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September 22, 2016: Redstar Gold Corp. (TSX.V: RGC, US: RGCTF, FRA: RGG) ("Redstar" or the "Company") announces results from it's summer geological mapping program at the Empire Ridge Prospect ("Empire Ridge") which is part of the Company's 100% controlled Unga Gold Project, Alaska. The Company released results from work on the Shumagin Zone on September 15, 2016 and results from the other district targets, including Orange Mountain, are expected to be released shortly.

Empire Ridge Zone Exploration Highlights:

  • The exposed vein breccias at Empire Ridge are structurally, texturally and geochemically similar to breccias at Apollo and are the source of strongly anomalous gold-silver in talus and soils.
  • As a result of the 2016 summer field work, an ~750m long by ~250m deep panel, occurring from the surface to above sea level, remains open to exploration for oxidized gold-silver bearing quartz-adularia +/-carbonate +/- base metal vein breccias and is a significant shallow exploration target.
  • Select rock chip samples in 2014 from within the Apollo, Rising Sun and Empire Ridge areas returned high-grade gold and silver results with values up to 401 g/t Au and 266 g/t Ag.

Redstar President & CEO, Peter Ball, commented: "Detailed geological mapping during the summer at Empire Ridge has outlined the structural framework of exposures along strike of the historically-mined vein system at Apollo, where mining efforts from 1894 to 1906 produced ~500,000 tonnes at an average grade of ~10 g/t gold. The Company can now plan new diamond drill targets along the approximate 750m long by 250m deep panel along the Taurus Bench and Empire Ridge Zones that collectively, define the continuation of the Apollo vein system to the southwest of historic mine development stopes. This immediately presents a drill ready target, for a potential shallow, high-grade oxidized vein gold system."

Unga Gold Project: Apollo-Sitka Trend - Historical Overview

The Empire Ridge Prospect, located along the southeast portion of Unga Island, is part of the Apollo-Sitka trend, which is one of two, partially fault-controlled, northeast to southwest oriented semi-linear trends exhibiting near continuous hydrothermal alteration and associated gold-silver bearing vein prospects. The Apollo-Sitka trend and the parallel Shumagin trend transects the entirety of Unga Island and is over approximately 10 kilometres long (See Fig. 1).

2014 exploration work performed along the Apollo-Sitka trend by Redstar and reported in a press release dated December 11th, 2014, consisted of rock chip, soil and talus sampling along a approximately 3.5km long corridor of exposed hydrothermal alteration and sheeted veins that includes the sites of historic underground mining at Sitka and Apollo (circa. 1894 to 1906) (See Fig. 2). The veins are anastomosing,conjugate gold-silver bearing quartz-adularia +/-carbonate +/- base metal (Pb > Zn> Cpy ± Au + Ag)

Results from Redstar's surface work established a continuous gold and silver geochemical soil anomaly of >100ppb Au (up to 821 ppb Au) and >1.3g/t Ag (up to 21.5 g/t Ag) covering the Sitka and Apollo mine areas that extended past the limits of historic mining at the Apollo open stope by ~1.3km to the southwest through Empire Ridge to near the California Prospect (See Fig. 2). Select rock chip samples of exposures of quartz-adularia carbonate veins and stockwork taken from within the Apollo, Rising Sun and Empire Ridge areas returned high-grade gold and silver results with values up to 401g/t Au and 266g/t Ag (see Table 1 for highlighted samples taken during 2014).

Summer 2016 Results: Mapping and Drill Targeting

Detailed geological mapping completed during the summer, in combination with an evaluation of historic mine maps and drill results including 2014 surface geochemical data, has outlined the structural nature of the historically-mined vein system at Apollo and has allowed the Company to properly plan drill target areas with the potential to host a southwest extension of the Apollo vein system (See Fig. 2).

Volcanic units within the Apollo-Empire Ridge area consists of a northwest dipping stacked sequence dominated by feldspar ± pyroxene-phyric basalt-andesite flows and flow breccias; with lesser dacitic lithic/airfall tuffs interbedded with volcaniclastic and/or lacustrine/fluvial argillite, sandstone, conglomerate and lahars (See Fig. 3). A narrow (~175 m) horizon of lithic tuffs and lacustrine sediments exposed at Empire Ridge widens to the southwest along the Apollo Trend and is exposed for ~5.0km to the southwest towards the coast at Heather (See Fig. 1). This volcanic unit consists of silicic bodies, ribs and lithocaps of residual vuggy silica, haloed by patches of advanced argillic alteration identical to hypogene alteration observed at the Orange Mountain zone. The residual silica bodies and altered tuffs are "capped" by relatively unaltered competent basalt & andesite distal-to and stratigraphically above and below the more permeable altered tuff units (See Fig. 3).

The continuous ~750m long gold and silver geochemical talus-soil anomaly trends to the southwest from the Apollo open stope along the north side of the Taurus bench through Empire Ridge and is correlated to subdued subcrops of stockwork veined andesite and altered lithic tuff near Taurus to exposed residual silica bodies cut by quartz-limonite breccias and quartz-adularia ± carbonate breccias along Empire Ridge (See Fig. 2). The exposed vein breccias at Empire Ridge are structurally, texturally and geochemically similar to breccias at Apollo and are the source of strongly anomalous gold-silver in talus and soils. Previous dilling efforts by Alaska Apollo Mines Inc. (circa. 1983) targeted the vein system to the southwest of the Apollo open stope with 5 drill holes, 2 of which failed to reach targets due to poor drilling conditions (at Empire) and one drilled into the Apollo # 2 structure located west of the Apollo open stope. The other two drill holes intersected the Apollo vein system (one deep, one shallow) but returned poor gold-silver grades and elevated base-metal mineralization (galena-sphalerite-chalcopyrite) (See Figs. 2-4).

