An Occurrence of Autunite, Lawrence County, South Dakota (open access)

An Occurrence of Autunite, Lawrence County, South Dakota

From abstract: In July 1952 an occurrence of autunite was found in the northern part of the Black Hills, South Dakota, during a reconnaissance for radioactive deposits.
Date: January 1953
Creator: Vickers, Rollin C.
System: The UNT Digital Library
Radioactivity and Uranium Content of Some Cretaceous Shales, Central Great Plains (open access)

Radioactivity and Uranium Content of Some Cretaceous Shales, Central Great Plains

Report discussing a reconnaissance search for uranium in shale during August 1953 in western Nebraska and southern South Dakota. The reconnaissance was part of the U.S. Geological Survey's search for uranium in carbonaceous materials.
Date: January 1955
Creator: Tourtelot, Harry A.
System: The UNT Digital Library
Geology and Pegmatites of the Fourmile Quadrangle, Black Hills, South Dakota (open access)

Geology and Pegmatites of the Fourmile Quadrangle, Black Hills, South Dakota

Report discussing the geology and pegmatites of the Fourmile Quadrangle, located on the southwest side of the Black Hills uplift in Custer County, South Dakota. "This report is an abstract of a paper with the same title that is planned for publication as a Geological Survey professional paper."
Date: January 1959
Creator: Redden, Jack A.
System: The UNT Digital Library
Preliminary Digital Model of Ground-Water Flow in the Madison Group, Powder River Basin and Adjacent Areas, Wyoming, Montana, South Dakota, North Dakota, and Nebraska (open access)

Preliminary Digital Model of Ground-Water Flow in the Madison Group, Powder River Basin and Adjacent Areas, Wyoming, Montana, South Dakota, North Dakota, and Nebraska

Abstract: A digital simulation model was used to analyze regional ground-water flow in the Madison Group aquifer in the Powder River Basin and adjacent areas. Most recharge to the aquifer originates in or near the outcrop areas of the Madison in the Bighorn Mountains and Black Hills , and most discharge occurs through springs and wells. Results from the model calculations indicate that the total flow through the aquifer in the modeled areas was approximately 200 cubic feet per second (5.7 cubic metres per second). The aquifer can probably sustain increased ground-water withdrawals probably would significantly lower the potentiometric surface in the Madison aquifer in a large part of the basin. The digital model could better predict the effects of withdrawals if more accurate estimates of the storage coefficient, transmissivity, and leakance could be obtained.
Date: January 1976
Creator: Konikow, Leonard F.
System: The UNT Digital Library
Geology of the Calamity Peak area, Custer County, South Dakota (open access)

Geology of the Calamity Peak area, Custer County, South Dakota

A report discussing and area of 2.5 square miles along the southwest border of the pre-Cambrian granitic rocks complex in the pre-Cambrian core of the Harney Peak region, Black Hills, South Dakota that was mapped to determine the relationship between the granite-pegmatite complex and the pegmatites containing beryl and other industrial minerals. This investigation was part of the U.S. Geological Surveys program for the investigation of domestic beryllium resources and was carried out on behalf of the Atomic Energy Commission.
Date: January 14, 1955
Creator: Kupfer, Donald H.
System: The UNT Digital Library