Meteorites Found in South Carolina: 7 Documented
South Carolina has 7 officially recognized meteorites — 2 witnessed falls and 5 finds. The largest, Ruff's Mountain (Iron, IIIAB — iron meteorite — nickel-iron metal), weighed 53.1 kg. The record here spans 127 years — from Bishopville in 1843 to Cordova in 1970.
Classification
Fell vs. found
South Carolina Meteorites
The full record
7 meteorites · exact coordinates in the map popups; entries marked “location withheld” are protected by the scientific record.
Reading the classifications
The most common meteorites — stony, with visible metal flecks. H = high iron content, L = low, LL = very low. The digit (3–6) says how much the parent asteroid heated it: 3 is the most pristine.
Primitive, carbon-bearing stones that predate the planets — some carry water-bearing minerals and amino acids. Fragile and rare on the ground.
Solid nickel-iron from the shattered cores of asteroids. Dense, magnetic, and the easiest meteorites to recognize — most of the biggest US finds are irons.
The showpieces: pallasites are gem-quality olivine suspended in polished metal, from the core-mantle boundary of destroyed asteroids.
Volcanic rocks from bodies large enough to melt — most trace to the asteroid Vesta; the rarest are from the Moon and Mars.
Frequently Asked Questions
How many meteorites have been found in South Carolina?
7 meteorites from South Carolina are officially recognized in the scientific record — 2 witnessed falls and 5 finds.
What's the biggest meteorite ever found in South Carolina?
Ruff's Mountain, a Iron, IIIAB (iron meteorite — nickel-iron metal) weighing 53.1 kg, found in 1844.
Can I hunt for meteorites in South Carolina?
On BLM-managed public land, casual collecting is legal without a permit: surface finds, up to 10 lb per person per year, personal use only. National parks prohibit all collecting, and on private land the meteorite belongs to the landowner. Always verify land status before hunting.
How do I know if a rock is a meteorite?
Quick field checks: meteorites are unusually dense, most attract a magnet (iron-nickel content), fresh ones have a thin black fusion crust, and many show regmaglypts (thumbprint-like depressions). Slag and magnetite are the common false alarms — our 60-second field test walks through all of it.
⚠️ Always verify current regulations, weather conditions, and access requirements before visiting any location. Information provided is based on community submissions and may not be current or accurate.
Coordinates are historical find locations from the scientific record, often approximate — not guaranteed collecting spots; verify land status and permissions before hunting. Source of record: Meteoritical Bulletin Database (Meteoritical Society).