Rush Gold Corp | Douglas Canyon

PROJECT SUMMARY

Douglas Canyon hosts a prospective geological setting

Douglas Canyon is located in the Camp Douglas area, in the Walker Lane, Camp David/ Mina district of southern Nevada
Walker Lane Trend hosts several significant gold (+/- silver) deposits:
- Comstock (5Moz Au)
- Borealis (2Moz Au) <50km west of Douglas Canyon
- Round Mountain (20Moz Au)
- Goldfield (4.5Moz Au)
Douglas Canyon has a favourable geological setting within a low-sulphidation epithermal gold-silver mineralised system
Mineralisation is structurally controlled by regional scale NW trending shear zones with shear linked structures hosting vein style gold mineralization along a major structural disconformity between Tertiary andesite and a Penn-Perm Havallah sedimentary package
Deflections in the shear zones as they cross the lithological contacts appear to be the focus for high grade Au and Ag mineralisations.
Host rocks are mainly andesitic volcanics with a number of prominent chert ridges separating individual flow units.

56 rock chip sampled taken across float samples and outcrops.
Sampling targeted high-grade outcropping quartz veins hosted in sheared structures.
Best results returned grades including 16.2g/t Au, 495 g/t Ag; 14.0 g/t Au, 423g/t Ag; and 18g/t Au, 398 g/t Ag.
Surface sampling confirmed that multiple structures crosscutting Douglas Canyon are similarly mineralised and are interpreted to continue to the northwest onto the Antimony Blossom Prospect.
One specific structure that seemingly aligns with the Antimony Blossom workings shows elevated antimony in previous sampling.