Photograph of Bermuda grass harvester made by SCS Okla.7.

Photograph of a seriously gullied area just after fencing for wildlife. Trees are planted above gullies. No other treatment given.

Photograph of State Game Rangers supervisiong seining of fish from lakes about to go dry.

Photograph of water held in contour listing furrows the morning after a 3 1/4 inch rainfall.

Photograph of bird dogs at point on covey of birds in quail census of wildlife areas on Wm. Lafave farm.

Photograph of State Game Rangers supervisiong seining of fish from lakes about to go dry.

Photograph of 72 skins (69 opossum and 3 skunk) representing all but 39 of Walter Holloway's catch of fur bearers between Dec. 1 and Dec. 16, inclusive.

Photograph of Twenty-two rabbits taken from 90 gums by two farm boys, Ola Adams and Herman Towery. Gums set in woodland area on Burl Prentice farm

Photograph of a fence row and field border of sassafras, Rhus ambrosia, ulmus and chenopodium prior to winter grazing by farmer's livestock.

Photograph of bird dogs at point on covey of birds in quail census of wildlife areas on Wm. Lafave farm.

Photograph of a fence row and field border of sassafras, Rhus ambrosia, ulmus and chenopodium prior to winter grazing by farmer's livestock.

Photograph of "Wild Tribe" at point on single quail. Quail census being taken of wildlife areas on B. Prentice farm.

Photograph of 72 skins (69 opossum and 3 skunk) representing all but 39 of Walter Holloway's catch of fur bearers between Dec. 1 and Dec. 16, inclusive.

Photograph of Twenty-two rabbits taken from 90 gums by two farm boys, Ola Adams and Herman Towery. Gums set in woodland area on Burl Prentice farm

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.