PLATEAU (YELLOW GIANT) HIGH GRADE GOLD DISCOVERY YUKON, CANADA 100% OWNED

January, 2016 1

1

On Track With Discovery

Goldstrike Resources Ltd. Flagship Plateau Gold Discovery Hess River, Yukon

PROPERTY OVERVIEW

2

PLATEAU GOLD DISCOVERY 













Independently confirmed new district scale gold system more than 25 kilometres long and 1,000 metres in vertical extent (Yellow Giant Trend) with tremendous untapped potential that remains open along strike and to depth. Rock grab samples up to 637.95 grams per tonne (18.66 ounces per ton); soil samples up to 26.82 grams per tonne. Gold is widespread in hydrothermal breccias, veins, stockworks, and disseminated in very strongly silicified and altered bedrock. Four major zones discovered to date include Goldstack (13.25 g/t Au over 17.5 m in core); Gold Dome (7.9 g/t Au over 9.03 m in core, up to 529.86 g/t (15.45 opt) Au in rock grab samples); Goldbank (up to 637.95 g/t (18.66 opt) Au in rock grab samples); Gold Rush zone (up to 26.82 g/t Au in soil, and 8.9 g/t Au in rock grab samples). These are original discoveries made by Goldstrike team in less than 15 weeks of cumulative field exploration. No record of any previous exploration on the property. Good access - four float-accessible lakes on and adjacent to property, and an airstrip 12 kilometres to south. 1,597 quartz mining claims covering approximately 352.5 square kilometres in the Mayo Mining District. All claims are located on Crown Land within the Traditional Territory of the Na Cho Nyak Dun First Nation, which has a settled land claim. Selected as one of only six projects to be showcased in the 2014 Media Tour sponsored by the Yukon Government. Written up by Northern Miner, Mining News North of 60, and Resource World in 2014. Yukoner Ron Stack received “Prospector of the Year” award for his discovery of the Goldbank zone. o e pert .

3

3

4

5

637.95

Sheared subvolcanic porphyry

Cretaceous intrusion

6

7

GOLDSTACK ZONE

8

GOLDSTACK ZONE • High grade gold was discovered in outcrop by prospector Tom Morgan in 2011, near the west end of the Yellow Giant Trend. The surface exposure consists of two mineralized outcrops 40 metres apart, with rock grab samples up to 49.1 grams per tonne (1.43 ounces) per tonne gold, and channel samples up to 14.25 grams per tonne gold over 2.4 metres. • Numerous grains of coarse native gold have been found in surface outcrop and downhole, and the gold is indicated to be free milling. This is evident both visually and petrographically, and suggests that a large proportion of the gold is likely amenable to gravity separation. • Discovery Hole PSGS13-04 intersected shallow gold mineralization grading 4.05 grams per tonne over 28 metres, including 10.91 grams per tonne gold over 10 metres, remains open. • Hole PSGS15-01 was drilled as a 30 metre stepout to the southeast. It intersected 13.25 grams per tonne gold over 17.25 metres true width, including 20.42 grams grams per tonne gold over 11.20 metres, including 35.28 grams per tonne (1.03 ounces per tonne) gold over 5.7 metres, and remains open (News Release September 9, 2015). PSGS15-02 is a vertical hole from the same setup that intersected 2.35 grams per tonne gold over 40.5 metres (38.1 metres true width), including 8.10 grams per tonne over 10.8 metres, and 18.09 grams per tonne over 4.00 metres, and remains open.

9

9

GOLDSTACK ZONE • Hole PSGS15-03 was drilled in a downdip direction to confirm the consistency and continuity of the gold mineralization. The hole averaged 1.78 grams per tonne gold over its entire 94.5 metre length and remains open. An upper high grade section averaged 11.26 grams per tonne gold over 8 metres. • Drilling in 2015 showed that the gold mineralized zone is consistent down dip and widens at depth. The drill intersections indicate that the top of the mineralized zone plunges southeast at 20 degrees. • The gold is associated with arsenopyrite in extensive sections of stockwork and hydrothermal breccia in the axial zone of a large southeast-plunging fold, along the leading edge of a steep northeast-directed thrust fault (the Goldstack Trend). This structure has been traced for 4 kilometres along strike, and other surface showings with similar mineralization and structure along this trend remain to be followed up.

