Abstract
Introduction Most of the writer’s experience with Rocky Mountain structure has been gained in eastern Idaho in connection with the United States Geological Survey’s study of the western phosphate field, but some years ago he conducted a series of field parties from the Harvard University Summer School in southwestern Montana. He therefore feels some measure of acquaintance with the structural conditions in that State as well. The remarks that follow are based chiefly on work in Idaho, but some mention is made of Montana and of other regions for comparison. Detailed or semi-detailed study has been made of three separate districts in eastern Idaho, namely: (1) the Fort Hall Indian Reservation, (2) an area comprising 7 quadrangles lying about 15 miles east of the Fort Hall Indian Reservation and extending to the southeastern corner of the State, and (3) an area lying immediately west and south of the Teton basin. . . .
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
