located in north east Tanzania within the historically productive Mara-Musoma Goldfield some 9 km due southeast of its namesake township, . Access is to the Sarama property along a local inter-village vehicular track. There is a track leading more directly to the town of Buhemba but it is in poor repair and difficult to follow. Local access on the property is generally poor and via village tracks and trails. The tenement straddles the contact between granites and greenstone belt of the Mara-Musoma goldfield. Approximately two-thirds of the tenement is underlain by granitic rock types while the north western third comprises sub-cropping volcanics of mainly mafic to intermediate composition of the Nyanzian System. Twof granite occur in the southern third of the property but most of the granite is covered by extensive mbugu plains. The volcanic rocks outcrop as a NE-SW trending range of hills and about half of the 4 km of strike length is exposed within the property boundary. Structural interpretation of the magnetic and gravity geophysical data also confirms the location and strike of the Nyanzian System rocks. - Sarama Project The Sarama tenement is located in north east Tanzania within the Mara-Musoma Goldfield, 10 km due south of the township of Buhemba and 20 km east of the Suguti Project. Access is via the sealed Mwanza to Musoma highway up to the small township of Butiama, then via graded roads to the township of Buhemba and on to Sarama village located close to the northern boundary of the property. Internal access is good as the land is relatively flat with drainage typically towards the south. Sarama extends approximately 4.5 km to the east and 4 km to the south for a total area of about 18 km². The tenement straddles the southern boundary of the Mara-Musoma greenstone belt with granites but the geology is largely covered by thin soils overlying sub-cropping residual laterites. The greenstones are most likely part of the Nyanzian System and the southern portion of the tenement is covered extensively by mbugu soils which are interpreted to overlie granite. At least 4 km of ESE striking granite-greenstone contact has been identified from reconnaissance mapping. Structural interpretation of the magnetic and gravity geophysical data indicates a series of easterly trending structures parallel the main contact into the greenstone sequences. Mapping of artisanal workings within the northwest quadrant of the tenement identified a quartz vein up