Ellsworth Schist is of Late Proterozoic to Ordovician age. Islesboro Formation is considered a distal facies of North Haven Greenstone, Ellsworth Schist, and schist at Columbia Falls (eastern coastal ME). Consists of interbedded grayish-green phyllite and white to gray, siliceous, feldspathic siltstone (Berry and Osberg, 1989).
Source: GNU records (USGS DDS-6; Reston GNULEX).
Age of Ellsworth Schist changed to Cambrian. Pb-U date on zircon from tuff within Ellsworth is 509+/-2 Ma (R.D. Tucker, written commun., 1995). Rb-Sr whole-rock age is 499+/-15 Ma (recalculated from Brookins, 1976). Age of Castine Volcanics, which contains clasts of Ellsworth, may be as old as Early Ordovician (Ruitenberg and others, 1993), thus indicating an earlier age for Ellsworth.
Source: GNU records (USGS DDS-6; Reston GNULEX).
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