10

10

PSGS15-03 – Visible Gold in Drill Core •

Best intersection 1.8 g/t Au over 94.5 m including 11.26 g/t Au over 8.0 m downhole width

PSGS15-01 – Visible Gold in Drill Core • Best intersection 13.25 g/t Au over 17.5 m including 35.28 g/t (1.03 oz/ton) Au over 5.7 m true width

PSGS-15-01 and PSGS-15-02 • 21 m (true width) of mineralized quartz stockwork and breccia containing visible gold PSGS-15-01 13.25 g/t Au over 17.5 m including 35.28 g/t (1.03 oz/ton) over 5.7 m TW •

Minimum 56 locations in PSGS-15-02 containing coarse visible gold (0.5-4 mm) over 15 m PSGS-15-02 2.0 g/t Au over 7 m including 5.5 g/t Au over 2.0 m TW

PSGS-15-03 • 77 m of quartz stockwork and breccia containing visible gold Assays as above

11

PSGS-15-01 13.25 g/t Au over 17.5 m incl. 5.28 g/t (1.03 oz/t) Au over 5.7 m true width

PSGS-15-01 13.25 g/t Au over 17.5 m incl. 5.28 g/t (1.03 oz/t) Au over 5.7 m True width

12

13

14

15

GOLDSTACK CORE PHOTOS

16

17

18

GOLD DOME

19

GOLD DOME • Seventeen kilometres east of Goldstack, numerous grab samples containing coarse visible gold assaying up to 529.86 grams per tonne (15.45 ounces per ton) gold have been found within a 9 square kilometre area along a broad, felsenmeer-covered ridge south of the Hess River. The gold is associated with extensive silica-albite alteration, quartz stockwork, and arsenopyrite, within a thick package of rhyolitic tuff and fine grained metasediments. • Eight exploratory holes with various azimuths and a dip of 45 degrees were drilled in 2015, to follow up Discovery Hole PSVG13-03 (7.6 grams per tonne gold over 9.03 metres – News Release 9 September, 2013) and other blind targets generated within a 450 by 450 metre area on Gold Dome. Seven of the eight holes intersected mineralized stockworks that remain open, and in addition, two of the holes (PSVG15-06 and PSVG15-08) contained multiple grains of coarse native gold (News Release July 21, 2015). • Hole PSVG15-06 was collared 63 metres south of Discovery Hole PSVG13-03 and was drilled to the north to test a blind, deep anomaly. It intersected four previously unknown gold mineralized zones downhole, including 9.09 grams per tonne gold over 1.5 metres near surface, and 12.65 grams per tonne gold over 0.5 metres within a 12.5 metre zone of mineralized stockwork and arsenopyrite at a downhole depth of 117 metres and remains open. The hole terminated in a previously untested area 30 metres north of Discovery Hole PSVG15-03, at a vertical depth of 93 metres below surface, and demonstrates strong upside potential for the discovery of additional new gold zones at depth within the largely unexplored 9 square kilometre Gold Dome area.

20

20

• Hole PSVG15-02 was collared 45 metres south-southeast of the Discovery Hole PSVG13-03 and drilled in a southwest direction that was previously unexplored. This hole intersected 3.48 grams per tonne gold over 2 metres at a downhole depth of 71.5 metres, including 6.45 grams per tonne gold over 1 metre, and remains open, again confirming the widespread distribution of gold on Gold Dome, both on surface and at depth, and demonstrating the strong potential for discovery of additional gold zones. Additional drilling is recommended in the next phase of exploration in order to trace the extent of the gold intersected in holes PSVG15-02, PSVG13-03, and PSVG15-06 that remain open. • Hole PSVG15-08 was collared 11 metres north of Discovery Hole PSVG13-03, and drilled in a downdip direction to test the continuity and consistency of the mineralization in Discovery Hole PSVG13-03. This hole intersected 18 metres of quartz stockwork with abundant arsenopyrite, and assayed 3.67 grams per tonne gold over 1 metre. It was drilled parallel to the southeast-plunging gold-mineralized structure, with an 11 metre offset, and intersected the halo around the main gold mineralization in the Discovery Hole (7.6 grams per tonne gold over 9.03 meters). Further drilling is required to delineate the full extent of the gold-mineralized structure confirmed in the Discovery Hole that remains open. • All Gold Dome exploratory drilling tested different targets at various azimuths as such the true widths of the gold mineralization intersected cannot be accurately estimated at this time. • Numerous shallow and deep targets on Gold Dome remain untested, including a large 800 by 100 metre soil anomaly that returned values up to 1,234.9 parts per billion (1.23 grams per tonne) gold, and are planned to be tested in the next phase of drilling.

