Most Prospectors Chase Shiny Rock.
We Chase Rust.

Most people chase shiny things. They want bright white quartz, glittering sulfides, and rock that looks like it belongs in a museum case. I don't mind pretty rock, but that's not what gets my attention first. What stops me in my tracks is ugly rock - rusty, crumbly, stained, and half-rotted. The kind of rock most people kick aside without a second look.

Deep underground, gold often travels with sulfur-bearing fluids and ends up tied to sulfide minerals - most commonly iron sulfides like pyrite. Down there, in the dark, those sulfides are stable. Bring that same rock up toward the surface and the environment changes completely. Oxygen, water, and time all go to work on those sulfides. The iron doesn't disappear - it turns into oxides and hydroxides. The rust colors you see as reds, browns, yellows, and oranges.

Gold, on the other hand, doesn't oxidize and dissolve as easily under these conditions. As the sulfides rot away, the gold they once hosted is often left behind - sometimes slightly concentrated in the remaining rock and soil. That “rotted” zone is what we're interested in...

The old-timers had a different world. Back then, gold was cheap by today's standards, and the equipment to crush and process ore was limited. That shaped how they thought. They chased visible, high-grade ore - rock that carried an ounce or more per ton - and they were quick to toss anything that didn't impress them right away.

That created two blind spots you can exploit: lower-grade material that would be perfectly profitable today, especially if it's easy to process - and fine and micro gold they couldn't see and couldn't reliably recover at the time.

When you stand on an old dump, you're not just looking at trash. You're looking at a filter. That pile represents the rock they decided was “not worth it” - by their standards, in their time. Your standards are different. You have better knowledge, better small-scale gear, and a very different gold price behind you...

Imagine a quartz vein running for half a mile along a hillside. On paper, that sounds like a gold mine. In reality, most of that length might carry only tiny amounts of gold - trace values, interesting, but not profitable. Then, within that same vein, there might be a hundred-foot stretch where the grade suddenly jumps. That enriched part is what we call an ore shoot.

An ore shoot is a zone - usually elongate - where the gold grade is significantly higher than the average. It might plunge down into the hill like a tilted cigar, follow a bend in the vein, or sit where two structures intersect. The key point is this: ore shoots form where the plumbing allowed more fluid to flow, slow down, or change pressure in a way that favored heavy deposition.

You are not trying to own an entire vein system. You are trying to recognize, test, and focus on the parts where the gold actually concentrated...