40 metres and the water table is approximately at a depth of 80 metres. 

Preliminary geological modeling suggests that the gold bearing system comprises a sub-vertical, north-trending Main Zone at least 350 metres in length, open to the north and south. Two other zones, West Zones, splay off the Main Zone, each with a strike length of approximately 100 metres. Using 0.5 g/t Au as a cut-off, the Main Zone has an interpreted true width ranging from 25-50 metres while the West Zones gradually decrease in width from 20-35 metres down to 8 metres south- wards along their length. The mineralization carries a high grade core, 6-16 metres in width, that can be traced along the length of the structures. 

## Kofi Southwest – Zone C 

Zone C is located on a ferricrete plateau 2.5 km west of Zone B. The mineralized system was first located by AXMIN in 2000 on a single RC drill fence across the 500-metre long soil anomaly. 

In 2002, a total of 1,568 metres, on six RC drill fences were drilled across the anomaly at intervals ranging from 40 to 120 metres. The central portion of the mineral- ized system was drilled on fences spaced at 40 metre intervals. 

The underlying geology is similar to that of Zone B and preliminary geological modelling of the mineralized zone suggests that it comprises of a single lens with a strike length of at least 160 metres. The mid-section of the lens has a maximum true width of about 40 metres. Two higher grade zones have been recognized within the lens which have strike lengths of about 100 metres. Drilling to date has tested the system to a vertical depth of only 30 metres. 

## Kofi Southeast 

The Kofi Southeast prospect, located 7.5 km to the east of Zone B, is defined by at least three parallel north to south trending soil anomalies covering an area 1.2 km by 1 km. This anomaly is interpreted to overlie a major north-south structure. 

Four RC drill fences were complet- ed across this anomaly during the 2002 drilling program for a total of 2000 metres. Angled RC holes were drilled to a vertical depth of 30 metres on three fences spaced at 200 metre intervals, a fourth fence was drilled at a further 100 metres to the north. 

Gold mineralization has been identified over a strike length of 400 metres and the mineralized zone remains open to the south where the soil anomaly indicates that the structure may extend for at least a further 400 metres. 

A preliminary interpretation indicates that the true width of the mineralized envelope, using a 0.5g/t Au cut-off, ranges from 50 metres in the north to about 10 metres in the south. 

