Second Annual Report year ending 23 October 1989 Woodleigh.

Abstract

Stream sediment sampling showed that the area north and northeast of ERL87 to have anomalous gold levels they rise with EL5346. Gold enrichment in stream draining from south southeast of ERL87 are probably caused by the northern extension of the North Ringwood mineralisation. No base metal anomalous zone defined in the south. Several scattered stream sediment anomalies occur in the central area. The east low order anomalies drain Henry's Hill-an area which gave values over 1g-t gold over a strike length of 3km peaking 8.8g-t over 0.7m. At Henry's Hill gold is hosted in quartz lenses within the Mount Bonnie and Burrell Creek Formations. An intermediate zone of enrichment extends approximately 8km northwest from Pelican Prospect. In the north several isolated anomalies have been outlined including Simon's Reef (quartz pods in silicified and sericitized siltstone). Grades were up to 3.9g-t gold. Reef strike length is approximately 200m.