Exploring Georgia's Natural History
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      • Coastal Plain Core Logs by Paul F. Huddlestun
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    • I, Periarchus (A Fossil's Tale)
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    • Georgiacetus Presentation; A Whale for Georgia
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    • An Introduction To Fossils; Presentation
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  • Meteorites
    • Did I Find A Meteorite?
    • Georgia's Lost Meteorite
    • Georgia's Witnessed Meteorite Falls
    • The Sardis Iron, Georgia's Largest Meteorite
  • 1: Georgia's Oldest Fossils; Archaeocyathids, At 513 Million Years Old
  • 2: Trilobites; 500 Million Years Ago
    • 2A; Murray County Stromatolites
    • 2B; A Trilobite Nest in Georgia
  • 3: Geologic Time
  • 4: Our Oldest Vertebrate?
  • 5: Georgia Before the Dinosaurs
    • 5A; Georgia’s Pennsylvanian Plant Fossils
    • 5B: Carpentertypus durhami, Georgia’s Giant Insect, 315 Million Years Ago
  • 6: 200 Million Years Ago
    • 6A: Birth of the Atlantic Ocean
  • 7: Cretaceous Georgia, Dinosaurs & more
    • 7A: Georgias Pterosaur
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    • 7D: Xiphactinus vetus
    • 7E: Side-necked turtles
    • 7F: Marine Reptiles
    • 7G: Dinosaurs in Georgia
    • 7I; The Blufftown Formation
    • 7L: Bill Montante's Mega "Gator" Tooth Discovery
    • 7K: The Pio Nono Formation
    • 7J: The Eutaw Formation
    • 7H: Deinosuchus schwimmeri in Recognition of Dr. David Schwimmer
  • 8: Suwannee Current, Gulf Trough, & Bridgeboro Limestone
  • 9: The Clayton Formation Report; By Hank Josey
    • 9A: The Georgia Turtle
  • 10: The Eocene; Georgia's Oldest Mammals
    • 10A: The Origins of Whales
  • 11: A Whale For Georgia
  • 12: Basilosaurids; The First Modern Whales
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    • 12F; Houston County, GA Basilosaurus to the Smithsonian
  • 13: Ziggy and The Museum of Arts & Sciences, Macon, GA
  • 14: Late Eocene
    • 14A: Eocene Fossils & Stratigraphy
    • 14B; Fossils, Impacts, & Tektites Dating the Clinchfield Formation
    • 14C: The Tivola Limestone
    • 14D: Twiggs Clay Vertebrates
    • 14F; Sandersville Limestone, By Hank Josey
    • 14E: Ocmulgee Formation Vertebrates
    • 14I: Dating Late Eocene Sediments
    • 14J: Georgia's Tektites; Georgiaites
    • 14K; Shell Bluff; Georgia's Most Historic Paleontology Site
    • 14L; Taylors Bluff, Paleo Paddling the Ocmulgee River
    • 14M; Eocene Terrestrial Mammals From Gordon, GA
    • 14N: Fossil Ridge, A Stratigraphic Study in Oaky Woods Wildlife Management Area
    • 14O; Georgia's First Entelodont
    • 14P: Historic Rich Hill
    • 14Q; Bibb County's Christy Hill, Clinchfield Formation Hilltop
  • 15: Early Oligocene
    • 15A: The Marianna Limestone
    • 15B; The Glendon Limestone
    • 15C: Undiffereniated Oligocene Residuum
    • 15D; Brissus bridgeboroensis; A New Echinoid Species From Georgia’s Bridgeboro Limestone
    • 15E: The Curious Steinkern Sea Biscuits of Red Dog Farm Road
    • 15F: Early Oligocene Gordian Knot
  • 16: Bonaire GA Entelodont
  • 17: The Whale Eating Shark
  • 18: Miocene Epoch; 23.3 to 5.3 Million Years Ago
    • 18A; Miocene Terrestrial Vertebrates
    • 18B; Paul Fell, Rockhouse Cave
    • 18C: The Marks Head Formation
    • 18D: Miocene Terrestrial Vertebrates of the Marks Head Formation
    • 18E: The Statenville Formation
    • 18F: South Georgia’s Dugong Metaxytherium calvertense
  • 19: Pliocene Epoch; 5.3 to 2.5 Million years Ago
    • 19A; Two Small Primitive Horses from Taylor County
  • 20: The Ice Ages; Pleistocene & Holocene Epochs
    • 20A; Clark Quarry's Mammoths & Bison
    • 20B: Pleistocene Vertebrate List
    • 20C: Georgia’s Eolian Dunes
    • 20D: Georgia’s Carolina Bays
    • 20E: Late Pleistocene Significant Events
    • 20F: Southeastern Thermal Enclave
    • 20G; Diamond Back Terrapins
    • 20H; A Kaolin Mine Beaver Dam
    • 20I; Pleistocene Vertebrate Fossils On Georgia’s Piedmont
    • 20J; Watkins Quarry Pleistocene Vertebrates, Glynn County, GA
  • *NEW* 20K: Pleistocene Vertebrates from Coastal Georgia
  • 21: Humans in Georgia
  • 22: Geology of the Coastal Plain, 1911
    • 22A: 1911 Cretaceous Fossil Locations
    • 22B: 1911 Eocene Fossil Locations
  • 23: Coastal GA Locations (1957)
  • 24: Needed; The Georgia Geologic Survey
  • Building This Site
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Georgia Meteorites 
Did I Find A Meteorite?
 
