Our Flagship High Grade Skarn System

Cerro Grande Skarn Corridor

Anchored by a High-Grade Copper-Gold-Silver Discovery

The Cerro Grande Skarn is located in the northern portion of the Adelita concession. The 300 metre high-grade discovery zone hosts 5 layers of Cu-Au-Ag skarn, remaining open in all directions.

Open in All Directions

Mineralization remains open laterally and at depth, with strong potential along a 6 km skarn corridor (Cerro Potrero and Cerro Potrero South)

Open in All Directions

Mineralization remains open laterally and at depth, with strong potential along a 6 km skarn corridor (Cerro Potrero and Cerro Potrero South)

Porphyry Link at Depth

Feldspar porphyry dikes and quartz–chalcopyrite veining (Hole-10) suggest a deeper porphyry copper source feeding the skarn

Porphyry Link at Depth

Feldspar porphyry dikes and quartz–chalcopyrite veining (Hole-10) suggest a deeper porphyry copper source feeding the skarn

Expansion Potential

The Cerro Grande Central Outcrop is interpreted to extend both northwest and at depth to ~1.2 km strike

Expansion Potential

The Cerro Grande Central Outcrop is interpreted to extend both northwest and at depth to ~1.2 km strike

Strong Magnetic Signature

The magnetite-rich skarn horizon provides clear targets for ground magnetic surveys and step-out drilling

Strong Magnetic Signature

The magnetite-rich skarn horizon provides clear targets for ground magnetic surveys and step-out drilling

Principal Objective: Cerro Grande Skarn

Cerro Grande is the primary focus of the current exploration program, with the principal objective to grow the existing high-grade, near-surface skarn discovery through targeted step-out drilling, delineating a resource.

Cerro Grande is the primary focus of the current exploration program, with the principal objective to grow the existing high-grade, near-surface skarn discovery through targeted step-out drilling, delineating a resource.

  • Stacked skarn horizons confirmed: Drilling supports a multi-horizon, vertically extensive skarn system, with mineralization open along strike and at depth.

  • Stacked skarn horizons confirmed: Drilling supports a multi-horizon, vertically extensive skarn system, with mineralization open along strike and at depth.

  • Strong inaugural results: Multiple mineralized intervals were intersected, including 14.8 m @ 1.4% Cu, 0.5 g/t Au & 20.0 g/t Ag (from 227.3 m).

  • Strong inaugural results: Multiple mineralized intervals were intersected, including 14.8 m @ 1.4% Cu, 0.5 g/t Au & 20.0 g/t Ag (from 227.3 m).

  • New mineralization below historic drilling: Step-out/deeper drilling intersected additional skarn horizons below prior drilling, materially expanding the interpreted scale potential

  • New mineralization below historic drilling: Step-out/deeper drilling intersected additional skarn horizons below prior drilling, materially expanding the interpreted scale potential

  • High-grade depth intercepts: Deeper intervals include 9.6 m @ 1.4% Cu, 0.4 g/t Au & 41.8 g/t Ag (from 339.1 m) and 7.8 m @ 1.3% Cu, 0.4 g/t Au & 48.6 g/t Ag, including 1.9 m @ 4.1% Cu (from 393.2 m).

  • High-grade depth intercepts: Deeper intervals include 9.6 m @ 1.4% Cu, 0.4 g/t Au & 41.8 g/t Ag (from 339.1 m) and 7.8 m @ 1.3% Cu, 0.4 g/t Au & 48.6 g/t Ag, including 1.9 m @ 4.1% Cu (from 393.2 m).

Vertically stacked skarn corridor with scale potential and plenty of room to grow.

Vertically stacked skarn corridor with scale potential and plenty of room to grow.

Cerro Grande sits within a structurally active intrusive–carbonate corridor that is highly prospective for copper–gold–silver skarn mineralization.

