REDEFINING EXPLORATION

January 2016

FORWARD LOOKING STATEMENT

This Presentation contains forward-looking statements that involve risks anduncertainties, which may cause actual results to differ materially from thestatements made. When used in this document, the words "may", "would","could", "will", "intend", "plan", "anticipate", "believe", "estimate", "expect" andsimilar expressions are intended to identify forward-looking statements. Suchstatements reflect our current views with respect to future events and are subjectto such risks and uncertainties. Many factors could cause actual results to differmaterially from the statements made, including those factors discussed in filingsmade by us with the Canadian or American securities regulatory authorities.Should one or more of these risks and uncertainties, such as results of currentexploration programs, the general risks associated with the mining industry, theprice of gold and other metals, currency and interest rate fluctuations, increasedcompetition and general economic and market factors, occur or shouldassumptions underlying the forward looking statements prove incorrect, actualresults may vary materially from those described herein as intended, planned,anticipated, or expected. We do not intend and do not assume any obligation toupdate these forward-looking statements. Potential shareholders are cautionednot to put undue reliance on such forward-looking statements.

COMPANY OVERVIEW

• Formed in 2015 by the previous founders of Tundra Copper Corp.o Tundra Copper Corp. was sold to Kaizen Discovery in Nov. 2014, 18 months after

its conception and for a significant return on investment to all shareholders

• Experienced management team of industry veterans with a proven track record of success and a strict focus on shareholder return

• Poised to take advantage of opportunities in current market conditions where mineral properties of incredible merit are available for acquisition

• Targeting gold and copper assets that meet a proven set of criteria to create substantial increases in shareholder value.

CORPORATE TEAMCorwin (Cor) Coe, B.Sc., P.Geo. Chairman, Director, CEO

President, Coelton Ventures Ltd., 25+ years experience as a Director and Officer of several public mining companies; B.Sc. in Earth Sciences from SFU; diploma in Mining Engineering Technology from BCIT.

Donald Penner, B.Sc., P.Geo. Director, PresidentPresident of DF Penner Geological Consulting Ltd., worked on grassroots to feasibility projects in North and South America, Africa and Europe since 1969; B.Sc. In Geological Sciences from University of British Columbia.

Dr. Henry (Rick) Sandri, Ph.D. DirectorPresident Vermillion Gold Inc.; Former President Duluth Metals Ltd.; Previously with Select Resources LLC, Inco Ltd., Burlington Northern Inc.; Graduate of Georgetown U., American U. & Colorado School of Mines.

Stephen Pearce, LL.B. Director, Legal CounselDirector and Officer of several resource-related companies, specializes in corporate finance and securities; Law degree from UBC; Honors degree in economics from York University.

Ryan Coe, B.Sc., M.B.A. DirectorPresident of Fox Exploration Ltd.; 20 years experience in mineral exploration; director and founder of several companies; B.Sc. from UVIC; MBA from UCW; expert in field operations and project management.

Scott Close, M.Sc., P.Geo. VP ExplorationPresident Ethos Geological, Inc.; Senior Technical Advisor and Exploration Manager roles throughout North America; M.Sc. Earth Sciences from SFU; specializes in resource evaluation and development.

ADVISORY BOARDJoseph (Joe) Piekenbrock, M.Sc. Advisor

35+ years of mining experience; past VP Exploration for NovaGold Resources Inc.; awarded Thayer Lindsley medal for discovery of DonlinCreek deposit; B.Sc. in Geology from the U. of Colorado; M.Sc. in Geology from the U. of Arizona.

Syd (Sipke) Visser, B.Sc., P.Geo. AdvisorPresident/Senior Geophysicist at SJ Geophysics Ltd.; 30+ years of international geophysical survey experience; Haileybury School of Mines graduate; B.Sc. in Geology & Geophysics from University of British Columbia.

PROGRESS TO DATEJanuary 2015: Sitka Gold Corp. formed.

March 2015: $250,000 of seed capital raised.

April 2015: Arctic Copper Corp. formed - a 100% owned subsidiary of Sitka.50,500 hectares (125,000 acres) of highly prospective copper property staked in Coppermine River, Nunavut (the Coppermine Project).

August 2015: Exploration Program completed at Coppermine Property. NEW DISCOVERY - Copper Leaf strataform copper showing.

December 2015: Additional financing (last at $0.15/unit) completed bringing total for 2015 to $400,000.Nevada Gold Property acquisition completed in prolific Carlin District.

ADOBE GOLD PROPERTY LOCATED IN THE PROLIFIC CARLIN DISTRICT

NEVADA PROJECT DETAILS

Adobe Gold Project

NEVADA GOLD DEPOSITS & DISTRICTSCarlin-type deposits >1-5M oz Au.Massive Carlin-Type Gold Districts: N. Carlin,Cortez >190 M oz Au.Open-pit and underground gold mines that cluster at structural intersections of oblique foldsets and collapse faults.Devonian host rocks “lower plate”.Consistent age of mineralization ~36-42 Ma.

