Goliath Resources Limited · TSXV:GOT

Goliath Resources — Investor Presentation (September 2019)

17 slides from Goliath Resources's investor presentation, Sep 3, 2019

  1. Slide 1: Lorne Creek

    Lorne Creek A Newly Discovered Au-Cu-Mo Monzonite Porphyry System near Terrace, BC TSX.V: GOT OTCQB: GOTRF FSE: B4IE September 3, 2019

  2. Slide 2: Disclaimer

    The content of information contained in this Presentation has not been approved by an authorised person within the meaning of the Financial Services and Markets Act 2000 (”FMSA”). Reliance upon this Presentation for the purpose of engaging in any investment activity may expose an individual to a sig

  3. Slide 3: Newly discovered Au-Cu-Mo monzonite porphyry system on Lucky Strike property

    • Newly discovered Au-Cu-Mo monzonite porphyry system on the 31,511 hectare Lucky Strike property located ~40 km north of Terrace, BC. • Property has logging road access and is less than 10 km to rail, power, and highway. • 2018 mapping outlined a 1,200m x 700m zone with alteration assemblages indic

  4. Slide 4: 1741 metres drilled over three holes from a single pad

    1741 metres were drilled over three holes from a single pad in August 2019. All holes contained widespread sulphides from surface to EOH and remains open. • LS-19-01: Drilled to 718m, Az: 0 (N), Dip: 70 • LS-19-02: Drilled to 501m, Az: 30 (NE) Dip: 70 • LS-19-03: Drilled to 522m, Az: 330 (NW) Dip: 7

  5. Slide 5: 62 bedrock grab samples taken in 2018

    62 Bedrock grab samples in 2018 were taken from the outcropping porphyry centre, stockworks, and veins at the Lorne Creek surface drainage. They have grades up to: • 2.95 g/t Au • 133 g/t Ag • 4.5% Cu • 0.34% Mo The outcropping porphyry centre contains gold-bearing chalcopyrite and molybdenite stock

  6. Slide 6: 2018 Bedrock Sample LC-18-Rep1

    2018 Bedrock Sample LC-18-Rep1 (~6” long) Taken From Surface of Lorne Creek’s Outcropping Porphyry Centre, Stockwork and Veining Sulphide Mineralization including Chalcopyrite, Molybdenite & Pyrite. The Molybdenite, Chalcopyrite and Pyrite Mineralization associated with Quartz Veining.

  7. Slide 7: LS-19-01 Core: Widely Disseminated Sulphides at Depth

    LS-19-01 Core ~470m assays pending; Widely Disseminated Sulphides at Depth

  8. Slide 8: Lorne Creek - Lithologies

    Lorne Creek - Lithologies Diorite containing widely disseminated sulphides, as well as irregular veinlets of pyrrhotite a pyrite with larger chalcopyrite-bearing sulphides in quartz veins. (LS-19-01 assays pending; 185.68m to 185.90m)

  9. Slide 9: Lorne Creek - Lithologies

    Lorne Creek - Lithologies Quartz Veining with Abundant Pyrite and Chalcopyrite (yellow) Sulphides. (LS-19-01 assays pending)

  10. Slide 10: Lorne Creek - Lithologies

    Lorne Creek - Lithologies Widely disseminated pyrrhotite and pyrite sulphides in plagioclase-biotite intermediate intrusive rock with crosscutting quartz vein containing chalcopyrite & molybdenite. (LS-19-01 assays pending; 463.15m to 463.3m)

  11. Slide 11: Lorne Creek - Lithologies

    Lorne Creek - Lithologies Heavily altered plagioclase porphyritic intermediate intrusive rock. Disseminated sulphides are pyrrhotite and minor pyrite. (LS-19-02 assays pending)

  12. Slide 12: Lorne Creek - Lithologies

    Lorne Creek - Lithologies Strongly silicified and brecciated intermediate intrusive rock with pyrite stringers and disseminated pyrite throughout. (LS-19-01 assays pending)

  13. Slide 13: Lorne Creek - Lithologies

    Lorne Creek - Lithologies Sedimentary rock hosting disseminated pyrrhotite (>20%) with veinlets of pyrrhotite and minor pyrite. (LS-19-01 assays pending; 242.85m to 243.10)

  14. Slide 14: August 2019 – Core Discussion Video

    August 2019 – Core Discussion Video Assays Are Pending Goliath YouTube Channel Link: https://youtu.be/9uXYiOE6odw

  15. Slide 15: How do porphyries form?

    How do porphyries form? • Magmas release fluid and gas at high pressures during magma crystallization. • Crystal growth and the associated change in volume create additional pressure in the system. • The carapace or ”rind” of the intrusion is fractured by high pressure H2O-CO2-H2S saline steam. • Go

  16. Slide 16: Schematic trace of drill holes LS-19-01, LS-19-02 & LS-19-03

    Schematic trace of drill holes: LS-19-01, LS-19-02 & LS-19-03 Diagrams for illustration purposes only. Modified after Sinclair, 2007

  17. Slide 17: Additional information on the Lucky Strike Property

    Additional information on the Lucky Strike Property and our Newly Discovered Large Au-Cu-Mo Porphyry System can be viewed on our website: https://goliathresourcesltd.com/projects/lucky-strike/ For additional information please Goliath Resources Limited contact: 25 Adelaide Street East, Suite 1614 To

Goliath Resources — Investor Presentation (September 2019) on 6ix