Flathead formation. Divided into Flathead shales above and Flathead quartzite below. The shales are soft, green, shaly beds interlaminated with thin beds of glauconitic limestone; toward base are beds of very dark reddish-brown and green sandstone. Thickness of the shales 290 feet. Overlain by Trilobite limestone, the basal member of Gallatin formation. Fossils. Age is Middle Cambrian. [For description of the quartzite see Flathead quartzite.]
Named from exposures in Flathead Pass, northeastern corner Threeforks [Three Forks] quadrangle, MT.
Source: US geologic names lexicon (USGS Bull. 896, p. 738).
The use of Flathead in 3 senses being objectionable, the name has for many years been restricted to the quartzite, and the so-called "Flathead shales" have been combined with the overlying trilobite-bearing limestones and OBOLELLA-bearing shales (originally included in Gallatin formation) into a formation named Gros Ventre formation.
Source: US geologic names lexicon (USGS Bull. 896, p. 738).
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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