From abstract: The Quinton-Scipio district includes about 450 square miles, mostly in Pittsburg County but partly in Haskell and Latimer Counties, Okla. The stratified rocks exposed at the surface in the district are the McAlester, Savanna, Boggy, Thurman, Stuart, and Senora formations, of Pennsylvanian age, and consist of alternating beds of shale and sandstone with some coal beds and a few beds of limestone less than 1 foot thick. The total thickness of these formations exposed in the district is between 3,000 and 3,300 feet. There are probably unconformities at the base of the Savanna sandstone and at the base of the Thurman sandstone. Overlying the Pennsylvanian formations in parts of the district are unconsolidated sand, gravel, and clay, which in part belong to the Gerty sand, a deposit in an abandoned Quaternary (?) river channel. Other unconsolidated deposits include sand on stream terraces and Recent alluvium.

From purpose and scope: The purpose of this report is to describe the hydrology of the Stigler area, based on the limited data collected since October, 1978.

From purpose and scope: The purpose of this report is to evaluate the water resources of an abandoned coal-mining area near McCurtain in Haskell County in Oklahoma coal field and to appraise the probably effects of reclamation on water-quality, based primarily on data collected from October 1980 to May 1983.