Inaugural drilling supports a multi-horizon, vertically extensive skarn system, with new skarn horizons identified below historic drilling and mineralization remaining open along strike and at depth. This provides a strong foundation for continued step-out and deeper drilling as we systematically expand the footprint and advance toward resource delineation.

Cerro Grande sits within a structurally active intrusive–carbonate corridor that is highly prospective for copper–gold–silver skarn mineralization.

Inaugural drilling supports a multi-horizon, vertically extensive skarn system, with new skarn horizons identified below historic drilling and mineralization remaining open along strike and at depth. This provides a strong foundation for continued step-out and deeper drilling as we systematically expand the footprint and advance toward resource delineation.

Description Of The Mineralised Skarn Horizons

Upper Skarn Section 1

Upper Skarn Section 1

Upper Skarn Section 1

The uppermost mineralized skarn was intersected between (227.26m – 242.05m), returning 14.79 m averaging 1.4% Cu, 0.5 g/t Au and 20 g/t Ag.

This section is characterized by a magnetite-rich skarn with brown and green garnet assemblages, hosting disseminated and vein-controlled chalcopyrite, bornite and chalcocite.

The thickness and grade of this section are consistent with the upper skarn zones encountered in historical drilling, confirming down-dip continuity.

The uppermost mineralized skarn was intersected between (227.26m – 242.05m), returning 14.79 m averaging 1.4% Cu, 0.5 g/t Au and 20 g/t Ag.

This section is characterized by a magnetite-rich skarn with brown and green garnet assemblages, hosting disseminated and vein-controlled chalcopyrite, bornite and chalcocite.

The thickness and grade of this section are consistent with the upper skarn zones encountered in historical drilling, confirming down-dip continuity.

Figure 1 - Skarn section 1 - Magnetite rich skarn

Figure 1 - Skarn section 1 - Magnetite rich skarn

Intermediate Skarn Horizon Section 2

Intermediate Skarn Horizon Section 2

Intermediate Skarn Horizon Section 2

A second mineralized interval was intersected between (323.00m-328.57m), grading 5.57m @ 0.4 % Cu, 0.2 g/t Au, 4.5 g/t Ag.

This section occurs proximal to intrusive contacts and displays skarn and skarnoid textures, with disseminated copper sulphides, and chrysocolla along fractures, the skarn presents fine grain green garnets and insignificant magnetite

A second mineralized interval was intersected between (323.00m-328.57m), grading 5.57m @ 0.4 % Cu, 0.2 g/t Au, 4.5 g/t Ag.

This section occurs proximal to intrusive contacts and displays skarn and skarnoid textures, with disseminated copper sulphides, and chrysocolla along fractures, the skarn presents fine grain green garnets and insignificant magnetite

Figure 2 - Skarn section 2 - Fine grain green garnet

Figure 2 - Skarn section 2 - Fine grain green garnet

Figure 2

Newly Discovered Lower Skarn Section 3 to 5

Newly Discovered Lower Skarn Section 3 to 5

Newly Discovered Lower Skarn Section 3 to 5

Three previously unknown mineralized skarn sections were intersected below 339 meters, representing a significant exploration breakthrough.

The first new horizon (339.10m – 348.65m), returned 9.55m @ 1.4% Cu, 0.4 g/t Au, 41.8 g/t Ag. This interval is characterized by fine grained green garnet skarn, with abundant magnetite and strong copper sulphide development, including chalcocite and chalcopyrite, locally accompanied by silver-rich sulphides

Three previously unknown mineralized skarn sections were intersected below 339 meters, representing a significant exploration breakthrough.

The first new horizon (339.10m – 348.65m), returned 9.55m @ 1.4% Cu, 0.4 g/t Au, 41.8 g/t Ag. This interval is characterized by fine grained green garnet skarn, with abundant magnetite and strong copper sulphide development, including chalcocite and chalcopyrite, locally accompanied by silver-rich sulphides

Figure 3 - Skarn section 3 - Fine grain green-garnet skarn with copper and abundance of magnetite

Figure 3 - Skarn section 3 - Fine grain green-garnet skarn with copper and abundance of magnetite

Figure 3

A second newly identified section (367.00 and 370.85m), returning 3.85m @ 1.1 % Cu, 0.5 g/t Au, 50.3 g/t Ag.

