Model Morphologies of Subsurface Quaternary Basalts as Evidence for Adecrease in the Magnitude of Basaltic Magmatism at and Near the Idaho National Engineering and Environmental Laboratory, Idaho

Authors

Paul H. Wetmore, Idaho State UniversityFollow
Scott S. Hughes, Idaho State University
Steven R. Anderson, U.S. Geological Survey

Document Type

Conference Proceeding

Publication Date

1997

Rights Information

Terms of use for work posted in Scholar Commons.

Was this content written or created while at USF?

No

Citation / Publisher Attribution

Proceedings of the 32nd Symposium on Engineering Geology and Geotechnical Engineering, p. 45-58

Scholar Commons Citation

Wetmore, Paul H.; Hughes, Scott S.; and Anderson, Steven R., "Model Morphologies of Subsurface Quaternary Basalts as Evidence for Adecrease in the Magnitude of Basaltic Magmatism at and Near the Idaho National Engineering and Environmental Laboratory, Idaho" (1997). School of Geosciences Faculty and Staff Publications. 992.
https://digitalcommons.usf.edu/geo_facpub/992