Ladonia Fossil Park: Fossil Hunting in Fannin County, Texas
- Minerals reported
- 5
- Elevation
- 630 ft
The North Sulphur River channel at Ladonia cuts into Late Cretaceous marine beds that yield shark teeth, mosasaur teeth and bone, ammonites, and Exogyra oysters. The Upper Trinity Regional Water District operates the site as a free public fossil park, and what visitors find is theirs to keep. Mosasaur material is among the more common vertebrate finds. Reported finds include fossilized shark tooth, ammonite, mosasaur tooth, fossilized oyster, petrified wood. Below: coordinates, access notes, nearby spots, and trip-planning links.
Plan your visit
Generally open to casual rockhounding
- County
- Fannin County
- State
- Texas
- Coordinates
- 33.46335, -95.87786
Coordinates are approximate. Confirm the exact ground in the RockHoundR app, where land overlays show which agency manages the area.
Land & collecting status
Generally open to casual rockhounding
Most public-tagged spots sit on BLM, U.S. Forest Service, or other federal land where reasonable hand collecting of common rocks and minerals is allowed. Confirm posted rules and active mining claims before you dig.
Access note: The park moved in 2025 to its permanent site at 2242 FM 904, where FM 904 crosses the North Sulphur River downstream of Leon Hurse Dam, near the Baker Creek confluence. Operated free by the Upper Trinity Regional Water District, open dawn to dusk; gates close automatically in bad weather. The former temporary park upstream closed 3 March 2025 and is no longer accessible.
Public-land rules vary by agency, season, and field office. The RockHoundR app pulls live BLM, USFS, NPS, and tribal overlays so you can see exactly which agency manages the ground at this spot.
Geology at Ladonia Fossil Park
This spot sits on Wolfe City Formation, mapped as sandstone mudstone that formed roughly 72 to 66 million years ago. Sedimentary layers like these are where fossils are typically preserved, and fresh exposures after rain or in active cuts tend to produce best.
- Mapped unit
- Wolfe City Formation
- Age
- 72–66 Ma (Late Cretaceous)
- Rock types
- sandstone mudstone
- Elevation
- 630 ft
Geologic mapping via Macrostrat and the underlying state geological survey maps (CC BY 4.0). Bedrock at the surface can vary within a mapped unit.
Today's weather
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The app shows live weather, recent rain, and a daily rockhounding score for Ladonia Fossil Park.
Get the appSources & verification
Spot details combine the public RockHoundR location dataset, normalized mineral labels, agency land-status checks in the app, and community submissions. Coordinates are approximate until verified in the field.
State guidance last verified:
- Texas Parks and Wildlife Department
- Bureau of Economic Geology, Texas geology
- Big Bend National Park, Rules
- Community submissions reviewed against published agency rules
Found at Ladonia Fossil Park
Each name opens all spots that produce that material; the encyclopedia link opens the full ID and field guide.
Nearby rockhounding spots
Other rockhounding spots within driving distance of Ladonia Fossil Park.
- Sides of creekEllis County, Texas · 93 mi awayPyrite
- S side of US 287Ellis County, Texas · 93 mi awayFossil Leaf Print
- General AreaEllis County, Texas · 95 mi awayFossilized Shark Tooth
- Lyndon B. Johnson National Grassland (Black Creek Lake)Wise County, Texas · 103 mi awayFossilized Oyster, Agate, Petrified Wood
- General AreaWise County, Texas · 104 mi awayPyrite Cube
- General Area N.E. Lake BridgeportWise County, Texas · 115 mi awayFossil
Across the state line from Ladonia Fossil Park
Ladonia Fossil Park is close enough to the Texas border that the next-closest rockhounding spots are in a neighboring state. Worth knowing if you are already on the road.
- AntlersPushmataha County, Oklahoma · 57 mi awayGreen Quartz
- Tenmile CreekPushmataha County, Oklahoma · 63 mi awayGrahamite
- AtokaAtoka County, Oklahoma · 68 mi awayNovaculite, Chert
- LehighCoal County, Oklahoma · 75 mi awayManganese
Ladonia Fossil Park FAQ
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More rockhounding in Texas
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