ADOBE RANGE DISTRICTNewly Recognized NW Fold &Thrust belt thatintersects and deforms an older NE Fold & Thrust belt: Dome Structure.Lower plate window of Devonian host rocks.Widespread Carlin-type Alteration and pathfinder geochemistry.Simple Land Acquisition of BLM and Fee Landwith 3-4 private land owners.

THE ADOBE RANGE, NEVADAA New Carlin-Type District-Scale Target

The Adobe Range District: rare opportunity to consolidate an entire District Scale Carlin-Type goldtarget play without competition.

SITKA’S ADOBE PROJECT

• Major Gold Districts: Laramide Age Geological Domes and Collapse Faults• Primary ore body controlling structures: through-going NNW anticlines and oblique WNW

anticlines within Devonian host rocks (Blue).• NNW and WNW faults sympathetic to folding are critical ore fluid feeder structures.

• Structural and Temporal comparisons at the Adobe Range:• NNW Anticlines oblique deforming NE and WNW anticlines & NNW tear faults,• Devonian upper-host strata is exposed west of the immediate dome structure

North Carlin Trend (>150Moz)All three scales are equivalent

SITKA’S ADOBE PROJECT

Cortez District (>40Moz)

~5km~5km~5km

Devonian Limestones “Lower Plate Window”

Dome Structures At Fold Intersections

ADOBE, N. CARLIN, CORTEZ STRUCTURAL COMPARISON

Widespread Carlin-type AlterationAssemblages

• Jasperoid Development along fold limbs & crests

• Decalcification & Clay Alteration in Devonian Limestones

• Silicification & Hematitic alt. along Perm/Miss Unconformity and in Elko Formation Conglomerates

• Anomalous Arsenic

Carlin-type disseminated gold andgold-breccia targets:1. Along the crest of NW-trending

Anticline in favorable DevonianLPW host rocks at depth (estimate ~500m depth)

2. Largest deposits where NW fold intersect NE Folds & High-Angle NNW Tear Faults.

10KM LONG CENTRAL NW FOLD TREND (~10,000 Acres)

• The Adobe LPW consists of Upper Devonian transitional limestone that is exposed over alarge area a few miles southwest of Intercept’s main acquisition target area & dome structure

• Semi-massive detrital petroliferous limestone is variably inter-bedded with thinly laminated,argillaceous limestone and limey shale.

• These units are comparable and equivalent to the tops of the main gold host rocks at Carlin (Rodeo Creek Formation) and at Cortez (Horse Canyon Formation)

• Structural interpretations show these units occur at depth (<500m) beneath our targeted domestructure and wide spread alteration assemblages observed at surface.

Panoramic view of the Adobe Lower Plate Window

ADOBE LOWER PLATE WINDOW: Main Targeted Gold Host Stratigraphy

• Eocene Elko Formation is foldedabout the Major NW Anticline

• Age of folding is bracketed by an angular unconformity ~40.4 Ma

• Timing linked with age of all Carlin-type gold deposits 36-42 Ma

• Main Target: young, unhealed breccia related to the NW brittle folding within LPW stratigraphylocated at depth along the NW foldtrend within Dome Structure

South Dipping, pervasively alteredand Arsenic-rich Eocene Elko Formation

MIDDLE EOCENE ANGULAR UNCONFORMITY: Syn-Mineral Deformation

Oil shale, conglomerate, limestone and tuff of theElko Formation is folded “domed” indicatingactive local tectonism in the Middle EoceneHydrothermal activity & alteration assemblagesare concentrated along the NW fold axis trend and occupies all pre-existing structures andpervasively alters the Eocene Elko Fm.Silicification & Hematite/Limonite (+arsenic) areextensively developed in folded Eocene Elko Fm.on the SW flank of the project areaMultiple areas mapped as “cherts” are actuallyjasperoids localized along stratigraphic horizons,unconformities, near tear faults and fold limbsIntense, pervasive decalcification, hematite -limonite alteration and jasperoids (+arsenic) occur along the folded Permian/Mississippian angular unconformityOther: base metal occurrences and small mines arepresent in Mississippian and Upper Plate rocksand represent the only publically reportedmineralization in the area. This is analogous to thePequop Range prior to the discovery of Long Canyon.

ResistantJasperoid

Silicified, Hematitic Elko

Fm.

Jasperoid creates a ridge along the Perm/Miss unconformity for overtwo miles in the exploration target

area

EVIDENCE OF CARLIN-AGE STYLE, STRUCTURALLY CONTROLLED ALTERATION ASSEMBLAGES

Limited rock samples (n= 52) indicate Carlin-type pathfinders are anomalous in most altered rock types and structures where sampled at Adobe.

