Pg. 29, 31, pl. 2. Hercules Tower sandstone in Lutie member of Theodosia formation. A massive red to reddish-brown medium-grained friable sandstone about 10 feet thick. Occurs near middle of Lutie and is separated from overlying Pocket Hollow oolite (new) by black and white chert and beds of finely crystalline dolomite and "cotton rock". Recognized in southern Missouri and northern Arkansas. Age is Early Ordovician.
Well exposed on MO Highway 125 south of Brush Creek about midway between village of Hercules and Hercules fire lookout tower, Taney Co., MO.
Source: US geologic names lexicon (USGS Bull. 1200, p. 1738).
Pg. 131. Cullison (1944, p. 29) proposed "Hercules Tower sandstone" for a prominent sandstone within his Theodosia formation. The sandstone is well exposed on Missouri Highway 125 south of Brush Creek about midway between the village of Hercules and the Hercules fire lookout tower, Taney County, Missouri. This sandstone is usually referred to today as the "Swan Creek sandstone" of the Cotter Dolomite. Age is Ordovician (Ibexian).
Source: Publication.
Pg. 3-4. [In the Ozark Plateaus region of Arkansas, Cullinson's "Hercules Tower sandstone" in Lutie Member of Theodosia Formation is not differentiated from the Early Ordovician Jefferson City and Cotter formations. The "cotton rock" (=Cullinson's Theodosia) is included in the Cotter.]
Source: Interpreted from publication.
For more information, please contact Nancy Stamm, Geologic Names Committee Secretary.
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