Wolfden Resources Corporation announced additional encouraging assay results from its 100%-owned Pickett Mountain Project, located in Penobscot County in north-eastern Maine, U.S.A. These assay results are from the final four drill holes of the 2018 infill and expansion drill program. The Pickett Mtn, Project is one of the high-grade undeveloped zinc-rich, volcanogenic massive sulphide ('VMS') deposits in the world and the new footwall zone discovery adds a third zone to the two known zones (East Lens and West Lens) that remain open for potential expansion. Lens (E1) at a vertical depth of 650 metres. The 4.1 metre massive sulphide intersection occurs in intensely altered felsic fragmental rocks suggesting the presence of folded and or stacked massive sulphide lenses. The replacement-style massive sulphide mineralization consists of pyrite, sphalerite, galena and chalcopyrite, that includes the high-grade base and precious-metal values as documented in the table below. Historic drill results from the 1980's, indicate that only two of the +70 drill holes were extended deep enough to intersect what would be the plane of the footwall zone. Those holes are situated at some distance away from the high-grade intercept of hole 031, and returned several narrow intervals of massive sulphide mineralization bearing appreciable zinc-lead values. Follow-up drilling is clearly warranted to test for extensions of this zone. Drill holes PM-18-029A and 032 represent deep step-out holes that intersected the West Lens at vertical depth of 550 and 600 metres below surface, respectively. These results were not included in the recently announced mineral resource estimate of January 7, 2019 and indicate the significant potential to add to the mineral resources at depth. Hole PM-18-035, intersected the East Lens at a vertical depth of 380 metres, with a massive sulphide intercept of 37.5 metres. This intercept is 40 metres west and 60 metes deeper than the neighbouring historical drill hole G-70, that yielded multiple intercepts including 17.2 metres of 4.1% ZnEq., 38.1 metres of 4.7% ZnEq. and 17.9 metres of 8.2% ZnEq., within a 90 metre massive sulphide interval. The excessive thickness of the massive sulphide lens at this locale is of more interest and may represent the hinge or keel of a fold in the lens that plunges at depth towards the southwest. Further drilling to test this theory and explore for higher grades is warranted.