- Carlin-5 (As, Hg, Sb, Tl, S)

The highest Arsenic values occur within silicified and hematite altered conglomerates of the ElkoFormation and along the Perm/Miss Unconformity withinthe NW fold axis corridor

Deformed, silicified, brecciatedand argillically altered carbonatessampled within the Lower PlateWindow exhibit trace concentrations of Carlin-type pathfinder elements

RECONNAISSANCE GEOCHEMISTRY

NUNAVUT PROJECT DETAILS

COPPERMINE RIVER PROPERTY

COPPERMINE PROJECT

- 50,500 hectare (125,000 acre) land package 20 – 50 km from Kugluktuk, NU

- Massive, under-explored district with potential to host world class

strataform sediment-hosted and volcanic-hosted copper deposits

- High-grade samples in area run up to 70%+ Cu.

- Potential for Ni-Cu-PGE mineralization

- Northwest Passage recently proven as viable shipping route

- Good access, close to town with commercial air and sea support

- Adjacent to Kaizen Discovery’s active 2015 drilling program

- Mining friendly jurisdiction with native land claims fully settled

MAJOR COPPER DEPOSITS OF THE WORLDEXAMPLES OF VOLCANIC-HOSTED COPPER DEPOSITS

KEWEENAW PENINSULA – Michigan, USAo 387.5 Million Tons @ 2% Cu ( ~ 15.5 Billion Pounds of Copper)

MT. ISA PROVINCE – Queensland, Australiao 280.3 Million Tons @ 3.3% Cu( ~ 18.5 Billion Pounds of Copper)

EXAMPLES OF STRATIFORM SEDIMENT-HOSTED COPPER DEPOSITS

KAMOA MINE – Katanga, Democratic Republic of Congoo Over 739 Million Tons @ 2.67% Cu

(~ 43.5 billion pounds of Copper)

FORE-SUDETIC MONOCLINE – Polando 3 Billion Tons @ 2% Cu, 50g/t Ag

(~ 120 billion pounds of Copper, 5.0 billion ounces of Silver)*All values are approximate, derived from government records, historic estimates and public documents or estimated from historic data

COPPERMINE PROJECT

Arctic Copper Claims blocks in red = 50,500 hectares (125,000 acres)

NEW DISCOVERY: Copper Leaf Showing.Sediment Hosted Copper

Copper Leaf Showing.Sediment Hosted. Surface samples up to 13.45 % copper and 65 g/t silver. Mineralization traced for over 2 km.Malachite and Chalcocite mineralization.

Copper Leaf Showing

Plan Map: Gravity Geophysics Survey Line and Assays

Section A-A’ Showing Gravity Anomaly and Coincident Copper Leaf Discovery

COPPERMINE PROJECT

Arctic Copper Claims blocks in red = 50,500 hectares (125,000 acres)

WIN Copper Showing41.54% Cu (select grab)

COPPERMINE PROJECT

Sample of Massive Chalcocite and Malachite

(volcanic-hosted Cu)41.54% Cu at the WIN

Showing (sample R442005)

TIMELINE

April/May 2015: 1st Open-Round Financing; 15 cent flow-through & 10 cent private placement- raise $250K for exploration capital and acquisition of gold asset (DONE)

August/Sept 2015: Secure gold property of significant merit (DONE)

August/Sept. 2015: Conduct preliminary exploration work on Coppermine Property- will qualify property as vehicle for future IPO (DONE)

Winter-Spring 2015/16:

Early 2016: Additional financing round

Spring/Summer 2016:

Fall/Winter 2016/2017:

Drilling advancement of Coppermine Project and Gold Property

Technical reports (REPORT FOR COPPERMINE COMPLETED AHEAD OF SCHEDULE)

Preliminary exploration and advancement work on Gold property

SUMMARYThe goal at Sitka Gold Corp. is simple: search out exceptional exploration stage gold and copper properties, advance and leverage those properties in a way that will maximize shareholder value, and provide an exit strategy so shareholders can capitalize on the value created.

The group behind Sitka has a track record of accomplishing this with incredible results. Through the recent sale of Tundra Copper Corp., this team of professionals has shown that, even during some of the most challenging market conditions in recent memory, plenty of opportunity exists for those with the ability to search it out and execute in a manner that places shareholders first.

The current market conditions present a ripe opportunity to acquire exceptional mineral properties that might not be available in more normal circumstances. We have identified and acquired two exceptional mineral properties of merit representing the commodities of both gold and copper and plan to leverage the development of these properties for the benefit of all shareholders.

Sitka Gold Corp. – REDEFINING EXPLORATION.

SITKA GOLD CORP.1500-409 Granville StreetVancouver, BC, V6C 1T2

Website: www.sitkagoldcorp.comEmail: info@sitkagoldcorp.comOffice: 604-979-0509Toll Free: 1-844-979-0509