The Port Ewen Formation of the Helderberg Group is subdivided into two members in the Silurian-Devonian outcrop belt in eastern New York. The lower member is here named the Lake Katrine Member. It consists of dark-gray to brown weathering, fissile to hackly, burrow mottled, nonresistant, platy claystone, mudstone, and shale with bioclastic debris and coarse-grained carbonate at the base. Transitionally overlies the Alson Formation; underlies the East Kingston Member of the Port Ewen. Thickness at type section is 6 m. Age is Early Devonian.
Source: GNU records (USGS DDS-6; Reston GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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