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At the Toiyabe,
Figure 1: Recumbent Fold on the East Saddle Property in Upper-Plate Vinini Formation;
Evidence for Compressional Tectonics
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Figure 2: Parasitic S-fold Looking North at the East Saddle Property in Upper-Plate Vinini Formation;
Continued Evidence for Compressional Tectonics
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Figure 3: Large-Scale Brecciated Disharmonic fold on the Turquoise Canyon Property
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187 surface rock chip samples were collected from the Toiyabe,
Figure 4: Location of Rock Chip Samples Collected from the Toiyabe,
Figure 5: Example of 1-Foot-Wide Quartz Vein Cutting through Upper-Plate Vinini Formation
At the Company’s Coyote and Rossi Projects on the Carlin Trend, tectonic breccia was observed along the mapped Coyote NE Fault, trending at an azimuth of 065° (see Figure 6 below), an identical orientation to the mapped fault. Local small-scale structures often coincide with larger-scale structures developed regionally in
Another set of structures trending at an azimuth of 010° and intersecting the Coyote NE fault were also observed. These structural intersections traditionally form a preferential setting for increased gold mineralization in
Figure 6: Tectonic Breccia Developed in Upper-Plate Vinini Formation;
Evidence for Compressional Tectonics
Figure 7: Hydrothermal Quartz Veins Developed in Upper-Plate Vinini Formation,
Above the Prospective Lower-Plate Carbonate Rocks
Qualified Person
The technical information contained in this news release was reviewed and approved by
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President, CEO & Director
colin@westwardgold.com
www.westwardgold.com
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