Lisbon Valley

United States· UtahUnknown
Contained Copper
—
Average Grade
0.53%
Deposit Type
Sediment-hosted Stratiform Copper (SSC)
Discovery Year
—

Overview

Disseminated deposits adjacent to Lisbon fault; deposits|occur as veins in faults and disseminated bodies in sandstone adjacent to|the veins. Disseminated bodies are stacked at more than one stratigraphic|level.

Geological Context

Host Rock: Arkosic sandstone (Cretaceous)

Geological Province: 5021

Resources & Operations

Data Provenance

Source: USGS MRDS

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