Windermere series named and divided into Toby conglomerate (base) and Horsethief formation (top) in this report. No type locality designated. Probably named for Windermere mining district, BC, CN in the Northern Rocky Mountain region. Unconformably overlies Purcell series [= Belt Series in US (Wilmarth, 1938, US geologic names lexicon, USGS Bull. 896, p. 1746)] and underlies Upper Cambrian Ottertail formation in the Windermere area. Is thought to be equivalent to Summit series of the International Boundary area, and to the Hector and Carrol Creek formations. Is of Late Precambrian age.
Source: GNU records (USGS DDS-6; Denver GNULEX).
Windermere series of Walker (1926) is adopted as the Windermere Group. Age is Precambrian Z.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
Age of the Windermere Group is [everywhere] revised from Middle(?) and Late Proterozoic to: Late Proterozoic based on isotopic age data (Sm/Nd whole-rock age of about 760 Ma) and regional stratigraphic relations.
Source: GNU records (USGS DDS-6; Menlo GNULEX).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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