to 1m wide within an easterly striking shear zone dipping to the north at 40°. The vein is hosted by sheared mafic volcanics and had been excavated over an estimated distance of 100m. Suguti Project The Suguti tenement application is located in northeast Tanzania within the historically productive Mara-Musoma Goldfield 40 km south of the township of Musoma and 25 km west southwest from the township of Buhemba. Access is gained from the sealed Mwanza to Musoma highway which passes through the western edge of the property. Internal access to the project is good with a graded access road traversing the property from east to west. The southern portion of the property is mostly soil-covered cultivated-ground that drains to the southwest into the Suguti River and then into Lake Victoria. The northern half of the property comprises steep hills and ranges with moderate to strong rock outcrop and has very little human habitation or cultivation. General land use is seasonal crop farming and no landholder access issues have been identified that will prevent exploration activities. The prospecting license extends approximately 9.3 km to the east and 8.3 km to the south for a total area of about 77 km². The Suguti property is located within the prospective greenstone belt of the Mara–Musoma goldfield. The outcropping geology comprises an area of mafic to intermediate volcanics that form a large easterly trending range of hills in the northern portion of the property. This range is dominated by a prominent and strongly magnetic BIF extending for at least 8 km across the property. Smaller BIF units occur elsewhere within the volcanic succession and these are typically 5 to 10m wide representing thin interflow sediments to the volcanics. The greenstones are most likely part of the Upper Nyanzian System. The south west corner of the project is covered by mbugu clays which have filled a topographic depression formed by the regionally significant northwest-trending Suguti shear. The primary shear extends in excess of 50 km and has displacements of several kilometres interpreted from the geology either side of the fault contact. The shear is also readily identified from the aerial magnetic data as zones of demagnetisation. A secondary cross cutting northeast trending fault terminates the eastern end of the prominent BIF horizon. This 0600 orientation is an important control on mineralisation which is known to host gold resources elsewhere in the Mara-Musoma goldfield. Nickel Overview