Script from the WBAP-TV/NBC station in Fort Worth, Texas, relating a news story.

Client card describing work completed at the Roman Bronze Works Foundry for Mr. Truman Bolinger, including a job number, brief description, monetary amount, and dates associated with each entry. This work order includes two bronze casts, both cowboy-themed.

Script from the WBAP-TV/NBC station in Fort Worth, Texas, relating a news story.

Script from the WBAP-TV/NBC station in Fort Worth, Texas, relating a news story.

Script from the WBAP-TV/NBC station in Fort Worth, Texas, relating a news story.

Photograph used for a story in the Daily Oklahoman newspaper. Caption: "Road toward diversification for half-century old Skelly Oil Co. of Tulsa came in the late 1950s when the firm teamed up with Tidewater Oil Co. and Getty Oil Co. (before the merger) in a uranium ore deposits hunt. This photograph shows equipment working in the Shirley Basin of Carbon County, Wyoming, site of initial discovery."

Pair of brown suede boots. Almost knee-high, the boots are constructed as slip-on rounded-toe shoes or moccasins with added segments on the quarter to create the length of the boots. At the top, the suede of the boots is folded over outwards forming a pocket for a drawstring around top and a band of suede fringe around the outside of the boot. Indistinct trademark/logo stamped on sole. Illegible stamped mark inside boots. Referred to as "Squaw Boots", these were worn by the donor who acquired them in 1968 from the Fishing Bridge Store, in Yellowstone National Park.

A report summarizing the geology of Crooks Gap, Fremont County, Wyoming, as related to Uranium Resources

From introduction: This is one of a series of three reports on airborne radioactivity surveys in the United States. The reports contain the 185 airborne anomaly maps issued by the U. S. Atomic Energy Commission as a result of the AEC's aerial surveying program conducted from March 1952 to June 1956; two ground reconnaissance maps of Utah also are included. Most of the reconnaissance was done in the western United States.

The following report is an evaluation of mineral potential of the Stratified Primitive Area in Wyoming.

A report about two new geologic formations in Wyoming. The Foote Creek Formation consists of beds of fine-grained sandstone with shale, siltstone, and coal beds. The Dutton Creek Formation consists of beds of coarse-grained locally conglomeratic sandstone.

Photograph of mountainous landscape with a body of water and trees in Grand Teton National Park in Wyoming.

Photograph of landscape and mountainous region in Yellowstone National Park in Wyoming.

A report about the Jefferson Formation and the Three Forks Formation. Both of them constitute a sequence of dominantly marine rocks.

Photograph of Yellowstone Falls in Yellowstone National Park in Wyoming.

The purpose of this investigation was to characterize the population dynamics of the benthos of selected pristine thermal springs.

Photograph used for a newspaper owned by the Oklahoma Publishing Company.

Photograph used for a story in the Daily Oklahoman newspaper. Caption: "H. A. "Dave" True, independent operator from Wyoming and the president of the big Independent Petroleum Association of America, was talking about the state of the domestic natural gas industry during an interview."

Photograph used for a newspaper owned by the Oklahoma Publishing Company.

Photograph used for a newspaper owned by the Oklahoma Publishing Company. Caption: "H. A. "Dave" True Jr. Caspar, Wyo. 1964 president of Independent petroleum Assn. of Amer."

A report about the Powder River Basin in northeastern Wyoming which is a physiographic unit bounded on the west by the Bighorn Mountains. There are sedimentary rocks which range in age from Cambrian to Oligocene.

This report follows the geological field studies of uranium deposits near Pumpkin Buttes in the central part of the Powder River Basin, Wyoming, and eventually moving south of the basin.

A report about sandstone in the black hills of Wyoming and South Dakota. It discusses the nonopaque heavy minerals found within it.

The following report describes the examinations of the nonopague heavy minerals in sandstone found in the Black Hills in northeastern Wyoming and western South Dakota. The studies were made to determine if differences in the shapes of the grains and proportions of minerals are sufficiently distinctive to be used in subdividing and correlating formations.