Lee Creek Mine, near Aurora, North Carolina, was one of the most important fossil shark localities in the world from the 1960s through the early 2000s. The mine itself is an active phosphate operation, and from its early years it released exceptional fossil material as a byproduct. Public collection access ended in 2009, which makes Lee Creek a finite supply in the contemporary market.
The Geology
The mine extracts the Pungo River Formation (Miocene) and the overlying Yorktown Formation (Pliocene). Both are marine sediments dense with vertebrate fossils. The Pungo River sits roughly 15 to 5 million years old; the Yorktown roughly 5 to 3 million years. The transition layer between the two has produced some of the most spectacular specimens in the locality’s history.
What Lee Creek Produced
The signature species is megalodon. Lee Creek megalodon teeth are noted for size, preservation quality, and a distinctive color palette of grays and charcoals with occasional warm undertones. Specimens above 6 inches in slant height are documented from the locality, and the proportion of large grade-A material in Lee Creek production was higher than at most other megalodon sites.
Beyond megalodon: extensive marine mammal material (early whales, dolphins, walruses), the great white ancestors C. hastalis and C. hubbelli, sand tiger sharks, mako teeth, and a wide range of bony fish material. The locality is also famous for producing the first identified Carcharodon hubbelli specimens, the transitional species between hastalis and the modern great white.
The Access History
For decades, the mine operator (then PCS Phosphate, later PotashCorp, now Nutrien) ran controlled public fossil-collecting events. Amateur and professional collectors paid a fee, brought tools, and worked the spoil piles for fossils. The arrangement produced an extraordinary volume of material that entered private and institutional collections worldwide.
The 2009 Closure
Public collection access ended in 2009 for liability and operational reasons. The mine continues to operate but no longer admits collectors. The result is that the Lee Creek market now relies on inventory accumulated before 2009: dealer holdings, private collections beginning to disperse, and estate dispositions of significant Lee Creek collections.
What This Means for Pricing
Lee Creek specimens command a meaningful premium over equivalent material from currently-accessible localities. A grade-A megalodon tooth from Lee Creek typically sells for 25% to 50% more than the same size and grade from Bone Valley, reflecting the supply constraint.
What to Look For
A reputable Lee Creek specimen comes with documentation that names the dig year or the original collector. Coloration is gray-to-charcoal; specimens labeled as Lee Creek but showing the warm tans of Bone Valley should be questioned. Preservation should be excellent — Lee Creek material was extracted from a relatively undisturbed sediment, and a Lee Creek specimen in poor condition is typically misattributed.
The Long Outlook
The Lee Creek market will continue to function on the inventory accumulated through 2009. As that inventory disperses over decades, prices for documented Lee Creek material will likely continue to rise relative to material from open localities. A high-quality Lee Creek specimen acquired today is a long-position holding for any serious fossil collection.