GMS     The Georgia Mineral Society, Inc.
4138 Steve Reynolds Boulevard
Norcross, GA 30093-3059

GMS Field Trip November 2024

If you have any questions about field trips send email to

GMS Field Trip
Copper Ore, Slag, and Sericite after Staurolite in Tennessee
Saturday, November 9, 2024

The history of this location goes back to the 1800s when copper was big business in the region. Unfortunately, early processing methods released sulfuric acid that wreaked havoc on the surrounding areas, killing almost all plant and animal life for miles around. It took many years of reengineering ore processing, and many more years to even begin repairing the ecosystem, work that continues to this day. The current owner of the property is dedicated to the environmental clean-up, so the area is recovering incredibly well and is safe for people like us to tromp around.

We often call this location a UGA – unique geological area – because it never disappoints in the diversity of the materials available. This trip marks the first time that we were treated to piles of copper ore that had been inaccessible before. The property owner moved piles of ore from one area to another to make it much easier for us to peruse. Members collected numerous samples from the piles including some stunning microminerals before we headed to our next destination – slag piles.

The slag there is the byproduct of copper ore processing from the 1800s to as late as the 1980s. Crushed ore was refined via chemical processes, then the concentrate was heated until it became molten. Flux, a substance that binds to impurities, was added to help make the impurities lighter than the copper. Impurities were skimmed off and cast aside as slag. More information about this process is available at www.tn.gov (click here or click here for the same pdf that we have downloaded). You may have seen slag that is very much like glass because of high silica content in the ore and flux. The ore at this location has a high iron content, so the slag is mostly iron.

At first thought, slag may not seem very interesting, but the slag here has some fun shapes, patterns, and often contains beautiful secondary microminerals. When the slag was poured off, it cooled into all sorts of shapes. At some point, cracking and resolidifying caused slag that has an other-worldly, reptile skin-like appearance with red and orange colors. We call it “slagon” skin, a portmanteau of slag and dragon. Members are always intrigued by it and it is one of my favorite kinds of slag to find. As water makes its way through the slag piles, secondary minerals form. Beautiful gypsum microcrystals and other micros we have yet to identify are but a loupe away from enchanting the diligent collector.

The trip continued with the opportunity to get nice and dirty digging and screening for sericite after staurolite. Staurolite is the state mineral of Georgia. Its crystals can twin to form a cross shape that is often called a “fairy cross”. Sericite is a type of mica that can form as staurolite alters during metamorphism or weathering. The alteration produces a sericite pseudomorph that retains the shape of the original staurolite, in this case, crystals or “blades” up to 6 or 7 inches long and 2 to 3 inches wide. What we have observed here is mostly incomplete alteration, so some of the staurolite remains inside the sericite pseudomorph. Most of the specimens are also peppered on the outside with tiny almandine garnets as well. Again, the owner of the property went to great lengths to dig large areas out for us and to provide large piles of material for us to search through. In one pile, members found a white sandy area that appears to be almost pure sericite, and they found sericite after staurolite specimens in it. In another area, a junior skillfully extracted specimen after specimen until he had a gallon baggie full! He donated one very large specimen to the club, and even offered specimens to other people. He had so much fun that he wanted to stay “just 20 more minutes”, but rain was beginning to tap us on the shoulder, so we had to call it a day.

As always, we cannot thank the property owner enough for everything he does to make each trip special and productive. He moves so much material around for us; stabilizes areas; makes parking easier; and he even scouts new places with new materials for us to collect! Members performed car ballets like pros as we caravanned around the property, and they were generous and kind with each other, making sure everyone got some goodies. It was a wonderful day thanks to Charles Carter and all of his hard work and time spent organizing the trip.

Lori Carter on behalf of Charles Carter
e-mail:

Copper Ore

Photos by Diana Poppelreuter

trip
trip
trip
trip
Diana got some good pictures of the ore piles and some copper ore too
Photos by Lori Carter

trip
trip
trip
The piles were arranged for easy access
Photo by Lori Carter

trip
There were man-made artifacts of mining in the piles, and this may be such a thing... or not?
Photos by Lori Carter

trip
trip
This piece of slag in the ore piles looks like a piece of wood with a dog's paw
Photos by Lori Carter

trip
trip
This piece is very light for its size
Photos by Lori Carter

trip
trip
The texture of this piece is interesting
Photo by Lori Carter

trip
Tiny but mighty little piece of copper ore

Weird Cool Slag

Photo by Lori Carter

trip
Mountainous piles of slag
Photo by Lori Carter

trip
Lawrence found the coolest piece of rippled slag ever!
It is not flat, it is like a waterfall flowing from the smaller bit at the top
Photo by Lori Carter

trip
This is a more typical flat piece of rippled slag
Photo by Lori Carter

trip
I like the iridescence and tiny spheres on this piece
Photo by Lori Carter

trip
Another iridescent piece
Photos by Lori Carter

trip
trip
The iridescence on this piece is nice, but I really like the other side
Photos by Lori Carter

trip
trip
This one is also interesting on both sides
Photo by Lori Carter

trip
Iridescent with spheres
Photos by Lori Carter

trip
trip
Bubbly on one side and weird, almost fossil-like markings on the other
Photo by Lori Carter

trip
Jabba the Huh?

Here be Slagons!

Photo by Lori Carter

trip
Classic piece of "slagon" skin
In days of yore, did dragons smelt the ore?
Photo by Lori Carter

trip
This slagon skin was molted with a bit of slagon bone attached -- eeew
Photo by Lori Carter

trip
Wrinkled slagon skin
Photo by Lori Carter

trip
Biggest hunk o' slagon skin we've ever seen
Photos by Lori Carter

trip
trip
Slagon skin with a claw scratches on the back
(Is that an eye in the middle of the top picture?)
Photos by Lori Carter

trip
trip
White slagons?

Sericite after Staurolite

Photo by Lori Carter

trip
One of the many piles set aside for us to search
Photo by Lori Carter

trip
Big trench dug specifically for us
Photos by Lori Carter

trip
trip
trip
Lawrence found this beautiful sericite after staurolite with garnets.
White specimens like this are very unusual. Most have iron and are reddish brown.
Photo by Lori Carter

trip
Photos by Olga Jarrett

trip
trip
Olga found a typical specimen plus a very large white one
Photo by Lori Carter

trip
Dori found this twin, a rare find for this location
Photo by Lori Carter

trip
Can you see the sericite after staurolite?
Photo by Lori Carter

trip
There it is!
(Note the distinct diamond shape at the end of the crystal)
Photo by Lori Carter

trip
What is this? Kallie and I found it in the big trench.
Kallie thought it was an alien egg hatching, so as one would do in a movie, I poked it with a stick.
Nothing came out screeching and clicking, so we figured it was just a blob of oil.
Photos by Lori Carter

trip
trip
trip
trip
trip
This junior became an expert sericite after staurolite finder
Photo by Lori Carter

trip
trip
The specimen the junior donated to GMS!

Micros

Photos by Lori Carter

trip
trip
Example of micro gypsum crystals in the slag
The close-up is the vug in the lower right of the piece
Photos by Lori Carter

trip
trip
These micros have a distinct "bow tie" shape

Click below for field trip policies

policies
Copyright © Georgia Mineral Society, Inc.