This interval comprises coarse grained garnet skarn with elevated silver values with copper sulphides and oxides disseminated and along fractures, suggesting a enhanced fluid flux or metal zonation at this structural level, with silver introduced or remobilized during a later fluid pulse rather than during peak skarn formation.

A second newly identified section (367.00 and 370.85m), returning 3.85m @ 1.1 % Cu, 0.5 g/t Au, 50.3 g/t Ag.

This interval comprises coarse grained garnet skarn with elevated silver values with copper sulphides and oxides disseminated and along fractures, suggesting a enhanced fluid flux or metal zonation at this structural level, with silver introduced or remobilized during a later fluid pulse rather than during peak skarn formation.

Figure 4 - Skarn section 4 - Green-garnet skarn with copper and silver sulphides (note the skarn front in the axis of the core sample)

Figure 4 - Skarn section 4 - Green-garnet skarn with copper and silver sulphides (note the skarn front in the axis of the core sample)

Figure 4

The deepest mineralized skarn horizon (393.17m-401m) returned, 7.83m @ 1.3% Cu, 0.4 g/t Au, 48.6 g/t Ag, including a high-grade intervale of 1.85 m @ 4.1 % Cu, 11 g/t Au and 150 g/t Ag.

This horizon exhibits strong copper-gold-silver enrichment associated with well-developed garnet skarn and sulphide assemblages, indicating a robust mineralizing system at depth 

The deepest mineralized skarn horizon (393.17m-401m) returned, 7.83m @ 1.3% Cu, 0.4 g/t Au, 48.6 g/t Ag, including a high-grade intervale of 1.85 m @ 4.1 % Cu, 11 g/t Au and 150 g/t Ag.

This horizon exhibits strong copper-gold-silver enrichment associated with well-developed garnet skarn and sulphide assemblages, indicating a robust mineralizing system at depth 

Figure 5 - Skarn section 5 - Green-garnet skarn with copper sulphides, disseminated and along fractures

Figure 5 - Skarn section 5 - Green-garnet skarn with copper sulphides, disseminated and along fractures

Figure 5

Figure 1

Figure 1

Algo Grande Drilling

Drill highlights from the Cerro Grande Skarn target (AG-GC_002 Skarn Intersects).*

Algo Grande Drilling

Drill highlights from the Cerro Grande Skarn target (AG-GC_002 Skarn Intersects).*


FROM (m)

TO (m)

INTERVAL (m)

COPPER %

GOLD (g/t)

SILVER (g/t)



Main

227.26

242.05

14.79

1.4

0.5

20,0

Horizon 1


Main

323.0

328.57

5.57

0.4

0.2

4.5

Horizon 2


Main

339.10

348.65

9.55

1.4

0.4

41.8

Horizon 3

Main

367.00

370.85

3.85

1.1

0.5

50.3

Horizon 4

Main

393.17

401.00

7.83

1.3

0.4

48.6

Horizon 5

includes

395.80

397.65

1.85

4.1

11

150




FROM (m)

TO (m)

INTERVAL (m)

COPPER %

GOLD (g/t)

SILVER (g/t)



Main

227.26

242.05

14.79

1.4

0.5

20,0

Horizon 1


Main

323.0

328.57

5.57

0.4

0.2

4.5

Horizon 2


Main

339.10

348.65

9.55

1.4

0.4

41.8

Horizon 3

Main

367.00

370.85

3.85

1.1

0.5

50.3

Horizon 4

Main

393.17

401.00

7.83

1.3

0.4

48.6

Horizon 5

includes

395.80

397.65

1.85

4.1

11

150



Cerro Grande Cross Section

Cerro Grande Cross Section

Open at Depth and Laterally

Testing the immediate Cerro Grande Skarn extensions with the aim to identify and grow the existing discovery.

