereas the western margin (yellow polygon in Figure 1) is interpreted to be truncated by a post-mineralization fault zone, which the Orkla River now occupies. The Orkla River lies at the current known western margin of the Løkken deposit (Astrup Shaft) and is interpreted by Capella Minerals to represent a broadly N-S-trending post-mineralization fault which has dissected the original Løkken VMS deposit. The potential exists for the discovery of displaced blocks of the original Løkken deposit on the western side of the Orkla River valley. Given the depth of mineralization at the nearby Astrup Shaft (approximately 900m vertically below the surface), the Company anticipates that any displaced blocks of mineralization at Løkken West would lie at similar depths to Astrup and, therefore, be beyond detection for the standard geophysical and geochemical techniques currently being applied at Løkken.
Figure 1. The Løkken Target Area
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The Løkken VMS Project
On the Hunt for The Next Løkken Deposit
The Høydal Cu-Co-Zn target lies immediately to the East of the former Løkken mining operations and within the highly prospective Løkken-Høydal-Åmot corridor. The primary target at Høydal is a 3 km-long corridor containing Cu-Zn-rich VMS-style mineralization (see Figure 1), with approximately 1km of this corridor having been tested by historical core drilling. A total of 20,846m of core drilling (see Figure 2) is reported to have been completed at Høydal by Orkla Grube AB between 1910 and 1976 (Grammelvedt, 1986); future exploration is expected to focus on extending higher grade (+2% Cu and +2% Zn) zones. Geological work completed by predecessors has also identified a potential new corridor of mineralization located approximately 500m South of the primary Høydal trend. Høydal represents a priority target for further drill testing based on its favourable geology / known mineralization and its proximity to the former mineral processing facilities at the old Løkken mine.
Figure 2. Overview of Høydal Target Showing Ground Magnetics and Soil Geochemistry
Figure 1. Høydal Historical Drilling and Model of Historical Mineralization Envelope
Caveat: The 3D model shown in Figure 1 was generated using LeapfrogTM software using a copper cut-off grade of 1% and with the explicit purpose of understanding the geological context of the historic Høydal mineralization with respect to the newly defined surface geophysical and geochemical anomalies. The historic mineralization envelope does not constitute a mineral resource estimate, and the Company does not treat the historic mineralization as a current resource.
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The Løkken VMS Project
On the Hunt for The Next Løkken Deposit
The Åmot Cu-Co-Zn target is located 5km East of the former Løkken mining operations. Åmot is hosted within stratigraphy considered favourable for the discovery of further Løkken-type massive sulfide (VMS) deposits. The primary target is a large (up to 2km in length) coincident electromagnetic (EM), ground magnetic, and geochemical anomaly, which together represent a highly favourable combination for a buried VMS deposit. The Åmot target is interpreted from geophysical data to lie approximately 150 m below the surface
Figure 1. Overview of Åmot Target Showing Ground Magnetics and Soil Geochemistry
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The Løkken VMS Project
On the Hunt for The Next Løkken Deposit
The Dragset-Halsetasen target hosts the former Dragset open pit and underground mining operation located approximately 5km West of the former Løkken mine. High-grade Cu-Co-Zn mineralization at Dragset is interpreted from both geological and geophysical data to be hosted within a fold nose, with the southern mineralized limb of the fold zone interpreted to extend eastwards towards the Halsetasen sector (see Figure 1). Further work is recommended in this Dragset-Halsetasen target to determine high-grade resource potential.
Figure 1. Overview of the Dragset-Halsetasen Target Showing Ground Magnetics and Soil Geochemistry
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The Løkken VMS Project
On the Hunt for The Next Løkken Deposit
The Fjellslett Cu-Co-Zn target lies on the western margin of the Løkken property It contains outcropping high-grade Cu-Co +/- Zn mineralization hosted within a broadly ENE-WSW-trending corridor as defined by both geology and ground magnetic survey data (see Figure 1). Additional exploration work, including ground-loop EM surveys and preliminary drilling, has been proposed by for the Fjellslett target area.
Figure 1. Overview of Fjellslett Target Showing Ground Magnetics
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Teako Minerals Corp. 400-601 West Broadway, Vancouver, BC V5Z 4C2 +1 (604)-871-4301 Contact us: Sven Gollan, CEO sven.gollan@teakominerals.com Mark Steeltoft, VP Corporate Development & IR mark.steeltoft@teakominerals.com
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