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The Lye Brook Wilderness, in the Green Mountains of Vermont is underlain by gneisses, quartzites, schists, and amphibolites of Precambrian to Ordovician age. A mineral-resource survey determined that only one commodity, quartzite, is present in large quantities and could be a source of dimension stone or crushed stone. Although an anomalously high radioactive area occurs within the Precambrian basement, geochemical studies indicate little promise for the occurrence of significant uranium mineralization or for the occurrence of other mineral or energy resources within the wilderness,
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LYE BROOK WILDERNESS, VERMONT.
Geological Survey Professional Paper (United States)