21

21

PSVG-15-06 Visible Gold in Core • (9.09 g/t Au over 1.5 m • and 3.04 g/t over 0.4 m • and 12.7 g/t over 0.5 m)

PSVG-15-08 Drill Hole • 18 m of mineralized quartz stockwork • Including 3.7g/t Au over 1.0 m

PSVG-15-06 Deep Discovery Drill Hole 12.5 m of mineralized quartz stockwork (true width) containing visible gold at 117 m downhole, assays as above, remains open

22

DISCOVERY HOLE PSVG13-03 • Blind mineralization under felsenmeer 7.6 g/t Au over 9.0 m downhole width

23

Discovery Hole PSVG-13-03 7.6 g/t Au over 9.0 metres

24

25

DEEP DISCOVERY PSVG-15-06 9.1 g/t Au over 1.5 m at subcrop And 12.7 g/t Au over 0.5 m in another zone 117 m downhole

DISCOVERY HOLE PSVG-15-03 7.6 g/t Au over 9 m At subcrop surface

DISCOVERY HOLE PSVG-15-03 7.6 g/t Au over 9 m At subcrop surface

GOLD DOME DRILL SECTION SELECTED HOLES LOOKING NORTH DEEP DISCOVERY PSVG-15-06 9.1 g/t Au over 1.5 m at subcrop And 12.7 g/t Au over 0.5 m in another zone 117 m downhole

26

27

28

HIGH GRADE SAMPLES, VG ZONE (GOLD DOME)

SILICIFIED FELSIC VOLCANIC ROCK WITH VISIBLE WIRE GOLD AND ARSENOPYRITE. 280.06 GRAMS PER TONNE (8.18 OUNCES PER TON) GOLD FROM METALLICS ASSAY

SILICIFIED FELSIC VOLCANIC BRECCIA WITH ARSENOPYRITE. 529.86 GRAMS PER TON (15.45 OUNCES PER TON) GOLD FROM METALLICS ASSAY

Metallics assay 131.85 g/t (3.8 opt) Au

GOLD DOME/VG ZONE - QUARTZ STOCKWORK WITH VISIBLE GOLD IN SILICIFIED FELSIC VOLCANIC ROCK, ASSAYED 3.8 OUNCES PER TON GOLD

NATIVE GOLD IN DRILL CORE PSVG15-06 (12.7 G/T OVER 0.5 M)

29

30

31

GOLDBANK

32

GOLDBANK ZONE • Numerous grab samples containing visible gold or gold mineralization have been taken from bedrock in areas of stockwork and hydrothermal breccia along the 11 kilometre long Goldbank zone, and the zone remains open. • Eight new selected grab samples taken in 2015 contained visible gold, and returned 639.75 grams per tonne gold (18.66 ounces per ton), 287.71 grams per tonne gold (8.39 ounces per ton), 47.83 grams per tonne gold (1.40 ounces per ton), 35.91 grams per tonne gold (1.05 ounces per ton gold), 33.43 grams per tonne gold (0.98 ounces per ton gold), 16.74 grams per tonne gold, 11.50 grams per tonne gold, and 7.66 grams per tonne gold from metallics assays (News Release July 21, 2015). • On re-examination, several other samples that returned high gold assays in 2013 were also found to contain free native gold, which was previously unknown in the Goldbank area. These and many other strong gold targets identified in bedrock remain to be drill tested. • The discovery of free native gold on Goldbank is very significant, as it shows that the mineralogy of Gold Dome, Goldbank and Goldstack is the same, and demonstrates that all three zones are part of one district-scale gold system (the 25 kilometre Yellow Giant Trend). • Structures associated with high grade gold and arsenopyrite along the Goldbank and Ron Stack-Stack SW trends closely resemble gold-mineralized structures that have been intersected in Gold Dome and Goldstack drill holes.

33

33

Ron Stack

Goldbank E

Stack SW

Goldbank W

34

35

Ground magnetic intensity shows southeast plunging structure like Gold Dome and Goldstack, and gold concentrated in the magnetic low 36

HIGH GRADE GRAB SAMPLES, GOLDBANK ZONE

37

38

GOLD RUSH (PLATEAU NORTH PROPERTY)

39

On Track With Discovery

GOLD RUSH ZONE •

The Plateau North property (Gold Rush Zone) was initially staked as a Carlin target in metasediments, based on strong Au, Ag, Hg and Tl anomalies in silt (99 and 98 percentiles in a Yukon-wide dataset). Only three weeks of field exploration has been done on the property to date.

