Coombs limestone member, at the top of the Islesboro formation in the Penobscot quad, southern ME, is chiefly shaly or quartzitic limestone, but in three localities is represented by fairly pure limestone. Thickness 7 to 100 ft. Underlies Battie quartzite. Unit is assigned a Cambrian(?) age.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Simplified stratigraphic column for the Islesboro-Rockport belt in eastern ME shows (ascending) Precambrian rocks of Gilkey Harbor, Islesboro Formation, Coombs Limestone, Cambrian Rockport Quartzite and Megunticook(?) Formation. Coombs is described as thinly intercalated quartz-plagioclase-biotite-diopside granulite and calcite marble. Precambrian age and formational status of the Coombs agrees with the usage presented on the 1985 State map of ME.
Source: GNU records (USGS DDS-6; Reston GNULEX).
Previously, all carbonate rocks in Isleboro Formation were called Coombs Limestone Member by Smith and others (1907). Because carbonate sequences within Islesboro Formation have different stratigraphic positions, variable thickness and lithology along strike, and may resemble each other locally, continued use of the name Coombs Limestone Member is unwarranted. Some of the carbonate rocks are now assigned to Seven Hundred Acre Island Formation (new name).
Source: GNU records (USGS DDS-6; Reston GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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