FISSION 3.0 CORP announced that drill programs are being planned for the upcoming 2022 winter and summer drilling seasons for its PLN Project in Canada's southwest Athabasca Basin region in search of high-grade uranium mineralization. PLN ranks highly in Fission 3's extensive portfolio by virtue of previous drilling having intersected basement hosted uranium mineralization and pathfinder elements showing large scale potential along a conductor that is open and untested to the NW, as well as having multiple untested and prospective drill-ready targets and being proximal to large-scale high grade uranium deposits. On September 29,2021 the Fission 3 announced a fully marketed private placement for gross proceeds of CAD 8,000,026. The Company intends to use the proceeds raised from the Offering for future exploration work on its uranium projects, including at PLN, corporate development and general corporate and working capital purposes. Fission 3.0 also announces 1.2 million options at $0.19. The 100% owned PLN property consists of 38 mineral claims and covers 39,946 ha; it is one of the most advanced of the Fission 3 projects and is prospective for high-grade uranium. It is located just inside and in the south-west area of the Athabasca Basin in proximity to Fission Uranium's Triple R and NexGen Energy's Arrow large high-grade deposits. The property is strategically located between Fission Uranium's PLS Property immediately to the south and the former Cluff Lake mine (>60M lbs U3O8 produced) and the UEX-Areva Shea Creek deposit to the north (42km and 27km respectively). Previous drilling at PLN by Fission 3 in 2014 identified a mineralized structure associated with the ~3 km long A1 conductor with strongly anomalous geochemistry, including uranium values, in addition to common pathfinder elements including boron, copper, nickel and zinc. Drill hole PLN14-019 intercepted a 7.5m interval (191.5m ? 199.0m) of anomalous radioactivity with peak measurements up to 1450cps (as measured by handheld spectrometer) over 0.5m within a strongly clay altered and brecciated graphitic gneiss which assayed 0.5m of 0.047% U3O8 within 6.0m of 0.012% U3O8.