•

The property is underlain by clastic metasediments of the Lower Hyland Group (Proterozoic/Early Cambrian), including sandy and carbonaceous or calcareous shale, with 5% felsic metavolcanics, and minor limestone, felsic quartz-eye porphyry and basalt. The volcanics are rhyolitic tuffs with relict lapilli, crystals, and clasts up to 8 millimetres long, and contain up to 20% feldspar. The sediments are dominant, and the felsic volcanic package is ten times thinner than on the Plateau South property.

•

Goldstrike’s initial sampling recovered high grade gold in graphitic soil (26.82 grams per tonne gold) on the crest of a high glaciated ridge at 1700 metres elevation. The gold must have weathered in situ, because there is no possible downslope movement and no water at this location.

•

Further soil sampling returned highly anomalous soil along a strike length of 350 metres. The structure has been traced for 1,500 metres along strike and remains open. A total of 35 soil samples assayed over 100 parts per billion gold, including 11 samples that assayed over 1 gram per tonne gold.

40

On Track With Discovery | GSR TSX.V

On Track With Discovery •

A bedrock grab sample taken in the same area assayed 8.99 grams per tonne gold, and ten other bedrock grab samples assayed over 1 gram per tonne, including a chip sample that assayed 5.56 grams per tonne over 1 metre, and another with 1.89 grams per tonne over 0.5 metres.

•

Overturned fold and thrust structures resemble those that control gold mineralization on the Plateau South property, but folds appear to plunge to the southwest, indicating a different structural domain. This is thought to be due to rotation on the Hess River sole thrust. Soil geochemistry and ground magnetics show patterns that are consistent with macroscopic southwest-plunging folds.

•

Gold extends the entire length of the ridge down to the Hess River, over a strike length of more than 12 kilometres. It is believed to be part of the same very large gold system as Plateau South. Gold is inferred to have been transported northeast along a splay coming off the Hess River fault.

•

Strong silicification shown on an ASTER satellite image is inferred to be a thrust fault plane outcropping along the northwest side of the ridge. This implies that the gold mineralization was deposited in the deformed upper plate of the thrust, similar to what is seen at Gold Dome and at Goldstack.

41

On Track With Discovery | GSR TSX.V

Plateau North is Goldstrike’s original discovery in silty metasediments north of the river. Felsic volcanics have been mapped on the property, but are ten times thinner than on the Plateau South property. Mineralization appears to be controlled by a splay off the Hess River thrust fault, and appears to be part of the same very large gold system. Plateau North has had only 3 weeks of field exploration to date.

42

PLATEAU NORTH GOLD RUSH ZONE Gold mineralized structures north of the Hess River appear to plunge SW in contrast to SE plunging structures on the Plateau South property. This is, thought to be due to rotational movement on the Hess River thrust. The same style of overturned folding and thrusting has been documented on both properties.

43

Vertical gradient mag

44

45

Strong silicification on ridge crest, Plateau North property 46

Plateau North property - overturned folding and thrust faulting in felsic volcanics

47

Plateau North property: quartz-fuchsite-chlorite shear with arsenopyrite where thrust fault cuts through the ridge crest

48

49

This presentation does not constitute an offer to sell or a solicitation of an offer to buy any securities of the Company in any jurisdiction. Any such offer or solicitation will be made only in accordance with all applicable laws. The common shares of the Company will not be and have not been registered under the United States Securities Act of 1933, as amended, and may not be offered or sold in the United States, or to a U.S. person, absent registration or applicable exemption therefrom. The technical data in this presentation have been reviewed and approved by Trevor J. Bremner, P. Geo., who is a qualified person as defined in National Instrument 43-101. Mr. Bremner serves as Chief Geologist and Director. Information included in the presentation is updated to September 20, 2015. Although the company updates its presentations from time to time, investors should refer to the company's news releases, financial statements and Management Discussion and Analysis for current information. Neither TSX Venture Exchange nor its Regulation Services Provider (as that term is defined in the policies of the TSX Venture Exchange) accepts responsibility for the adequacy of accuracy of this presentation.