Exploration Outlook

Building on the discovery of five stacked skarn horizons and the confirmation of high-grade continuity at depth, the next phase will target expansion of the mineralized envelope along the 6 km-long trend and vectoring toward a potential porphyry source.

Building on the discovery of five stacked skarn horizons and the confirmation of high-grade continuity at depth, the next phase will target expansion of the mineralized envelope along the 6 km-long trend and vectoring toward a potential porphyry source.

Integrated 3D System Modelling

Integrated the full historical dataset, discovered new skarn horizons, and will use new data to advance a scalable, district-scale porphyry-skarn system

Integrated 3D System Modelling

Integrated the full historical dataset, discovered new skarn horizons, and will use new data to advance a scalable, district-scale porphyry-skarn system

Integrated 3D System Modelling

Integrated the full historical dataset, discovered new skarn horizons, and will use new data to advance a scalable, district-scale porphyry-skarn system

Deeper & Step-Out Drilling

Systematic testing of the newly identified horizons within Cerro Grande and follow-up drilling on porphyry intercepts at depth.

Deeper & Step-Out Drilling

Systematic testing of the newly identified horizons within Cerro Grande and follow-up drilling on porphyry intercepts at depth.

Deeper & Step-Out Drilling

Systematic testing of the newly identified horizons within Cerro Grande and follow-up drilling on porphyry intercepts at depth.

Detailed Lidar and Magnetic Surveys

Detailed drone based surveys to trace skarn horizons along the 6 km corridor and fast-forward addition of drill-ready targets.

Detailed Lidar and Magnetic Surveys

Detailed drone based surveys to trace skarn horizons along the 6 km corridor and fast-forward addition of drill-ready targets.

Detailed Lidar and Magnetic Surveys

Detailed drone based surveys to trace skarn horizons along the 6 km corridor and fast-forward addition of drill-ready targets.

The cross-section illustrates the interpreted subsurface geometry of the Mezquital & Cerro Grande Porphyry Target at Adelita.

The cross-section illustrates the interpreted subsurface geometry of the Mezquital & Cerro Grande Porphyry Target at Adelita.

The cross-section illustrates the interpreted subsurface geometry of the Mezquital & Cerro Grande Porphyry Target at Adelita.

The cross-section illustrates the interpreted subsurface geometry of the Mezquital & Cerro Grande Porphyry Target at Adelita.

Drilling, surface mapping, and alteration patterns indicate a porphyry intrusion at depth, with a potassic core surrounded by phyllic and propylitic alteration and associated copper-bearing ore shells.

Drilling, surface mapping, and alteration patterns indicate a porphyry intrusion at depth, with a potassic core surrounded by phyllic and propylitic alteration and associated copper-bearing ore shells.

Drilling, surface mapping, and alteration patterns indicate a porphyry intrusion at depth, with a potassic core surrounded by phyllic and propylitic alteration and associated copper-bearing ore shells.

The Cerro Grande skarn at surface is interpreted as the upper expression of this system, while the model highlights strong potential for a large, continuous porphyry copper body extending below and adjacent to known mineralization

The Cerro Grande skarn at surface is interpreted as the upper expression of this system, while the model highlights strong potential for a large, continuous porphyry copper body extending below and adjacent to known mineralization

The Cerro Grande skarn at surface is interpreted as the upper expression of this system, while the model highlights strong potential for a large, continuous porphyry copper body extending below and adjacent to known mineralization

Unlocking a District-Scale Copper-Gold System

Five stacked skarn horizons confirmed, including three newly discovered. High-grade copper-gold-silver mineralization remains open in multiple directions.

Five stacked skarn horizons confirmed, including three newly discovered. High-grade copper-gold-silver mineralization remains open in multiple directions.

Our inaugural drill program has advanced Cerro Grande from a historical occurrence into a multi-horizon, stacked Cu-Au skarn system with porphyry affinity. The next phase is designed to aggressively expand the mineralized footprint and define the system architecture:

  • Vertical Extension: Systematic drilling above and below the newly identified horizons and follow-up on porphyry intersects.

