Jadar Resources Limited announced the transfer of the Khartoum tenements to the Company, thus concluding acquisition of the Project. The Khartoum Project comprises five granted Exploration Licence for Minerals (EPM) and one EPM application covering 390 square kilometres. The tenements host a large number of historic mines, primarily for tin, although lead-zinc-silver, tungsten and minor amounts of copper and gold have also been won. Recent sampling has also returned elevated indium results. Jadar is currently compiling the large amount of available historic exploration and mining data to define an exploration strategy for the Project. Work by previous explorers has already outlined several drill targets with only one prospect tested by recent drilling. Historic drilling has returned significant results at several prospects, however exact collar locations are unknown. Numerous outcropping occurrences tin-greisen mineralisation have previously been mapped and sampled within the Khartoum Project. The greisen-style mineralisation provides an attractive low-grade, bulk tonnage Mineral Resource target, particularly with tin prices over $US35,000/tonne2. Potential also exists for smaller high-grade (>1% Sn) Mineral Resources associated with historic workings that could be blended with the greisen mineralisation to increase mill head grade. Tin mineralisation in the Khartoum-Kitchener area occurs mainly as fracture-controlled fissure filling associated with quartz veining, or replacement greisen bodies. Figure 1 shows historic mine production within the Khartoum area. It should be noted that all the historic production is from higher-grade (typically greater than 1% tin) vein-associated mineralisation. Greisen mineralisation was too low grade for historic production. There is demonstrated potential for both economic low-grade, bulk tonnage greisen-style mineralisation and high-grade vein-style mineralisation within the Khartoum Project. Mineralisation in the Kitchener area is of the higher-grade, quartz vein-hosted style. Host lithologies are sediments of the Hodgkinson Formation, with metalliferous veining infiltrating fissures within the sediment carapace from the underlying tin-granite source. Mineralisation is generally less continuous however grades are greater than 1% Sn. An example is the Kitchener line of lode that includes the Black Rock, Central Hill, Kitchener, Kitchener Extended, Ivanhoe and Eclipse quartz reef workings, and extends further north to the You and Me open pit, a line of lode that extends for 1.3km . The major years of production were from 1903-1910 when approximately 144,000t of ore was mined at an average grade of 1.7% Sn (Blake, 1970)3. The You and Me Mine was the last of the deposits to be worked - between November 1964 and July 1969, the mine produced approximately 3,090 tons of greater than 2% Sn ore. The Ivanhoe Mine accounted for almost half the historic tin production with 32,364 tons of ore produced at 3.26% Sn.