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Section 2. Bed 03. East-facing escarpment, Franklin Mountains

El Paso County, Texas
Directions
Next site in TexasHitt Canyon Prospect · 1 mi

Can I collect here?

Pro
See who owns this land and whether it is claimedPro shows the owner, the claim on this spot and every claim within a mile.
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Based on our latest records, with claims updated from the BLM on Oct 3, 2026. Land and claims can change quickly, so check before you go.

Minerals on record here

1 mineral

Recorded here: fossil.

1 miHitt Canyon ProspectAzurite, bornite, chalcopyrite +82 miVinton Canyon, Franklin Mountains, phylloid-algal horizonFossil4 miEl Paso MineCassiterite, fluorite, limonite +8

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About Section 2. Bed 03. East-facing escarpment, Franklin Mountains

Section 2. Bed 03. East-facing escarpment, Franklin Mountains is a fossil collection site in El Paso, Texas, cataloged in the Paleobiology Database. Fossils here come from the Upham Formation, dated to the Edenian to Maysvillian (451–449.6 million years ago). The depositional environment is recorded as carbonate indet. The collection holds 1 recorded fossil occurrence.

Geologic setting

Formation
Upham
Geologic interval
Edenian to Maysvillian
Age
451–449.6 Ma
Depositional environment
carbonate indet.
Recorded occurrences
1
Locality notes

1.1 miles south of the State line, El Paso County, Texas

Records and references

Data: Paleobiology Database collection 10637 (CC BY 4.0) — view the source record

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Questions about Section 2. Bed 03. East-facing escarpment, Franklin Mountains

Can you collect at Section 2. Bed 03. East-facing escarpment, Franklin Mountains?

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 Section 2. Bed 03. East-facing escarpment, Franklin Mountains?

Fossil.

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Meteorite nearbyA 140.7 kg iron meteorite was found at Ysleta in 1914, 30 miles from here.

Source: Paleobiology Database.