Montego Resources Inc. announced that it has planned an airborne mag survey over 1,400- hectares of its Black Dog Project. An airborne Triaxial Magnetometer survey will be flown over the project and the Company plans to utilize the data from the survey to interpret lithology and geological structures which are known to have a control on gold mineralization. The proposed survey may indicate anomalism within the property which could be used in future exploration programs by narrowing hot zones.

About the Black Dog Property: The Black dog project consists of a block of 27 mineral claims for a total of 1,400 Ha, and is road accessible and located approximately 60 kilometers north of Nemiscau, Quebec. Historic Exploration: While there is minimal historic exploration on the property, exploration in the immediate area has focused on the narrow volcanic belt which hosts the Black Dog Lake Showing and most recently on Dios Exploration's adjacent AU33 West project where the recently discovered Heberto gold showing is being drilled. The adjacent Black Dog Lake showing was discovered in 1988 when Eastmain resources re-sampled 1970's Hudson Bay core which returned a value of 5.1 g/t Au over 1.52 meters.

Subsequent geophysics, geochemistry and AQ drilling by Eastmain identified the Black Dog Lake zone with values of 15 g/t Au, 5.6 g/t Au and 4.3 g/t Au, each over close to 1m. Geology: Most of the property overlies large granodiorite and gneissic intrusives with lesser pegmatite which are largely unexplored. Immediately east and south of the Black Dog property, Dios Exploration holds the AU33 property underlain by the same geology.

Dios has had multiple recent discoveries of surface gold showings within silicified granodiorite and tonalite, as well as within quartz veins and has been following up on the showing with successful drill campaigns in 2015 and 2016. These same intrusive rocks carry onto the Black Dog property and warrant investigation. Mineralization: The adjacent Black Dog zone is described in the MERN Sigeom files as an east- west trending zone, 600 meters long, with a thickness varying from 1 to 3 meters.

The host rock is a metamorphosed mafic to felsic tuff enclosing layers of chert with interbedded semi-massive sulphide. The chert is interpreted to be an iron formation. The semi-massive sulphides are predominantly pyrrhotite with lesser pyrite and minor chalcopyrite.

Gold, silver, minor zinc and copper are the principal economic elements.