



Iron Fen (Tqm) #03
Iron-rich spring water painted it red.
The base stone is quartz monzonite, some of the youngest granite in Colorado. Over thousands of years, warm water rich in dissolved iron coated it a deep red. This happens in fewer than a dozen places in the world. I sealed the red outer layer in epoxy to protect it.
Only about 7–9 stones like this are within reach, and I broke the first two while learning to cut them. There will be five or six more in this series, and each one will cost more than the last.
- Dimensions
- 26 × 20 × 10 in
- Weight
- 212 lb
- Age
- 38.8 ± 0.5 Ma
- Formation
- Iron bath / post-Pinedale
The western half of Colorado is chock full of idyllic wilderness spots to plop down and repose next to a lovely babbling brook.
But there's this one particular brook who babbles (slightly warm) water with wild concentrations of dissolved iron ions, even still to this day
This stone originally snapped loose a bit uphill of the modern day fen, eventually sliding to rest well downstream of the protected area, so it's hard to say if the thick outer red iron accumlation took more or less than 40,000 years to form. I encased it in epoxy to preserve it regardless
The base stone is a tertiary quartz monzonite, some of the youngest granite in Colorado; and the land owner I sourced it from is definitely one of the most eccentric ones I've ever met. The iron deposition process which painted the exterior red happens in less than a dozen other places in the world. There are probably only 7-9 more stones like this one that I can get my diamond saws on, and I shattered the first two I worked with, till I figured out the technique/touch required
The price reflects the rarity. There will only ever be 5 or 6 more like this one; so assuming anyone buys the first, I'll likely (p*2^n) the price for the remainder of the series


