Between the villages of Rocker and Silver Bow, in southwestern Montana, are found an interesting group of placers. Gold occurs in Tertiary gravel beds that are interstratified with beds of rhyolitic volcanic ash. With the aid of a plane table and open-sight alidade, a small portion of the lake-bed area near Rocker was mapped; all distances were paced, but numerous checks assure a fairly accurate map
The Holyrood granite batholith is a dome-shaped igneous body, approximately 40 miles in length and 8...
The morphology of the Broadmarsh-Elderslie area is very largely controlled by lithology and structu...
A total of 179 chemical analyses of igneous rocks are available for the state of Montana, but these...
For many years the Elliston District, of Powell County has been a minor producer of gold, lead, zinc...
Although the majority of geologic structures in Montana have been tested in the search for petroleum...
The objectives of this investigation include the following: (1) to map the distribution of the igneo...
Potential gold mines lie high among the rugged peaks of the Tobacco Root Mountains of southwestern M...
The Ermont Mines are located sixteen miles northwest of Dillon, Montana, in section 35 of T.6S., R.1...
Purpose of the Investigation: The geology of the Jefferson Mine was mapped to determine the relation...
The purpose of this investigation was to map and study, both at regional and detailed scales, the un...
A Thesis submitted to the faculty of the Graduate School of the University of Minnesota by Mark John...
Plane table and pacing methods were used in the mapping of the individual areas, but an automobile t...
Purpose and Scope During recent years geologic investigations have been made in various parts of nor...
The study of the geology and mineralization of the Crystal Mine was undertaken at the suggestion of ...
This investigation was undertaken primarily as a problem in geologic mapping, coupled with a study o...
The Holyrood granite batholith is a dome-shaped igneous body, approximately 40 miles in length and 8...
The morphology of the Broadmarsh-Elderslie area is very largely controlled by lithology and structu...
A total of 179 chemical analyses of igneous rocks are available for the state of Montana, but these...
For many years the Elliston District, of Powell County has been a minor producer of gold, lead, zinc...
Although the majority of geologic structures in Montana have been tested in the search for petroleum...
The objectives of this investigation include the following: (1) to map the distribution of the igneo...
Potential gold mines lie high among the rugged peaks of the Tobacco Root Mountains of southwestern M...
The Ermont Mines are located sixteen miles northwest of Dillon, Montana, in section 35 of T.6S., R.1...
Purpose of the Investigation: The geology of the Jefferson Mine was mapped to determine the relation...
The purpose of this investigation was to map and study, both at regional and detailed scales, the un...
A Thesis submitted to the faculty of the Graduate School of the University of Minnesota by Mark John...
Plane table and pacing methods were used in the mapping of the individual areas, but an automobile t...
Purpose and Scope During recent years geologic investigations have been made in various parts of nor...
The study of the geology and mineralization of the Crystal Mine was undertaken at the suggestion of ...
This investigation was undertaken primarily as a problem in geologic mapping, coupled with a study o...
The Holyrood granite batholith is a dome-shaped igneous body, approximately 40 miles in length and 8...
The morphology of the Broadmarsh-Elderslie area is very largely controlled by lithology and structu...
A total of 179 chemical analyses of igneous rocks are available for the state of Montana, but these...