This article contains a list of fossil-bearing stratigraphic units in the state of Vermont, U.S.
Phalagnostus is a genus of small trilobites, in the order Agnostida. It lived during the Middle Cambrian, in what are now Canada, China, the Czech Republic, Denmark, England, France, the Russian Federation, Wales, Sweden, and possibly the United States (Vermont). The headshield is almost entirely effaced and wider than the tailshield. The pygidium is also very effaced, but the ovate pygidial axis is well defined and a border furrow is also present.
The Valcour Formation is a geologic formation in New York and Vermont. It preserves fossils dating back to the Ordovician period.
The Crown Point Formation is a geologic formation in New York and Vermont. It preserves invertebrate fossils dating back to the Ordovician period. Notable fossiliferous localities within the Crown Point Formation include quarries in the towns of Panton and Isle La Motte, Vermont.
The Day Point Formation is a geologic formation in New York and Vermont. It preserves fossils dating back to the Ordovician period.
The Highgate Formation is a geologic formation in Vermont. It preserves fossils dating back to the Ordovician period.
The Gorge Formation is a geologic formation in Vermont. It preserves fossils dating back to the Cambrian period.
The Monkton Quartzite is a geologic formation in Vermont. It preserves fossils dating back to the middle of the Cambrian period.
The Parker Slate is a geologic formation in Vermont. It preserves fossils dating back to the Cambrian period.
The Skeels Corner Slate is a geologic formation in Vermont. It preserves fossils dating back to the Cambrian period.
The St. Albans Shale is a geologic formation in Vermont. It preserves fossils dating back to the Cambrian period.
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