Serengeti Resources Inc. announced the results of drilling completed on UDS property located four kilometers east of Centerra Gold's Kemess property in north-central British Columbia, approximately 250 kilometers north of Smithers, BC. Serengeti also provides an update on a geophysical survey completed on the Nub Mountain property located 30 kilometers north of Kemess within the Toodoggone region of BC. 2017 UDS Drill Program; Drilling at UDS in 2017 totaled 1,132 meters in three holes targeting zones identified by a 2016 Induced-Polarization (IP) survey and earlier property-wide geophysical and geochemical surveys. All three drill holes intersected variably altered volcanic and intrusive rocks similar to those hosting the Kemess deposits. Although no assay results of economic significance were intercepted, Serengeti is strongly encouraged by geological observations made during the 2017 drill program, and plans to expand the IP survey coverage in 2018 to refine the target area for additional drilling. All three drill holes intersected porphyritic andesitic volcanic rocks of the Late-Triassic Takla Group displaying propylitic and phyllic alteration mineral assemblages, and monzonitic rocks of the Late Triassic to Early Jurassic Black Lake Group. Serengeti is particularly encouraged by the presence of a distinct zone of strong to intense quartz ­ sericite ­ pyrite altered fragmental volcanic rocks analogous to those present at the Kemess Underground and Kemess East systems, as well as the identification of similar geochemical zonation patterns. The 2017 UDS program was successful in identifying the presence of an intense hydrothermal system. Specifically, the broad zone of phyllically-altered fragmental volcanics is similar to that found above the Offset Zone at Kemess, which lies between the Kemess East and Underground deposits. Monzonitic rocks at UDS show moderate to strong pervasive phyllic and weak potassic alteration associated with quartz ­ pyrite ­ magnetite +/- chalcopyrite veins. Multi-element geochemical zonation patterns in gold, copper, zinc and sulphur, as well as other elements, have added greatly to the understanding of lithological and alteration features at UDS, and provide encouraging vectors toward a possible mineralized center.