As a follow on to the announcement made by West African Resources Limited on 29 April 2020 with regard to it entering into a definitive agreement to acquire 100% of the Toega gold deposit (Toega) from B2Gold Corp. (B2Gold) and their partner, GAMS-Mining F&I Ltd. (GAMS), the Company clarifies the following regarding the foreign Mineral Resource under listing rule 5.12: A summary of the work undertaken by B2Gold to produce the Mineral Resource Estimate follows: The Toega Project is hosted in the Paleoproterozoic-aged Birimian Supergroup (2150 - 2100 Ma) and is located close to the intersection of the northeast striking Tenkodogo greenstone belt and the regionally significant, north-northeasterly trending Markoye Fault corridor. The Toega Prospect area is underlain by metasedimentary rocks which have been affected by greenschist to lower amphibolite facies regional metamorphism. Alteration mineralogy comprises potassium feldspar, quartz and white mica. Pyrrhotite, pyrite and arsenopyrite are the dominant sulphide mineral phases and sulphide content is typically less than 5% in mineralized zones. Locally, visible gold is observed in association with quartz veins and rarely, as intrafolial grains in the metasedimentary rocks. The majority of gold mineralization in the Toega deposit occurs in unweathered rock. There are three main lithologies (MPEL=metapelite, MMSA=mafic meta-sandstone, FMSA=felsic meta-sandstone) with more than 77% of the ore grade mineralization (by volume) in FMSA. A 3D structural model was built using foliation (and likely some bedding) measurements made on drill core. The structural model was used to inform the search orientations used to build the lithology model. Base of overburden, saprolite and saprock surfaces were modeled; gold grades were estimated in all saprolite, saprock and fresh (grades not estimated for overburden). Mineralization domains (grade zones) at nominal grade thresholds of 0.2g/t and 0.8g/t were implicitly modeled as 3-D solids using Leapfrog software. Lithology, mineralization and structural measurements were used to control the overall geometry of the zones.