AFMS Member
Associated with the American Federation of Mineralogical Societies
 
Mineral Section
 
Member of the South east Federation
Members of the Southeast Federation of Mineralogical Societies
 

MINERAL SECTION Meeting –
July 15, 2008
7:30 pm
The next Mineral Section Meeting will be held on July 15 at Richard Graveline’s house in Snellville. His address is 2223 Chaparral Drive and phone is 770-972-8741.

The topic for the evening will be Optical Properties of
Minerals. This will be a repeat since only one member was able to make it to the May meeting.

The meeting will be at the usual time of 7:30PM. RSVP
with Richard for directions and any plans about supper before the meeting.

Thanks and I hope to see everyone in July.

 I hope everyone cam make the meeting.  It promisses to be an interesting evening.  We always have lots of interesting minerals to look at in support of the topic of the meeting. 

 If you are interested in hosting a section meeting at your home or have an idea for a presentation, please contact us.  The topics are always interesting and educational, so please join us!


Jay Gorday
1690 Granger Ct
Chamblee, GA 30341
770.986.0822

minerals@gamineral.org
Mineral Section Chair


Friends of Mineralogy Southeast Chapter
www.Southeastfm.org
The Southeast Chapter of Friends of Mineralogy has launched a new web page, which can be found at www.southeastfm.org.  Membership details and many mineralogy events in the southeast as well as useful links can be found there.  Details of the Southeast FM fall symposium can also be found there.  

 Friends of Mineralogy Southeast Chapter Fall Symposium
(Information and details at http://www.southeastfm.org)

Dahlonega Gold Symposium
SE Chapter FM Meeting - 2001


WEINMAN / TELLUS SCIENCE MUSEUM
Mineral Section Meeting
PHOTO ALBUM
MINERAL LINKS
MINERAL CLEANING INSTRUCTIONS:
COPPER SPECIMEN CLEANING:
Cleaning Pyrites:
"Enhydros"
 Fluorescence
and Other Color Changes in Minerals:
 "Zoning in Minerals"
Fluorite (CaF2)
Care and Feeding of Crystals
Begins in the Field

[ Home ] [Mineral Section] [ Gem Section ][ Fossils Section ] [Micromount Section][Junior Section]

  

Large Calcite Formation Found in N.M. Cave

Snowy River Calcite formation

By SUE MAJOR HOLMES, Associated Press Writer
Tue May 31, 8:48 PM ET

ALBUQUERQUE, N.M. - A calcite formation named Snowy River could prove a gold mine for scientists.

Snowy River, believed to be the largest continuous calcite formation in the world, was discovered in September 2001 by a  Bureau of Land Management team led by veteran speleologist John McLean of Colorado.

The stark white passage, looking like a river of snow surrounded by walls of brown clay and black manganese dioxide deposits, stretches more than two miles from Fort Stanton Cave in sourthern New Mexico.

It's not a Carlsbad Caverns-type cave. Fort Stanton has few secondary formations such as stalactites; the one outstanding formation is Snowy River, expedition leader John Cocoran said Tuesday, the day the formation's discovery was formally announced.

Water originally carved a channel in the clay and gravel, then eventually filled it with brilliant white calcite.

It's not easy to explore. So as not to contaminate the formation, scientists who go into the passage change shoes — and in some cases, clothes — when moving from the clay edges to the Snowy River formation, Cocoran said. The round trip to the south end requires 16 changes of shoes, he said.

Scientists believe the new passage could yield information on everything from specialized bacteria to underground drainage, Cocoran said.

The original discovery drew a few local news reports, but scientists wanted to keep the passage's existence quiet until an environmental assessment could be done and arrangements could be made to protect it.

The emphasis for the future will be for scientific research and conservation — not recreation, Cocoran said.

"It's a really unique formation," he said. "Nothing of this size or quality is seen in any other caves."

Researchers would like to know how the passage formed and how old it is. Initial study indicates the last time calcite was deposited was about 150 years ago, but the formation could be much older, Cocoran said.

Penny Boston, director of the cave and karst studies program at New Mexico Tech in Socorro, has been studying the microbiology of the passage. She has found several types of bacteria that live in a lightless environment and are unknown anywhere else.

"The chemical byproducts of these bacteria may have pharmaceutical applications and there are other things biologists and biochemists can learn," Cocoran said.

Fort Stanton Cave itself, which was designated a National Natural Landmark in 1975, is open by permit only. It is not improved, and going into it requires hard hats and boots.



The Virtual Cave:

From the comfort of your keyboard, browse the wonders of the underground!

Underground wonders
They're dissolved out of limestone, formed from flowing lava, eroded in rocks by water and wind, carved by the power of oceans, and now uploaded on the Internet. Just say no to bat guano and explore these beautiful wonders from the critter-free comfort of your keyboard.

"Hardness made harder"
or 
and you thought I was a nerd?

The Moh's scale of hardness is familiar to all.  An interesting item by J. Alex Speer of the Mineralogical Society of America appeared on page 273 of the July/August 2003 issue of Rocks and Minerals magazine.  This technical note refines one of the standard points on the Moh's hardness scale.

Most mineral identification books list pennies as having a hardness of 3.  Alex reports that in 1983 the U.S. Mint switched to a softer copper-alloy.  After 1983, pennies were minted from copper-plated zinc.  During 1983 both copper and copper-alloy pennies were minted, so you cannot be certain of their composition.  Therefore, 1983 pennies may have a hardness of either 2 or 3.  Pennies with a 1984 or younger date have a hardness of 2!  In order to use pennies as a hardness 3 standard, they must bear a mint date of 1982 or older.  I guess you could have two pennies in your hardness kit to test, one for H = 2 and another for H = 3.

Thanks Alex.  This is why I invested in a set of hardness points.

Julian

Basic Crystallography
by Albert M. Hines



THE DIFFERING VIEWS OF GEORGIA



SATELLITE VIEW OF GEORGIA


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