First Energy Metals Ltd. announced that it has entered into an option agreement to acquire a lithium exploration property located in Landrienne & Lacorne-Townships, Quebec, Canada. The property consists of three non-contiguous claim groups representing a total area of 627.35 hectares located approximately 40 kilometres northwest of the town of Val d'Or on map sheet 32C/05. The geology and the mineralization of the Augustus property are similar to the geology and mineralization of Quebec Lithium mine located approximately 6 kilometers to the southeast of the property. The Augustus pegmatite was explored in 1955 by trenching followed by diamond drilling. The pegmatite is oriented N30°W, extending more than 850 meters along strike with 7.6 meters in average width. Its depth extension is not fully known yet, however previous drilling has intersected high-grade lithium down to 682 feet (207 m). Lithium mineralization is confined to the pegmatite body with an average grade of 1.12% lithium oxide (Li2O) (0.52% Li) across a width of 7.6. meters (Source: Géologie Québec - Results of the query (gouv.qc.ca)). The highlights of the previous drilling results include:1.69% Li2O over 9 feet (2.74m), 1.25% Li2O over 27.5 feet (8.38m), 1.07% Li2O over 20 feet (6.1m), 1.66% Li2O over 12.5 feet (3.8m), and 1.41% Li2O over 27 feet (8.23m) (Source Report GM03952). Based on the 1955 drilling results, the continuity of lithium mineralization is established between all drill holes for over 850 meters strike length down to a depth of 207 m (682 feet) of the Augustus pegmatite body . If mineralization continuity can be proven by future drilling down to over 200 meters level as shown in historical drill hole results, a potential resource target of 4 million tonnes at 1% Li2O can be achieved. The Canadian lithium prospect is a worked deposit located in Range 1 lot 25-26 in the Landrienne Township at G.P.S 284861 E - 5368288 N. The main outcrop was discovered in 1948 near the boundary line separating the Landrienne and Lacorne Townships. A group of parallel pegmatite dykes associated with Lacorne Batholith contains aggregates of spodumene, lepidolite, quartz and feldspar accompanied by traces of beryl, clevelandite, colombo-tantalite. Drilling at the prospect have shown low grade lithium bearing pegmatite intersections of extensive widths. A total of 11 historical drill holes are located on this prospect. The Company is in the process of compiling historical drilling data on this prospect and will release as soon as possible (Source Reports GM03952 and GM00744).