Golden Goliath Resources Ltd. announced that the drilling of the proposed holes has now been completed on its 100% owned Wish Ore project, located 12 km from the Trans-Canada Highway north of Sault Ste Marie, Ontario. Samples from Hole 1 have been sent to the laboratory, but core from the other holes is still being logged and sampled. The purpose of this program was to do a preliminary drill test of the known showings to get a better understanding of the mineralization, geology, structure, and alteration associated with the known gold values.

The company find the core quite interesting and are doing detailed geological analysis. This preliminary drill program consisted of 4 diamond drill holes totaling 583 meters. The program targeted the two main showings on the property and IP chargeability with coincident gold geochemical anomalies near the showings.

W22-01 The hole was drilled for 201 meters, located 130 meters to the northwest of the New Zone. The drill hole targeted an IP chargeability anomaly which is coincident with anomalous gold, arsenic, and copper in soil. W22-02 Was drilled for 101 meters targeting the New Zone trench that had returned channel sample results of 4.28 gpt gold over 3 meters, including 1 meter of 9.05 gpt gold within a larger area of anomalous gold results.

The entire hole showed alteration with quartz veining. A 10-meter zone near the bottom of the hole with sulfides is particularly interesting. W22-03 This hole was drilled for 170 meters and located 120 meters north of the trench zone, targeted on an IP chargeability anomaly with coincident gold in soil anomalies.

W22-04 Was drilled on the Trench Zone for 111 meters. The Trench zone is a broad area of quartz carbonate alteration with anomalous gold values of up to 0.5 gpt over 2 meters. Alteration with quartz veining and sulfides are present throughout the hole, with a 40-meter section with more intense silicification and sulfides.

Permitting is presently underway to allow for a potential winter geophysics program to better refine the possible source of the mineralized boulders along the trend north of Crack Mouse Lake.