Stratford Hall Cliffs (Potomac, VA)
The Virginia counterpart to Maryland's Calvert Cliffs — towering Miocene exposures along the Potomac at Stratford Hall. Public access is by paid plantation entry only, but the beach below produces exceptional Calvert and Choptank Formation teeth.
Event timeline
Calvert Cliffs Spring Freeze-Thaw Erosion Window
endedLate winter freeze-thaw cycles destabilize the Chesapeake Group cliffs. March–early May historically produces the most fresh fall material on the beaches at Brownie's, Matoaka, and Westmoreland.
Walk the narrow beach below the cliffs at low tide. Search the swash zone and recently slumped material; do not dig into or undercut the cliffs. Best after winter storms.
Stratford Hall Plantation charges admission and provides the only legal cliff-base access. Strict 'no-dig' policy on the cliffs themselves; beach surface collecting is allowed.
Surface collecting only on plantation property with paid admission. Removing material from the cliff face is prohibited.
- Falling cliff debris
- Rising tide trapping you against the bluff
- Sun exposure
- Time your visit for the lowest tides — Stratford's beach narrows fast
- Look for slumps from recent rain; freshly fallen blocks weather out teeth quickly
- Bring a small mesh sifter for the gravel pockets
Shark teeth findable here
Trophy = headline find · Rare = real score · Uncommon = some trips · Common = most trips.
Also findable here
The beachcomber's bonus round — what else the geology gives up.
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