Locations

The self-styled Shark Tooth Capital of the World. A long, dark-sand beach where the Hawthorn and Peace River formations are eroded constantly offshore - every wave delivers fresh teeth.

Caspersen's quieter southern cousin. Same Peace River geology offshore, fewer crowds, surprisingly productive at low tide.

North Florida's secret. Coquina ledges offshore release dark gravel along Ponte Vedra's beaches. Patient walkers find megalodons.

Florida's northeasternmost barrier island. The north end (Fort Clinch SP / inlet jetty area) reworks shell hash into surprising fossil hauls.

South Florida sleeper hit. Anastasia coquina ledges offshore release teeth along Carlin Park and Coral Cove. Less famous = less competition.

Florida's legendary fossil river. Ice-age megafauna mixed with Miocene sharks: mammoth, mastodon, giant ground sloth, megalodon - all in one screen.

Central Florida's phosphate mining belt — the world-famous fossil bed that supplies most of the megalodon teeth on the dealer market. Direct mine access is industrial-only, but reclaimed lands, fossil parks, and creek tributaries downstream of the district are open to hunters.

The classic North Florida beach hunt — Ponte Vedra and the adjacent Mickler's Beach feed off the same offshore Hawthorn-derived phosphate horizon. Mickler's gets the press but Ponte Vedra (just north) is quieter and just as productive after a NE blow.

St. Augustine Beach and the long strand of Anastasia State Park sit on the same offshore Hawthorn-source phosphate horizon as Mickler's and Ponte Vedra. Less famous, more shoreline to spread out, and a state-park gate keeps weekend crowds manageable.

Quiet Georgia option. Limited but real - Pleistocene-reworked finds, especially after the 6+ ft tidal swings the GA coast routinely hits.

South Carolina's classic. The Edisto and Ashley formations offshore drop teeth right onto the beach. The state park stretch is the easiest haul.

Charleston's surf town. Erosion at the Washout area exposes shell hash full of teeth - best on a low spring tide.

A polished resort coast hides genuine fossil hash. The mid-island beaches see tidal swings that move serious sand and reveal teeth.

The historical 'megalodon capital of the world.' Summerville and the surrounding Cooper-Ashley-Edisto river drainages have produced more giant teeth than any other US locality. Most prime ground today is private; legal hunts run via licensed guides on the rivers themselves.

The legendary mile-long stretch of the Cooper River north of Charleston that has produced more giant megalodon teeth per dive than almost anywhere on Earth. Visibility is near-zero — divers fan the gravel bottom by feel ("braille diving"). Strictly hobby-permit + boat + ideally guided; this is not a beach you walk up to.

The Grand Strand isn't famous for fossil beach hunting — but it should be. The same offshore phosphate horizon that feeds Cherry Grove and North Myrtle drops small black teeth onto the wrack line after every onshore blow. Best at the inlets (Cherry Grove channel, Murrells Inlet) where shell hash concentrates.

Trucked-in spoil from the world-famous Lee Creek phosphate mine. A hill of Miocene & Pliocene treasure, free and open to the public - and it gets refreshed.

Quiet barrier island that punches above its weight. Pliocene-Pleistocene shell hash washes up along the south end, with consistent finds in winter.

Topsail Island's main town. Same Yorktown-fed gravel, easier access, lots of nearby food. Great family base.

Southport-area sleeper. Less famous than Topsail, less crowded. Patient walkers find good Hemipristis and small megs.

The most famous Miocene-Pliocene shark-tooth locality in the United States. Operated as a phosphate mine since the 1960s, Lee Creek produced the spectacular megalodon teeth that defined a generation of collectors. Public collecting ended in 2008. Today the Aurora Fossil Museum across the river is the legitimate way to engage with the deposit (already in our atlas).

A small urban creek that cuts through the Yorktown Formation as it winds through Greenville and East Carolina University. Green Springs Park is the most popular access point — locals and ECU geology students have been finding small Pliocene shark teeth in its gravel bars for decades. Teeth are typically 0.25–1 in (think tiger, sand tiger, mako, the occasional small meg) — this is a 'lots of small teeth' creek, not a trophy spot.

The wider, slower river that Green Mill Run drains into. The Tar–Pamlico cuts the same Yorktown Formation and exposes phosphate-rich gravel bars at low water. A small jon boat or kayak between Greenville and Washington gets you to bars that nobody walks to — and that means undisturbed teeth.

The Neuse cuts through the same Yorktown and Pleistocene marine deposits as the Tar–Pamlico, with broad gravel bars upstream of New Bern. Less famous, less worked, and very kayak-friendly.

The Cape Fear cuts Cretaceous Peedee Formation, Eocene Castle Hayne Limestone, and Miocene-Pliocene marine deposits before reaching Wilmington. Boat divers and kayakers find a wider age range of teeth here than anywhere else in NC — including occasional Cretaceous mosasaur and Squalicorax material.

