The Fort Union formation is one of the most important and best known geologic formations of the northern Great Plains, and is found lying almost horizontal at the surface over large areas in this region
Potential gold mines lie high among the rugged peaks of the Tobacco Root Mountains of southwestern M...
The Roundup quadrangle is located in central Montana in parts of Musselshell, Yellowstone, and Golde...
This paper is a report of a geological survey made of an area of approximately fifty square miles ly...
The Fort Union and Lance formations are widespread terrestrial sediments exposed in Montana, North D...
To better acquaint seniors in Geology and mining with actual field practice, the Montana School of M...
Work was first done on a known section, the south Boulder Section, in order to familiarize the stude...
In 1915 the United States Geological Survey published a folio by Calkins and Emmons on the geology o...
The following evaluation of the mineral resources of the University Land-Grant lands has been made f...
The five counties discussed in this paper compose the northernmost and westernmost counties in Monta...
A vast amount of information has been published by many workers on particular features of the geolog...
Glacial deposits are increasingly entering into consideration in engineering projects, soil surveys,...
The Livingston formation is a thick succession of late Cretaceous lava flows, tuffs, and bedded wate...
Sometime prior to 1870, a group of prospectors made what was believed to be a rich strike\u27 on on...
As yet the knowledge of Ordovician and Devonian physiography in this vast northwest region remains a...
The purchase and continued operation of the Mike Horse mine in the Heddleston district, by the Ameri...
Potential gold mines lie high among the rugged peaks of the Tobacco Root Mountains of southwestern M...
The Roundup quadrangle is located in central Montana in parts of Musselshell, Yellowstone, and Golde...
This paper is a report of a geological survey made of an area of approximately fifty square miles ly...
The Fort Union and Lance formations are widespread terrestrial sediments exposed in Montana, North D...
To better acquaint seniors in Geology and mining with actual field practice, the Montana School of M...
Work was first done on a known section, the south Boulder Section, in order to familiarize the stude...
In 1915 the United States Geological Survey published a folio by Calkins and Emmons on the geology o...
The following evaluation of the mineral resources of the University Land-Grant lands has been made f...
The five counties discussed in this paper compose the northernmost and westernmost counties in Monta...
A vast amount of information has been published by many workers on particular features of the geolog...
Glacial deposits are increasingly entering into consideration in engineering projects, soil surveys,...
The Livingston formation is a thick succession of late Cretaceous lava flows, tuffs, and bedded wate...
Sometime prior to 1870, a group of prospectors made what was believed to be a rich strike\u27 on on...
As yet the knowledge of Ordovician and Devonian physiography in this vast northwest region remains a...
The purchase and continued operation of the Mike Horse mine in the Heddleston district, by the Ameri...
Potential gold mines lie high among the rugged peaks of the Tobacco Root Mountains of southwestern M...
The Roundup quadrangle is located in central Montana in parts of Musselshell, Yellowstone, and Golde...
This paper is a report of a geological survey made of an area of approximately fifty square miles ly...