Geophysical logs and coal sections of holes drilled during 1977 and 1978 in T. 15 N., Rs. 90 and 91 W., Ketchum Buttes and Doty Mountain quadrangles, Carbon County, Wyoming
Explore the source record for details and available documents.
Geology topics
Publications and source records attributed to C.S. Venable Barclay.
Explore the source record for details and available documents.
Explore the source record for details and available documents.
During gas and oil exploration efforts in the Washakie Basin in Sweetwater County, Wyoming, undertaken by Ladd Petroleum Co. (a subsidiary of Utah International Inc.) core from the Upper Cretaceous Almond Formation of the Mesaverde Group was collected from their 1-22 Federal well. (See figure 1 for location.) From this core three coal and two carbonaceous shale samples, orginally at depths ranging from 3,091 to 3,116 m (see table 1 for descriptions), were selected and given to the U.S. Geological Survey for study. Results of chemical analyses on the samples and a comparison of these analyses with analyses of near-surface Almond Formation coal samples in Carbon County, Wyoming, are the topics of this report.
Explore the source record for details and available documents.
Explore the source record for details and available documents.
Explore the source record for details and available documents.
The Glen Ullin quadrangle occupies approximately 51 square miles inwestern Morton County, southwestern North Dakota. Glen Ullin, a small agricultural community on the Northern Pacific Railroad, about 52 miles west of Bismarck, is near the center of the quadrangle (fig. 1). The Glen Ullin quadrangle is one of a group of 14 adjoining 71/2-minute quadrangles (fig. 1) that are being mapped by the U.S. Geological Survey to furnish a basis for classification of lands withdrawn by the Federal Government pending classification for coal and to contribute to the geologic map atlas of the United States. Most of the fieldwork for the Glen Ullin quadrangle was done during the late summers and early falls of 1964 and 1965. During the summer of 1966 the U.S. Geological Survey conducted a drilling program in the Glen Ullin and nearby quadrangles (Smith, 1970) to gather information on the existence, thickness, and depth of lignite beds in withdrawn Federal lands. Three of the holes drilled are in the Glen Ullin quadrangle.