  • Strike Extension: Step out drilling along the 6 km corridor, to demonstrate lateral continuity of newly identified system, advancing a district-scale structural framework.

Positioned as more than a single-zone discovery, Cerro Grande is being advanced as a scalable, multi-horizon copper-gold system: Built for systematic expansion along trend and at depth as we define the broader architecture and growth potential.

Our inaugural drill program has advanced Cerro Grande from a historical occurrence into a multi-horizon, stacked Cu-Au skarn system with porphyry affinity. The next phase is designed to aggressively expand the mineralized footprint and define the system architecture:

  • Vertical Extension: Systematic drilling above and below the newly identified horizons and follow-up on porphyry intersects.

  • Strike Extension: Step out drilling along the 6 km corridor, to demonstrate lateral continuity of newly identified system, advancing a district-scale structural framework.

Positioned as more than a single-zone discovery, Cerro Grande is being advanced as a scalable, multi-horizon copper-gold system: Built for systematic expansion along trend and at depth as we define the broader architecture and growth potential.

PART OF A BIGGER SYSTEM

PART OF A BIGGER SYSTEM

The Adelita Project

Current evidence indicates that Adelita hosts multiple mineral systems. Together, these systems point to a district-scale opportunity with the potential to support multiple deposits across the property.

Current evidence indicates that Adelita hosts multiple mineral systems. Together, these systems point to a district-scale opportunity with the potential to support multiple deposits across the property.

Explore the full Adelita Project

Explore the full Adelita Project

Dive into our interactive VRIFY model to explore all aspects of the Adelita Project

Dive into our interactive VRIFY model to explore all aspects of the Adelita Project

Get an overview of the project, learn more about the location, explore the interactive maps and dive deeper into the results.

Get an overview of the project, learn more about the location, explore the interactive maps and dive deeper into the results.

*43-101 Disclaimer References

The scientific and technical information contained in this website has been reviewed and approved by Mr. Lorne Warner, P. Geo., an independent Qualified Person for Algo Grande Copper Corp. as defined in NI 43-101.

Mr. Warner has examined information regarding the historical exploration at the Adelita copper project, which includes his review of the historical sampling, analytical and procedures and two site visits to verify drill collar locations and personally collect rock samples for analysis. Mr. Warner also completed a technical report on the Adelita Project prepared in accordance with NI 43-101 dated effective August 15, 2025, which is available under the Company’s profile at www.sedarplus.ca.

Management notes that historical results were collected and reported by operators unrelated to the Company but have been verified by its Qualified Person; as a result, the historical results create a scientific basis for ongoing work on the Adelita property. Management cautions that historical results, discoveries and any published resource estimates on adjacent or nearby mineral properties, whether in stated current resource estimates or historical resource estimates, are not necessarily indicative of the results that may be achieved on the Adelita property.

*43-101 Disclaimer References

The scientific and technical information contained in this website has been reviewed and approved by Mr. Lorne Warner, P. Geo., an independent Qualified Person for Algo Grande Copper Corp. as defined in NI 43-101.

Mr. Warner has examined information regarding the historical exploration at the Adelita copper project, which includes his review of the historical sampling, analytical and procedures and two site visits to verify drill collar locations and personally collect rock samples for analysis. Mr. Warner also completed a technical report on the Adelita Project prepared in accordance with NI 43-101 dated effective August 15, 2025, which is available under the Company’s profile at www.sedarplus.ca.

Management notes that historical results were collected and reported by operators unrelated to the Company but have been verified by its Qualified Person; as a result, the historical results create a scientific basis for ongoing work on the Adelita property. Management cautions that historical results, discoveries and any published resource estimates on adjacent or nearby mineral properties, whether in stated current resource estimates or historical resource estimates, are not necessarily indicative of the results that may be achieved on the Adelita property.