Keith, Arthur, 1924, Cambrian succession of northwestern Vermont: Vermont Geological Survey [Report of the State Geologist], 14th, p. 105-136., Also issued in Amer. Jour. Sci., 5th ser., v. 5, no. 26, p. 97-139, 1923.
Pg. 137, footnote. Missisquoi formation is here applied to thin-bedded upper part of Milton dolomite as defined by me in 1923. [See 1924 entry under Milton dolomite.]
Source: US geologic names lexicon (USGS Bull. 896, p. 1387).
Pg. 137-138, 197-202. Missisquoi formation. [Describes the Upper Cambrian fossils from thinly bedded limestone and conglomeratic strata exposed in gorge of Missisquoi River at Highgate Falls (at Highgate village, St. Albans quadrangle), which were named Missisquoi formation by Keith.] "Fauna resembles that of Hoyt limestone."
Source: US geologic names lexicon (USGS Bull. 896, p. 1387).
Pg. 266-268. †Missisquoi schist. Introduced Mill River conglomerate to replace this name, which is preoccupied by Missisquoi schist of Richardson, an Upper Cambrian formation on east side of Green Mountains, Vermont.
Source: US geologic names lexicon (USGS Bull. 896, p. 1387).
Pg. 1053. †Missisquoi formation. Beds termed Missisquoi by Keith (1924) are now referred to Gorge formation (new). Term Missisquoi preoccupied.
Source: US geologic names lexicon (USGS Bull. 1200, p. 2528-2529).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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