Stratigraphic succession in Middlebury synclinorium in north-central part of Glens Falls quad consists of (ascending) Late Proterozoic Dalton Formation and Pinnacle Formation, Lower Cambrian Cheshire Quartzite, Lower and Middle Cambrian dolomites (Rutland Dolomite, Dunham Dolomite as used by Cady (1945), Winooski Dolomite) with minor quartzite (Monkton Formation), and Upper Cambrian Danby Formation. Middlebury synclinorium is considered a parautochthonous shelf sequence.
Source: GNU records (USGS DDS-6; Reston GNULEX).
On the correlation chart for Precambrian rocks of the conterminous United States, the Pinnacle Formation in the northern Laurentian Appalachians is shown to be of Late Proterozoic and Early Cambrian age.
Source: GNU records (USGS DDS-6; Reston GNULEX).
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