50

50

NI 43-101 DISCLOSURE Sample analysis and assaying for all of Goldstrike's projects have been conducted by Acme Analytical Laboratories Ltd in Vancouver, BC, which is ISO 9001 accredited. Soil samples are dried at 60C, and 100 grams is sieved to -80 mesh. A 15 gram sample split is then leached in aqua regia at 95 degrees C, and analyzed by a 36-element ICP package that includes semi-quantitative gold. Rock samples are crushed to 80% -10 mesh, and a 250 gram sample split is pulverized to 85% -200 mesh. 50 gram charges are then assayed for gold using fire assay fusion and ICP-ES finish with a lower detection limit of 2 ppb, and an upper detection limit of 10 ppm Au. In addition, 0.5 mg charges are digested by modified 1:1:1 aqua regia (HCl-HNO3-H20) and analyzed by 36-element ICP-MS that also includes semi-quantitative gold with a lower detection limit of 0.5 ppb Au and an upper detection limit of 100 ppm Au. Selected samples are subjected to 500 gram metallics fire assays, for which the plus fraction is finished gravimetrically and the minus fraction is finished with AA. Rigorous procedures are in place regarding sample collection, chain of custody and data entry. Certified assay standards, duplicate samples and blanks are routinely inserted into the sample stream to ensure integrity of the assay process. Note: Grab samples are selective by nature, and are unlikely to represent average grades on the property.

51

51

CAPITAL STRUCTURE AS OF SEPTEMBER 20, 2015 •

Cash $169,000, no debt;

•

97,819,636 shares issued and outstanding;

•

32,108,279 warrants issued and outstanding at an average price of $0.20/share;

•

7M of these warrants held by Petro One Energy at an average exercise price of $0.44/share;

•

10,390,000 options at an average exercise price of $0.19/share;

•

3 month average price $0.16, volume 324,174 shares per day with a total of 13,939,500 shares traded;

•

Traded on TSX Venture Exchange as GSR:TSXV.

52

52

•

Terry King, LL.B. - Chairman, President, CEO, and Director Terry King provides Goldstrike Resources with guidance and advice on all legal matters. He has more than 20 years of experience in corporate finance and securities matters. Mr. King is former Chairman of the B.C. Chapter Securities and Natural Resources Subsection (mining, oil, gas) of the Canadian Bar Association. He is also principal of Holmes and King, an association of law corporations.

•

Trevor Bremner, M.Sc., P. Geo. - Director and Chief Geologist Trevor Bremner is a consulting geologist with a wide range of Canadian experience in mineral exploration, petroleum, and government. In the mineral exploration industry he worked eight years on gold, nickel, and leadzinc projects in Nunavut, Northwest Territories and Ontario, including four seasons for Aurora Geosciences. He also worked eight seasons for Archer, Cathro and Associates on a variety of copper, lead-zinc, tungsten, and uranium exploration projects in the Yukon. Mr. Bremner also served the Government of Canada for 15 years in a variety of roles, including two years as Yukon's Chief Geologist, one year as Yukon's Acting Director of Mineral Resources, and three years as Head of Mining Legislation in Ottawa, and was instrumental in setting up the Yukon Geology Program (precursor to the Yukon Geological Survey), and helped to devolve mineral resource administration to the Yukon Government. As a member of the original syndicates that founded Goldstrike Resources Ltd. and Petro One Energy Corp., Mr. Bremner was part of the project generation team that led to the discovery of the new Plateau and Summit gold discoveries in Yukon, and the Milton Viking oil field in Saskatchewan. He is a registered Professional Geologist in Alberta, Saskatchewan, Manitoba, and Northwest Territories.

53

•

William S. Chornobay - Chief Operating Officer Bill Chornobay is responsible for managing the Company's exploration programs and related operations. Bill is a business man with over 20 years experience in negotiations, identifying and acquiring undervalued assets, corporate finance, corporate development, team building, and managing exploration programs in the Americas. He has held Board and Senior Management positions, and has been instrumental in raising over $100 million dollars (CDN) in the resource sector. Mr. Chornobay is a leader and company builder who has provided the overall corporate vision and building blocks that are required to grow successful companies. He has extensive experience in project generation, acquisition, and management of exploration projects in the Yukon. In the 1990s, Mr. Chornobay was the founder of the Yukon Prime Properties Syndicate, a group that included Terry King, LL.B., and Bart Jaworski, P. Geo. (now Senior Mining Analyst at Raymond James), and was set up to focus on northern properties that had potential for the discovery of world class gold deposits. The Prime Properties Syndicate specialized in project generation and identified a number of original gold prospects that were optioned to public companies, including the original Coffee Creek claim block that now forms the nucleus of the Kaminak Supremo zone gold discovery. The Coffee Creek property was originally optioned to Prospector International by the Syndicate, and Prospector obtained very encouraging results from initial geochemical grid soil surveys, but that was in 2000 and market conditions at the time made it difficult to fund gold exploration projects. Accordingly, the Coffee Creek claims were permitted to lapse, and remained dormant until the ground was later staked by Shawn Ryan and optioned to Kaminak. Bill Chornobay is a firm believer in the resource potential of the Yukon, and his practical approach and vision have a proven track record of success. 54

