
Crushed Quartz & Fault-Fill Veins – Hidden Feeders in Gouge Zones
Description:
Beneath your feet, shattered quartz veins may be doing more than just looking interesting—they may be acting as hidden feeder systems for gold. In this eye-opening class on structural geology and gold prospecting, we dive into the role of crushed quartz and fault-fill veins in guiding mineral-rich fluids to fault gouge zones.
These are not just random breaks. When quartz veins get caught in a fault, they fracture and break under tectonic stress. That crushing action opens fluid conduits, creating localized pressure drops that allow gold to precipitate. The result? Gold gets trapped in the adjacent gouge—often where most prospectors never test.
In this module, you’ll learn:
• What crushed quartz looks like when it’s associated with fault gouge
• How vein reactivation feeds gold-rich hydrothermal pulses into surrounding rock
• Why gouge acts as a chemical and physical trap for gold when located near shattered veins
• How to sample both vein interiors and clay-lined fault walls
Key Features to Watch For:
• Angular quartz fragments in soft gouge matrix
• Limonite and manganese staining along fractures
• Talc-like clays near the edge of broken quartz zones
• Intermittent silica cementation or brecciation within the gouge
These aren’t just geological curiosities—they’re pathways that can lead to high-grade ore pockets. If you’re prospecting in areas with known fault zones, don’t just follow the vein—follow the crushed path.
We’re giving you the field knowledge that old-timers learned the hard way. And if you want to boost your edge, pair this with our Deep Dig AI Gold Maps. They highlight fault traces and structural intersections where gouge zones and crushed quartz veins are likely to occur—across the western U.S. and beyond.
🎯 Don’t forget to check out the full video and grab your downloadable field guide PDF below.
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