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U. S. Highway 40 Roadcut, just west of Conococheague Creek at Wilson

Maryland
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Next site in MarylandAshton · 2 mi

Can I collect here?

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Based on our latest records, with claims updated from the BLM on Oct 15, 2026. Land and claims can change quickly, so check before you go.

Minerals on record here

1 mineral

Recorded here: fossil.

2 miAshtonSerpentine, steatite3 miSchemeompf’s old Quarry, top of a hill, west of Conococheague CreekFossil5 miUnit 2, Rose Hill Formation, North Mountain Section, MarylandFossil

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About U. S. Highway 40 Roadcut, just west of Conococheague Creek at Wilson

U. S. Highway 40 Roadcut, just west of Conococheague Creek at Wilson is a fossil collection site in Maryland, cataloged in the Paleobiology Database. Fossils here come from the Chambersburg Formation, dated to the Blackriveran (457.3–449.6 million years ago). The depositional environment is recorded as carbonate indet. Documented finds include Glyptorthis equiconvexa.

Geologic setting

Formation
Chambersburg
Geologic interval
Blackriveran
Age
457.3–449.6 Ma
Depositional environment
carbonate indet.
Recorded occurrences
1
Locality notes

Williamsport (15') Quadrangle.

Fossils found here

Glyptorthis equiconvexa
Rhynchonellata · Glyptorthidae

Records and references

Data: Paleobiology Database collection 164466 (CC BY 4.0) — view the source record

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Questions about U. S. Highway 40 Roadcut, just west of Conococheague Creek at Wilson

Can you collect at U. S. Highway 40 Roadcut, just west of Conococheague Creek at Wilson?

It depends on who owns the land and whether a mining claim covers it. BLM land usually allows hand collecting for personal use, national parks allow none, and private land needs the owner’s permission. Pro members see the owner and any claims at this spot.

What minerals are found at U. S. Highway 40 Roadcut, just west of Conococheague Creek at Wilson?

Fossil.

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Meteorite nearbyA 450 g iron meteorite was found at Emmitsburg in 1854, 30 miles from here.

Source: Paleobiology Database.