Exploring Georgia's Natural History
  • Home: Georgias Fossils
  • 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: Georgia's Oldest Vertebrate?
  • 5: NW Georgia, 488 to 300 million years ago
    • 5A; Georgia’s Pennsylvanian Plant Fossils
    • 5B: Carpentertypus durhami, Georgia’s Giant Insect, 315 Million Years Ago
    • 5C: Mississippian Trilobites in Northwest Georgia Describing the New Species Australosutura georgiana
    • 5D: Crinoids & Blastoids Of Northwest Georgia
    • 5E; Fossil Locations of Northwest Georgia
    • 5F: Pennsylvanian Plant Fossils of NW Georgia
    • 5G; Ordovician Invertebrates of Northwest Georgia
    • 5H: Trace Fossils in NW Georgia’s Metamorphic Rock
  • 6: 200 Million Years Ago
    • 6A: Birth of the Atlantic Ocean
  • 7: Cretaceous Georgia, Dinosaurs & more
    • 7A: Georgias Pterosaur
    • 7B: So Many Sharks
    • 7C: Coelecanths
    • 7D: Xiphactinus vetus
    • 7E: Side-necked turtles
    • 7F: Marine Reptiles
    • 7G: Dinosaurs in Georgia
    • 7H: Deinosuchus schwimmeri in Recognition of Dr. David Schwimmer
    • 7I; The Blufftown Formation
    • 7J: New Species of Cretaceous Flowers Reported From Crawford County
    • 7K: Field Trip, Chattahoochee River Valley 1980
    • 7L: The Eutaw Formation
    • 7M: The Pio Nono Formation
    • 7N: Plant Fossils of Crawford County, GA
    • 7O; 1914 Report Georgia Plant Fossils From the Upper Cretaceous
    • 7P: Bill Montante's Mega "Gator" Tooth Discovery
  • 8: Suwannee Current, Gulf Trough, & Bridgeboro Limestone
  • 9: 60 million years ago, The Paleocene's Clayton Formation, A Report; By Hank Josey
    • 9A: The Georgia Turtle
    • 9B; Sassafras Hill Quarry Huber Formation Plant Fossils in Kaolin
  • 10: The Eocene; Georgia's Oldest Mammals
    • 10A: The Origins of Whales
  • 11: A Whale For Georgia
  • 12: Basilosaurids; The First Modern Whales
    • 12A: Basilosaurus cetoides
    • 12B: Basilotritus
    • 12C: Cynthiacetus (Revised)
    • 12D: Chrysocetus
    • 12E: The Redmond Mandible of Albany Ga
    • 12F: The Tivola Whale; From Houston County 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
    • 14C1: Oldest Oreodont in the Southeast & Georgia's first!
    • 14D: Twiggs Clay Vertebrates
    • 14E: Ocmulgee Formation Vertebrates
    • 14F; Sandersville Limestone, By Hank Josey
    • 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
    • 14R: Browns Mount, The Fall Line, Elevations, Uplifts, & Native Middle Georgians
  • 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: Georgia’s 13 Million Year Old Dugong Metaxytherium calvertense
    • 18G: Gastropod Gulch, Julia Gardner, & Miocene Invertebrates In Decatur County
    • 18H; Bony Bluff, Rocky Ford, Echols County In Southernmost Georgia
  • 19: Pliocene Epoch; 5.3 to 2.5 Million years Ago
    • 19A: Two Small Primitive Horses from Taylor County Advance the Science of Georgia Geology
  • 20: The Pleistocene & Holocene Epochs, The Ice Ages
    • 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
    • 20K: Pleistocene Vertebrates from Coastal Georgia
    • 20L; Sandy Run Creek Core, Warner Robins, Houston County, GA
    • 20M: Bone Bed, Pleistocene, Coastal Georgia
    • 20N: Caribou & Elk Fossils from Georgia & Alabama
    • 20O; Tapir Veroensis, Walker County, Late Pleistocene
    • 20P; Ladds Pleistocene Vertebrates, Bartow County, GA
  • 21: Humans in Georgia
  • 22A: Echinoids of Georgia, Cenozoic Era (Sand Dollars & Urchins)
    • 22B: Echinoids of Georgia, Cenozoic, By County
  • 23A; Exploring the Paleontology of Southernmost Georgia
    • 23B; Seminole County
    • 23C: Decatur County Fossils & Natural History
    • 23D: Grady County Blowing Caves, Forest Falls, Fossils & Natural History
  • 24: Georgia's Meteorites
    • 24A: Did I Find A Meteorite?
    • 24B: Georgia's Lost Meteorite
    • 24C: The Sardis Iron, Georgia's Largest Meteorite
  • 25: Dr. Burt Carter, Georgia Southwetsern, Professor Invertebrate Paleontologist, Emeritus
    • 25A; Burt Carter, Uniformitarianism
    • 25B; Burt Carter, Inclusions
    • 25C; Burt Carter, Superposition
    • 25D; Burt Carter, Principal of Horizonality
    • 25E, Burt Carter, Cross Cutting
    • 25F; Burt Carter, Deep Time
    • 25G; Burt Carter, Fossil Succession
  • 26: Paul F. Huddlestun Coastal Plain Core Logs
    • 26A: Late Eocene & Older... Coastal Plain Stratigraphy
    • 26B: Gulf Trough Cores, Colquitt County, by Paul Huddlestun
    • 26C; Washington County Core Logs By Paul Huddlestun
    • 26D: Coastal Plain Core Logs by Paul F. Huddlestun
  • 27: Science, Georgia Research
    • 27A: Coastal Plain Correlation Chart
    • 27B: Physiographic Map of Georgia
    • 27C: Collections & Stewardship of Georgia’s Fossils
    • 27D: Needed; The Georgia Geologic Survey
    • 27E: GA County Localities, Houston County
    • 27F: Trace Fossils on the Coastal Plain
  • *NEW* 27G: Georgia’s Decapod Fossils
  • 28: Educational Matetrial For Georgia Classrooms
    • 28A: Oaky Woods Stratigraphy, PowerPoint
    • 28B: Fossils of Oaky Woods
    • 28C: I, Periarchus (A Fossil's Tale)
    • 28D: The Tivola Whales (April 2023 talk to the Mid-Georgia Gem & Mineral Society)
    • 28E: Georgiacetus Presentation; A Whale for Georgia
    • 28F: My Field Kit; What You Need In The Field
    • 28G: Meet Crassostrea gigantissima, Georgia's Historic Giant Oyster
    • 28H: The Natural History & Fossils Record of Houston County, GA
    • 28I: Evidence for Evolution in Georgia's Fossil Record... A look at Teeth
    • 28J: Georgia's State Fossil; Shark Teeth
    • 28K; An Introduction To Fossils; Presentation
    • 28L: Library & School Presentations
    • 28M: Georgia's Paleontology For Georgia's Classrooms
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24A: 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; [email protected]
 
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; [email protected]