The southernmost NC barrier island, just over the line from Little River SC. Same shelf-source phosphate-tooth wash as the Grand Strand, with much less foot traffic — especially the Bird Island Reserve walk at the west end.

Small Pungo River tributary creeks near Yeatesville cut directly through Pungo River and Yorktown Formation. A very local hunt — small teeth, no crowds, perfect after-rain creek walk for travelers staying in the Aurora area.

The most accessible window into the famous Calvert Cliffs. The Chesapeake Group cliffs erode constantly, dropping 10-18 million-year-old teeth into the surf at your feet.

A semi-private cliff stretch with day-pass access. Famous for prolific Hemipristis and the occasional sizable meg fragment.

Calvert County park with cliff exposures. Quieter than Brownie's, gentler walk-in. Great for first-time families.

The big public access. Two-mile hike each way through forest to a strict no-cliff-touch beach. Quiet and rewarding for those who walk in.

Paleocene unicorn. The Aquia Formation here yields ~60 million year old shark teeth - vastly older than Calvert. Striatolamia striata and goblin shark cousins.

Virginia's fossil-hunting flagship. Cliffs of the Calvert Formation drop Miocene treasure into the Potomac shore.

Type locality for the Yorktown Formation. The fossil shell hash here is so good it has its own shell mountain (Pliocene scallop reef!).

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.

The Calvert Cliffs reach between Plum Point and Scientists' Cliffs HOA — same Calvert/Choptank/St. Marys Miocene exposures as Calvert Cliffs State Park, but accessed from the north via Brownie's, Matoaka, and the (private) Scientists' Cliffs association beach. Listed here as the upper-cliff alternative for travelers staying on the Plum Point end of the bay.

An East Coast unicorn: a Cretaceous fossil creek in the woods. Mosasaur teeth, ancient sharks, and even rare amber - none of which need the ocean.

Middletown's family-friendly Cretaceous creek. Smaller than Big Brook but easier with kids. Same age, same star species.

Yes, the river is named after sharks. Shark River yields Eocene Manasquan-Formation teeth - a rare epoch on the East Coast.

Delaware's gem. Walking from the point northward yields Pleistocene-reworked teeth and the occasional surprise from the offshore deposits.

Alabama's best public Gulf beach for fossil hunters. Storm-cut shell hash and inlet bars occasionally throw Miocene shark teeth onto the sand.

Louisiana's best-known public beach for opportunistic fossil finds. Big Gulf storms strip the sand and briefly expose tooth-rich shell lines.

The classic public Late Cretaceous (Campanian) marine site in the US. Operated as a science center by Memphis Pink Palace Museum — fee-paid digs let you walk out with mosasaur teeth, Squalicorax, ammonites, and the famous aragonite-preserved shells of the Coon Creek Formation.

Texas's most dependable public beach for shark teeth. Frontal systems and longshore transport rework offshore lag into shell-heavy cuts and bars.

A legendary Texas beach for rolled fossils and artifacts. Big storms can turn McFaddin into one of the most diverse beachcombing beaches in the country.

North Texas's best beginner Cretaceous creek. Public access, easy wading, and a steady supply of shark teeth from the Western Interior Seaway.

One of the best public Cretaceous river systems in America. Fresh flood cuts reveal shark teeth, mosasaur material, and big marine reptile country.

The classic California Miocene site. Guided quarry access to the Round Mountain Silt still produces broad makos, tiger sharks, and the occasional megalodon.

California's most accessible public beach for shark teeth. Winter surf and cliff erosion rework Purisima and Santa Margarita material into the gravel.

Bakersfield's legendary Middle Miocene 'bonebed' — a single thin layer of the Round Mountain Silt that has produced more shark teeth, marine mammals, and reptile remains per square meter than almost any other site on Earth. The classic locality is the Ernst Quarries (already in our atlas as a separate dossier); this entry covers the broader formation.

A public Kansas classic where the Western Interior Seaway still shows through. Rain and runoff expose Cretaceous shark teeth in spillway gravels and eroding shale.

An Upper Cretaceous chalk locality in Dallas County, Alabama — classic Mooreville/Demopolis Chalk producing mosasaur, plesiosaur and Cretoxyrhina shark teeth. Access is private; landowner permission or organized university/club trips are the path in.

The Niobrara Formation Smoky Hill Chalk member exposed in the western Kansas badlands — the source of the most famous Late Cretaceous marine fossils in North America (Xiphactinus, mosasaurs, Squalicorax). Castle Rock is the iconic public landform; surrounding land is private and requires permission.

Classic Eocene London Clay coast where storm and cliff-fall windows can produce shark teeth and marine fossils.

Belgium's Rupelian and related marine units are famous for high-quality Oligocene shark material.

The yellow Pietra Leccese building stone of Italy's heel preserves a famous Miocene marine fauna — including Otodus megalodon. Outcrops appear in road cuts, quarries, and coastal cliffs around Lecce, Cursi, and Melpignano. Italian heritage rules govern collecting.

