Otis Gold Corp. announced that it has drilled the following intercepts at its Kilgore Gold Project, Clark County, Idaho: 128.0 meters (m) of 1.79 grams per tonne gold (g/t Au) in hole 16 OKC-353; 27.5 m of 2.63 g/t Au and 80.8 m of 1.87 g/t Au in hole 16 OKC-354; 120.4 m of 1.18 g/t Au in hole 16 OKC-349; and 74.6 m of 1.01 g/t Au and 35.9 m of 1.12 g/t Au in hole 16 OKC-352. The 4 holes above, and 8 additional holes reported below, represent the final 12 holes of the 10,300 meter, 40-hole drill program completed in November 2016 at the Kilgore Gold Project. Analytical results for the 12 drill holes reported in this release, along with those for the initial 28 holes previously reported, confirm the presence of significant gold mineralization in the Aspen Formation sedimentary host rocks, the primary target of the 2016 drill program. A majority of these intercepts are of both higher grade and longer intervals than most of those encountered in prior drilling at Kilgore and thus demonstrate a clear potential to increase the overall size and grade of the Kilgore Deposit. 2016 Kilgore Drill Program Highlights includes: highlights from the drill program and of importance to the future development of the Kilgore Deposit include: 1) Twenty-five of the 40 holes drilled in 2016 encountered mineralization in the newly-emerging Aspen Formation host. 2) An additional 11 holes encountered mineralization in Tertiary lithic tuff and dikes, the primary host of gold mineralization within the existing deposit. 3) In total, 36 of the 40 holes drilled in 2016 intersected reportable gold mineralization, representing a drill success rate of 90%. 4) A complete Table of 2016 drill results can be found on the Otis website. 5) Results of Otis' 2016 drill campaign continue to support the premise that gold mineralization in the Aspen Formation is more extensive than indicated by previous drill testing and appears to lie along a northwesterly-trending belt or corridor in the northern half of the deposit, much of which remains open for further drilling. 6) Results of drill holes targeting the basement Aspen Formation sedimentary host rocks continue to reveal the presence of significant open-ended mineralization that is typically higher-grade and displays thicker mineralized intercepts than those comprising the current bulk of the deposit in the overlying volcanic host rocks. 7) Reported intercepts in basement Aspen Formation sedimentary rocks demonstrate that mineralization exists to depths of up to 300-meters below the surface of the deposit, with some still open at depth. 8) The Tertiary intrusive sill (Tct), which directly overlies the Aspen Formation and locally intrudes the upper portion of it, has been proven to host significant mineralization and the extensive contact between the two rock types is an important locus for additional mineralization in the basement. Significant intercepts can and do exist in both the Aspen Formation and the Tct, and in many cases straddle the contact between them to occur continuously throughout both units. 9) Some intercepts drilled in Aspen Formation rocks along the mineralized northwest-trending corridor contain coarse-grained visible gold indicative of potential bonanza grades at depth. Immediate next steps at the Kilgore Gold Project include: a. Production of an updated set of geologic cross-sections reflecting the 2016 drill results; b. Preparation of an updated NI 43-101 resource estimate; and c. Development of a 2017 drill program and completion of associated program permitting.