You may have noticed a theme in my recent postings... these are all from a new series I am working on from the Southwest, photographs made over the past year. I'm hoping to get the whole body of work up on my site in the next week or so.
These are Moki Marbles in Harris Wash, near Escalante. 30D, 17-40 L, processed in Lightroom.
If anyone can explain how these are formed I'd be happy to hear it...
Moki Marbles are such fun subjects! One of these days I'm going to get out there and find some of my own.
These "marbles" are just iron rich concretions. If you look around you will probably find them weathering out of nearby sandstones, uphill. The Jurassic, Navajo Sandstone seems to be the dominant host rock. Apparently the porosity and permeability of these dune sands is especially suited to iron concretion precipitation. They certainly are capable of transmitting a LOT of fluid.
Very nice, Nat. I like the high-key treatment as it strengthens the graphic qualities of the image. Nice work with the comp, too. I imagine this looks phenomenal in print!
Discussion
9 repliesThese are Moki Marbles in Harris Wash, near Escalante. 30D, 17-40 L, processed in Lightroom.
If anyone can explain how these are formed I'd be happy to hear it...
These "marbles" are just iron rich concretions. If you look around you will probably find them weathering out of nearby sandstones, uphill. The Jurassic, Navajo Sandstone seems to be the dominant host rock. Apparently the porosity and permeability of these dune sands is especially suited to iron concretion precipitation. They certainly are capable of transmitting a LOT of fluid.
See pages 8 through 11 in this pdf for some additional details on the chemistry. Page 11 as a condensed summary:
http://geology.utah.gov/online/pdf/pi-77.pdf
I heard that you and my dad (Edward Coalson) used to work together at Amoco?
Small world...
So, how is it that you didn't already know the answer to your question?