Pg. 387, 416. Saddle Creek bed in Cisco division. Limestone, usually massive, light-gray, 6 to 12 feet thick. Underlies Camp Creek bed and overlies Waldrip bed in Colorado coal field of Texas. Is member of Cisco division. [Age is Pennsylvanian.]

Source: US geologic names lexicon (USGS Bull. 896, p. 1865).

Saddle Creek bed is finely exposed 1 to 2 miles south of mouth of Saddle Creek [McCulloch County, central Texas]. On north side of Colorado River it remains north of the river from north of mouth of Saddle Creek to northwest of Waldrip. [Age is Pennsylvanian.]

Source: US geologic names lexicon (USGS Bull. 896, p. 1865).

Pg. 136. Saddle Creek of Drake immediately underlies Pueblo formation. [Age is Pennsylvanian.]

Source: US geologic names lexicon (USGS Bull. 896, p. 1865).

Saddle Creek limestone (=Saddle Creek bed of Drake) is top member of Harpersville formation. [Many details.] [Age is Pennsylvanian.]

Source: US geologic names lexicon (USGS Bull. 896, p. 1865).

Pg. 18-42. Saddle Creek limestone (top member of Harpersville formation) consists of 2 or 3 beds 1 to 3 feet thick separated by shale. To north the Saddle Creek bed changes to calcareous sandstone. [Age is Pennsylvanian.]

Source: US geologic names lexicon (USGS Bull. 896, p. 1865).

Pg. 66 (fig. 1), 91. Saddle Creek formation of Pueblo group. Rank raised to formation and reallocated to the Pueblo here redefined, given group status and assigned to the Permian. [Expanded to include Waldrip Nos. 2 and 3 limestone beds of Plummer and Moore (1922).] Underlies Stockwether formation. Redefined Pennsylvanian-Permian boundary is placed at disconformity in Harpersville formation above Waldrip-Newcastle coal zone about 40 to 150 feet below Saddle Creek limestone.

Source: US geologic names lexicon (USGS Bull. 1200, p. 3376).

Sheet 2. Saddle Creek limestone member of Pueblo formation. Described in Colorado River Valley as limestone member of Pueblo formation. Consists of thin iiregular layers of brittle fine-grained blue-gray limetone 4 to 5 feet thick. Underlies Camp Creek shale member; overlies Waldrip shale member [rocks previously included in Saddle Creek formation by Cheney]. Age is Permian.

Source: Publication; US geologic names lexicon (USGS Bull. 1200, p. 3376).

Saddle Creek Limestone [unranked] at base of Pueblo Formation of Cisco Group. Fine-grained, thin-bedded, gray limestone, locally contains fossils. Thickness 2 to 10 feet, thickens northward. Lies below Camp Creek Shale [unranked] in Pueblo Formation and above Harpersville Formation of Cisco Group. Age is Early Permian (Wolfcampian).
Mapped in Brown, Callahan, Coleman, Shackelford, Stephens, and Throckmorton Cos., central northern TX.

Source: Publication.

Saddle Creek Limestone [unranked] at base of Pueblo Formation of Cisco Group. Fine-grained limestone interbedded with shale toward top, medium to thick beds in lower part, thin-bedded and flaggy at top, resistant, dark gray to light gray and light brownish gray, weathers light gray; forms scarp, cut out by sandstone near north edge of map sheet; fossils include crinoids, corals, fusulinids, brachiopods, and encrusting algae. Thickness 3 to 8 feet. Lies below Camp Creek Shale [unranked] in Pueblo Formation and above Harpersville Formation of Cisco Group. Age is Early Permian (Wolfcampian).
[Mapped in Brown, Coleman, and McCulloch Cos., central TX.]

Source: Publication.