PAYDIRT PRACTICE PANNING WITH SILVER 1Kilo, 1,000 grams
GOLDEN RULE OF GOLD PANNING - CLASSIFY!
Classify to 300, 200, 150, 100 and 50 Microns.
Process the individual size groups separately. Pour waste water through a 75 and 50 Micron filter and note how much material is caught while the water is dirty vs cleaner.
For extremely fine, sub 75 Micron Gold capture, filter waste water through a 75, 50 and 37 Micron sieve.
BIG MINING GETS 3-15 GRAMS PER TONNE, PER 1,000KILOS
This is1 Kilo. Except for the obvious silver, Youll need a zoom lense to check for other precious metals.
EXCEPT FOR SILVER AG - There are No Guarantees, Our Other Panning Product IS Guaranteed, NOT THIS ONE. However if you classify as directed, it is almost certain to find Gold. Albeit Tiny Gold! Flour Gold!
This is REAL GOLDFIELDS DIRT CLAY AND HEAVIES WITH a chance for fine gold, very small amounts, and heavies from Goldfields in Kings Plains NSW.
DOES CONTAIN SILVER...
POTENTIALLY Contains....
Because Its for fun and Practice... a variety of minerals and metals, potentially including potential traces of:
Electrum: Gold and Silver composite.
Gold (Au): Often found as fine particles, flakes, or even small inclusions.
WILL CONTAIN Silver (Ag): Associated with gold in sulfide ores.
Copper (Cu): A base metal often found in conjunction with gold and silver.
Platinum Group Metals (PGMs): Osmiridium, platinum (Pt), palladium (Pd), and iridium (Ir).
Iron Oxides: Such as magnetite and hematite, commonly present in heavy mineral deposits.
Sulfide Minerals: Includes pyrite (fools gold), chalcopyrite and arsenopyrite potential indicators of precious metals.
Quartz (SiOâ): Often the host rock for gold veins, quartz fragments may also be present.
Zircon (ZrSiOâ): A dense mineral found in heavy mineral sands, occasionally in placer deposits.
Garnet: A common dense mineral, often reddish or brown.
Ilmenite (FeTiOâ): Heavy and black, often found in placer deposit
Finding the smallest Gold when prospecting allows the Prospector to begin "Tracing" or tracking the Gold back to its source.
Learn how to do this and find you own source!!