The base of the Kinzers Formation is primarily a dark-brown shale. The middle is a gray and white spotted limestone and, locally, marble having irregular partings. The top is a sandy limestone which weathers to a fine-grained, friable, porous, sandy mass.[2]
^ abStose, G.W., and Jonas, A.I., 1922. The lower Paleozoic section in southeastern Pennsylvania, Washington Academy of Sciences, Journal v. 12, no. 5, p. 358-366 [1]
^Berg, T. M., Edmunds, W. E., Geyer, A. R., and others, compilers, 1980, Geologic map of Pennsylvania: Pennsylvania Geological Survey, 4th ser., Map 1, 2nd ed., 3 sheets, scale 1:250,000.
^Resser, C.E. & B.F. Howell. 1938. Lower Cambrian Olenellus zone of the Appalachians. Bulletin of the Geological Society of America 49: 195-248, 13 pls. [2]
^Rigby, J. Keith, 1987.
Early Cambrian sponges from Vermont and Pennsylvania, the only ones described from North America. Journal of Paleontology, Volume 61, Issue 3, May 1987, pp. 451-461
DOI: https://doi.org/10.1017/S0022336000028638
Upper Warren, Lower Warren, Speechely Stray, Speechely, Balltown A, Balltown B, Balltown C, Sheffield, First Bradford, Second Bradford, Third Bradford, Kane