Anson Resources Limited has conducted additional testing of flow rates of brine from its recently completed exploration drilling of the Skyline Unit 1 and Long Canyon No. 2 wells at its Paradox Brine Project, located in Utah, USA (the Project) in conjunction with the completion of down hole geophysical surveys. The data collected is being analysed and will be used in the estimation of a JORC Resource. The flow rates have increased significantly in both wells, with the Skyline well now averaging 6,000 barrels per day and Long Canyon No. 2 averaging 2,700 barrels per day. The increase in flow rates is due to the natural cleanup of the clastic horizon following the re-entry drilling and not to any break down of the zone. Table 1 shows the original and updated flow rates recorded. The flow rates at Skyline Unit 1 and at Long Canyon No. 2 wells were significantly higher than Anson found during the re-entry of Cane Creek 32-1 well which supports Anson's theory that the fracturing by the geological structures in the central and southern area of Anson's claims, particularly the Roberts Rupture, will assist with brine flow without the need for extraction pumping which is significant for Project economics. The Roberts Rupture structure, which is thought to provide natural fracturing of the host rock allowing the flow of fluids, is located striking through the eastern claims. The western claims show areas of structures which are similar to that near Roberts Rupture. The plan below shows the location of the Project claims and their proximity to the wells in the area that have previously been assayed for lithium. The dolomite is quite porous and permeable, whereas the anhydrite and black shale is crushed and broken. Usually the fractures are filled with salt, but where brine is present no salt filling occurs. Historical drilling of the White Cloud No. 2 well, which offsets the Long Canyon No. 1 well, recorded brine flowing when the top anhydrite was penetrated, and rapidly increased by the time the underlying black shale was penetrated, so that no further drilling was done. The dolomite zone was not drilled. Vertical porosity, permeability, and communication are indicated. Brine flows have been encountered in Clastic Zone 31 over a distance of six miles north-south and eight miles east-west, and it remains to be proved if brine is present and the zone is communicable over a much larger area. A reason for the presence of supersaturated brine in the clastic zones is that these horizons overlie rich potash and magnesium zones. In the classical concept of the evaporite cycle, the most soluble compounds are the last to precipitate. Therefore, the clastic units often overlie the end products of the preceding evaporite cycle. Potassium and magnesium chlorides and certain complex evaporite minerals can be found among the end products of evaporation. The fractured clastic zones form an excellent reservoir for brines derived from underlying evaporite units. The fracturing is caused by salt flowage, and it is possible that, when brine is removed from these zones, salt will flow into voids from which brine has been removed. This would help maintain high reservoir pressure and assist in a high ultimate recovery of brine. Cores obtained from wells in the area have exhibited fractures filled with salt when brine has not been present.