Cadzand-Bad and the Zeelandic beaches are Europe's friendliest hobbyist shark-tooth destination. Sand replenishment dredged from the North Sea floor delivers tens of thousands of small Miocene-Pliocene teeth onto the beach every summer. Walk barefoot, watch the swash, fill a vial.

The Eocene Fur (Mo-clay) Formation on Mors and Fur islands in the Limfjord is world-famous for exquisitely preserved fish, insects, and shark teeth in laminated diatomite. Local moler quarries and coastal exposures are accessible with respect for landowner rules.

Malta's iconic yellow Globigerina Limestone holds a Miocene marine fauna including Otodus megalodon teeth famously displayed at the Natural History Museum in Mdina. Pwales Beach and surrounding coastal exposures (Għar Lapsi, St Thomas Bay) are the classic in-situ contexts. Casual surface collecting tolerated; export restricted.

The European reference Miocene marine site, just south of Bordeaux. A protected geological reserve with public guided walks through Aquitanian and Burdigalian shell beds that yield small shark teeth, ray plates, and beautiful invertebrates.

Miocene shallow-marine cliffs running south from Lisbon along the Costa da Caparica beaches. After winter storms, small black teeth (sand tiger, mako, requiem) wash from cliff lag onto the wide tourist beaches — easy day trip from the city.

A world-famous phosphate basin with extraordinary Eocene marine vertebrate diversity, usually accessed through organized operators.

The active phosphate mining belt of central Morocco is the single largest source of fossil shark teeth on the global dealer market. Eocene Otodus obliquus teeth, mosasaur jaws, and basilosaur whale bones move out of Khouribga and Ouled Abdoun by the truckload. Mines are operated by OCP and not open to casual collecting.

A UNESCO World Heritage Site in Egypt's Western Desert preserving the most important fossil record of early whale evolution — the basilosaurid 'walking whales.' Shark teeth (Otodus, Carcharias) co-occur in the Late Eocene Birket Qarun Formation. Strictly heritage-only: visit, learn, photograph; no collecting.

A world-class Pliocene marine bone-bed about 100 km north of Cape Town. The site is run as a public museum and research park; guided tours walk you through an in-situ excavation of one of the richest 5-million-year-old terrestrial-marine assemblages on Earth, including extinct sharks, sabretooth cats, and short-necked giraffes.

The Tunisian counterpart to Morocco's Khouribga — Eocene phosphate deposits worked by the Compagnie des Phosphates de Gafsa. Same geological story (Tethyan upwelling), same kinds of Eocene-Paleocene shark teeth. Access is via mining-company arrangement and university paleontology programs only.

Atacama coastal formations with famous Neogene marine vertebrate deposits and documented large shark teeth.

The Atacama desert south of Lima preserves one of Earth's richest marine vertebrate fossil records. The Pisco Formation has produced Carcharocles megalodon, the leviathan whale, and Carcharodon hubbelli — the proposed great-white ancestor. Collecting requires a Peruvian government permit and partnership with Peruvian institutions.

The cliffs around Puerto Madryn and the Valdés Peninsula expose the Puerto Madryn Formation — a late Miocene shallow-marine unit famous for trophy megalodon teeth, Otodus chubutensis, and abundant marine mammal bone. Access is via guided paleo-tours run from town.

A renowned Australian marine fossil coast with Miocene-Pliocene shark and marine vertebrate material in wave-worked lag zones. The famous Beaumaris fossil cliff produces Carcharodon lineage teeth, penguin bones, and dwarf-whale fragments. Companion site to the Surf Coast's Jan Juc / Bird Rock — both are part of Victoria's classic shark-tooth itinerary.

Australia's classic shark-tooth coast. The Jan Juc Marl west of Torquay is a Late Oligocene marine unit famous for Carcharocles angustidens and the largest Miocene shark community Down Under. The eroding cliff base is a public foreshore — walk it at low tide.

A small Canterbury beach community an hour north of Christchurch sitting on the Pliocene Greta Siltstone — one of the Southern Hemisphere's best beach localities for shark teeth, including Carcharodon megalodon. A New Zealand Geopreservation Inventory site.

The Chichibu basin west of Tokyo exposes the middle-Miocene Chichibumachi Formation, the most accessible Asian site for shark teeth — including occasional megalodon. Best engaged via the Saitama Museum of Natural History and its public field walks; private quarry access is not allowed.

A modest Pacific entry: the Banderas Bay coast around Sayulita and Punta Mita produces small modern and Pleistocene shark teeth on storm wrack. Not a trophy site — a vacation-friendly addition to the atlas for travelers in the Puerto Vallarta area.

Late Cretaceous Haslam Formation shales exposed along Vancouver Island streams and shorelines (Trent River, Brannen Lake). Small Cretaceous shark teeth, ammonites, and the occasional mosasaur fragment — Canada's most accessible marine Cretaceous public hunt.