Oxidized quartz-adularia +/- carbonate +/- base metal veins and vein breccias exposed along the ribs of the Apollo open stope and along Empire Ridge document a complex structural framework that hindered expansion of the mining efforts to the southwest. Observed structural features at Apollo include: 1) conjugate sets of vertical to moderate-southeast dipping extensional veins localized within pre-existing structures along the east side of the main stope; 2) the occurance of dilation zones and associated breccia bodies localized about vein intersection lineations that have contrasting orientations (sub-horizontal & sub-vertical); 3) high-angle, post-mineral cross faulting at the extreme southwest end of the Apollo open stope that has offset the vein system (where extensions could not be located by historic drifts and cross cuts); and 4) the overall "northwest dip" of historic mine stopes is a result of mining along multiple vein sets, juxtaposed along side one another by vertical strike-slip and northwest dipping thrust faults with minor (<10m) top-to-the-east sense of displacment, that has resulted in an apparent northwest dip of historic mine development (See Figs. 2- 4).

Drilling of the vein system will require drill targets to be oriented to cross cut all vein generations and target zones of maximum dilation, centered about vein intersection lineations where gold-silver grades are likely to be enhanced (See Fig. 4). A steep, northwest target will be sufficient to test the multiple vein generations southwest of Apollo and may be supplemented by scissor holes until significant intersetions are discovered. As a result of the 2016 field work, an approximate 750m long by 250m deep panel, occurring from the surface to above sea level, remains open to exploration for oxidized gold-silver bearing quartz-adularia +/-carbonate +/- base metal vein breccias and is a significant shallow exploration target.

About The Unga Gold Project

The 100% controlled Unga Gold Project covers key strategic portions of adjacent Unga and Popof Islands, approximately 900 kilometers southwest of Anchorage, Alaska. Redstar controls a 240 square kilometer land package that is host to numerous structurally controlled, volcanic hosted intermediate-sulfidation epithermal high-grade vein, breccia, stockwork and disseminated gold-silver occurrences.

The Unga Project has excellent infrastructure, including direct daily flights from Anchorage, a deep-sea port and a temperate climate. The former Apollo-Sitka gold mine, located on the southern Apollo-Sitka Trend, was Alaska's first underground gold mine and the site of historic high-grade gold production.

Quality Control/Quality Assurance

The 2016 exploration program at the Unga Project includes a Quality Control/Quality Assurance (QA/QC) program, overseen by Jesse C. Grady, Redstar's Vice President of Exploration. All soil/talus/rock samples have been shipped to ALS Minerals for preparation and geochemical analysis.

Jesse C. Grady, MSc, CPG-11592, is a Qualified Person as defined by NI 43-101. Mr. Grady has prepared and approved the technical information contained within this release.

Redstar is a junior exploration company focused on high-grade gold exploration in North America. In Alaska, the Company is exploring the 100% controlled high-grade Unga Gold Project. In addition, Redstar recently sold its Nevada portfolio to NV Gold Corp. (TSXV: NVX), in return for two (2) board seats and 29.9% of NV Gold Corp. Redstar also owns 30% of the Newman Todd Gold Project, in Red Lake, Ontario, Canada.

On Behalf of the Board of Directors,

Peter A. Ball, President and CEO

For additional information please contact:

T: +1.604.245.5861
Toll Free: 877.310.3330
E: pball@redstargold.com

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 or accuracy of this release.

Forward-Looking Information This release includes certain statements that may be deemed "forward-looking statements". All statements in this release, other than statements of historical facts, that address events or developments that Redstar Gold Corporation (the "Company") expects to occur, are forward-looking statements. Forward-looking statements are statements that are not historical facts and are generally, but not always, identified by the words "expects", "plans", "anticipates", "believes", "intends", "estimates", "projects", "potential" and similar expressions, or that events or conditions "will", "would", "may", "could" or "should" occur. Although the Company believes the expectations expressed in such forward-looking statements are based on reasonable assumptions, such statements are not guarantees of future performance and actual results may differ materially from those in the forward-looking statements. Factors that could cause the actual results to differ materially from those in forward-looking statements include market prices, exploitation and exploration successes, and continued availability of capital and financing, and general economic, market or business conditions. Investors are cautioned that any such statements are not guarantees of future performance and actual results or developments may differ materially from those projected in the forward-looking statements. Forward-looking statements are based on the beliefs, estimates and opinions of the Company's management on the date the statements are made. Except as required by applicable securities laws, the Company undertakes no obligation to update these forward-looking statements in the event that management's beliefs, estimates or opinions, or other factors, should change.


Figure 1. Generalized geological map of the SE portion of Unga Island, Alaska.


Figure 2. Geological map of the ~Apollo-Empire Ridge area showing anomalous gold in soil geochemistry centered on zones of pervasive stockwork veining that trends from the southern most extent of the Apollo open stope through Empire Ridge.


Figure 3. Schematic Cross Section X-X' of Empire Ridge showing northwest-dipping volcanic stratigraphy and tuffaceous hosted residual silica bodies that are cut by fault offset quartz-vein breccias.


Figure 4. Detailed Plan Map and Annotated Picture of the Apollo open stope area. Note the geometry of fault/vein patterns that indicate early WNW extension prior to post-mineral extension. This is a common vein pattern observed across the Unga Gold Project including Shumagin, Aquila and Sitka areas.


Table 1. Selected rock chip samples taken from the Apollo-Sitka trend by Redstar during 2014.

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