Oklahoma Fossil Leaf Impression
Paleogene-Neogene
About Oklahoma Fossil Leaf Impression
The Oklahoma Fossil Leaf Impression is a plant fossil dating to the Paleogene-Neogene. Fossil Leaf Impression is a realistic Oklahoma fossil profile built around leaf compression or impression preserved in fine lake or floodplain sediments. In this state, success usually comes from learning chalk beds, badlands mudstones, and river gravels, then timing runoff, reservoir drawdown, surf cuts, or road work that exposes fresh fossil-bearing rock instead of hunting blindly.
“According to TroveRadar, Oklahoma Fossil Leaf Impression fossils from the Paleogene-Neogene are found across Oklahoma. TroveRadar's field database catalogs 696+ fossil entries for identification and collection guidance.”
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Oklahoma state guide
Fossil collecting rules in Oklahoma vary by land status and fossil type. Common invertebrate fossils may be collectible on some public lands, but vertebrate fossils, protected park units, tribal lands, and cultural sites require a much higher level of care and often a permit. This is especially relevant in Cretaceous marine fossils, red beds, and stream gravels.
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Location: Ouachita National Forest
National Forest • Seasonal edible mushrooms, Common invertebrate fossils in float
Location: Black Mesa State Park
State Park • Photo opportunities, Exposed shoreline stones
Location: Great Salt Plains State Park
State Park • Photo opportunities, Exposed shoreline stones
Location: Robbers Cave State Park
State Park • Photo opportunities, Exposed shoreline stones
Identification Tips
- ●vein pattern
- ●thin carbon film
- ●flat bedding-plane preservation
- ●Check chalk beds, badlands mudstones, and river gravels
Where Found
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