•

Dr. Lawrence (Larry) Dick, Ph.D., P. Geo. - Director Dr. Larry Dick has over 35 years of mineral experience, and is an internationally recognized explorationist who has been credited with or played a key role in five major mineral discoveries in North and South America. He is very familiar with the Yukon, having spent more than ten years working throughout the Territory including the Carmacks gold camp and the Nisling Range, which both form part of what is now known as the White Gold District. Dr. Dick formerly held a variety of positions with Chevron Resources Company in the Americas including Exploration Manager, and led the exploration teams that discovered the Golden Bear deposit in British Columbia, and discovered and developed the Can Can gold-silver deposit in north-central Chile. He is a co-founder of General Minerals Corp. (now Sprott Resource Corp.) and has served for many years as its Executive Vice President and Independent Director, as well as directing its exploration activities. He also founded Copper 1 Inc., serving as its Chief Executive Officer and President, and subsequently co-founded and served as the President, CEO and Chairman of Evolving Gold Corp., before assuming his present role as Chief Geologist and Manager of Resources for Baron Global Financial Canada Ltd. Dr. Dick continues to serve on the Boards of a number of public companies, including Timmins Gold Corp., and is a Full and Fellow Councillor of the Geological Association of Canada Cordilleran Section, and a Full and Fellow Member of both the Society of Economic Geologists and the Geological Association of Canada. For his exploration successes in Chile, Dr. Dick was awarded the Chevron Chairman's Award, and the "Mente et Malleo" award at the Chilean Geological Congress for the most successful exploration team in Chile.

55



John A. Kuehne, M. Mgmt., CA, CPA (Illinois) – Director John A. Kuehne is a management consultant in the business of advising, assisting and investing in both startups and small public companies. Previously, he was Chief Financial Officer of Doman Industries Limited. He began his career in corporate finance and accounting, spending over 9 years with Deloitte in Edmonton and Chicago. Mr. Kuehne has been appointed as an additional independent director, and a member of the Audit Committee.



Lucy Zhang, MBA, CGA – Director and Chief Financial Officer Ms. Lucy Zhang is a member of the Certified General Accountant Association of British Columbia. She has an Honours BA from Suzhou University, China, and an MBA (Honors) from Royal Roads University. Ms. Zhang's recent experience has included controller positions in administration, accounting, and finance with publicly traded mining and exploration companies.



Reimar Koch – Director and Past President Mr. Koch is an entrepreneur with a proven history of building new ventures into successful businesses. As CEO of Cellular Direct, he took this cell phone company from inception to a multi-unit chain serving major corporate clients – e.g. Pacific Press, Ministry of Social Services – achieving annual sales in the millions.

56

•

Tom Morgan – Advisor to the Board Tom Morgan is a lifetime Yukon prospector with a proven track record of success resulting in many new discoveries. Throughout his years of experience, Mr. Morgan has developed a tremendous feel for Gold mineralization in the Yukon, whether placer or hard rock in origin. He won Yukon Prospector of The Year Award in 2004, and was an early pioneer who made a significant contribution in confirming the potential of the White Gold Camp. His property was subsequently acquired by Underworld, and today, this property forms part of what is the renowned Kinross White Gold Property. More recently, Mr. Morgan made the first gold discovery on Goldstrike's flagship Plateau property. His experience, reputation and long history of proven success in the Yukon has proved invaluable to Goldstrike’s exploration team.

57

CONTACT INFORMATION Investor Relations Services Provided By: Jeff Stuart King James Capital Corporation Vancouver, British Columbia Mobile: 604-805-0375 [email protected]

Non-Investor and Business Inquiries: Goldstrike Resources Ltd. 1300-1111 West Georgia Street Vancouver, British Columbia Tel: (604) 681 1820 Fax: (604) 681 1864 [email protected]

Corporate Website: www.goldstrikeresources.com

58

58