Pg. 55 (fig. 1), 57-58. Angell member of Ballard formation of Meade group. Name applied to sand, gravel, and cobble member at base of Ballard formation. Thickness about 7 feet. Underlies Missler member; overlies Rexroad formation. Age is Pleistocene (Nebraskan).
Type section: Sanders gravel pit, in SE/4 NW/4 sec. 7, T. 32 S., R. 28 W., Meade Co., southwestern KS. Name from old Angell Schoolhouse which was located in southeast corner of NE/4 sec. 31, T. 32 S., R. 29 W.
Source: US geologic names lexicon (USGS Bull. 1200, p. 100).
Zakrzewski, R.J., 1975, Pleistocene stratigraphy and paleontology in western Kansas; The state of the art, 1974: University of Michigan, Museum of Paleontology Papers on Paleontology, no. 12., Claude W. Hibbard Memorial Volume, no. 3
Pg. 122 (fig. 1), 124 (fig. 2), 125 (fig. 3), 126. Angell Gravel Member of Ballard Formation. Lies below Missler Silt Member of Ballard Formation. Deposits interpreted to represent pre-Nebraskan cool interval. Age is Pliocene (Blancan NALMA); Plio-Pleistocene boundary placed at base of Irvingtonian NALMA (base of Nebraskan-Aftonian), = 1.8 Ma.
Source: Publication.
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