By
Thomas Thurman
Filed; 24/April/2022
​

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​First of all, does it stick to a magnet? Yes? Still, you should accept the fact that you probably did not find a meteorite, There is a great deal of naturally occurring iron in Georgia, much of it is still pure enough to stick to a magnet.
 
However, just to be sure, let’s continue with the observations and test procedures below. If your find passes a magnet, bright scratch, & nickel test, (#3, #5, & #7) contact me for further guidance. Thomas Thurman; GeorgiasFossils@aol.com
 
It did not stick to a magnet? It’s probably not a meteorite. Even most stony meteorites have enough iron content to stock to a magnet.


Meteorites fall into three broad classifications
  • Irons
  • Stones
  • Stony-Irons
As we've discussed, there is plenty of naturally occurring iron in Georgia so a metal detector is not helpful. Also, three centuries of habitation by an iron using civilization have left many not-meteorites in the soil for us to find.
​Can your find be explained by naturally occurring iron minerals? Our natural terrestrial iron will almost always be found with sand, encrusted in sand, and often with sand inclusions. If you see sand included on your find, it is probably not a meteorite. If there is sand inside your find, it is not a meteorite.
 
There is one large, confirmed Georgia meteorite which had been buried for so long that it became encrusted with sand on the exterior as it weathered. This is the famous Sardis Iron, Georgia’s largest meteorite. But it is important to note that there was no sand inside the meteorite. So, let’s continue to the tests below.
​#1; Context
Does your find match the rocks of the local terrain?
Use a hammer and break open other local rocks and critically compare them to your find. Meteorites are never abundant in any local area.
 
#2; Crust
There will often be a fusion crust on the surface. This is typically a black coating. There may also be dimples on the surface, little pits the size of a fingertip.
 
#3; Magnet Test
All irons will respond strongly to a magnet.
The vast majority of stones contain enough iron to respond to a magnet.
Does your find respond to a magnet?
 
#4; Inclusions or veins?
There will often be metallic inclusions surrounding silicate bodies, possibly rounded bodies. Do you see thin black veins?
 
#5; Bright Scratch
Fresh scratches on an iron meteorite will be bright, like bare metal or the color of a 5 cent coin. Fresh scratches on terrestrial iron will be dark, rust colored. If you get a bright scratch, polish a small spot with a whetstone, or fine file, is the polished spot bright?
 
#6; Is the iron softish?
Meteoritic iron is malleable, meaning it will bend or is on the soft side. You can dent it.
Natural terrestrial and man-made irons are both brittle, they will break instead of bend.
 
#7; Nickle
Iron meteorites are fairly rich in the metal nickel.
Terrestrial & manmade iron is nearly devoid of nickel.
Nickel test kits are available at Walmart and pharmacies. Some people are allergic to the nickel found in inexpensive jewelry. Such test kits are readily available. Test for your find for nickel, if the test is positive, test again. If your find tests positive for nickel three times in a row, then have it looked at by someone with the experience to confirm it.

I would be happy to assist in getting you in touch with someone who can help; Thomas Thurman; GeorgiasFossils@aol.com