Sponsor
Portland State University. Department of Earth Sciences
First Advisor
Paul E. Hammond
Term of Graduation
Spring 1981
Date of Publication
6-5-1981
Document Type
Thesis
Department
Earth Science
Language
English
Subjects
Geology -- Oregon -- Mount Jefferson Wilderness
DOI
10.15760/etd.3259
Physical Description
1 online resource (xiii, 181 pages)
Abstract
The volcanic stratigraphy and petrography is described for a 46 km2 area on the southern flank of Mount Jefferson in the north-central part of the Oregon High Cascades. Here, volcanic processes have been active throughout Quaternary time, resulting in complex stratigraphic relationships. In addition, three formerly recognized glaciations and a two-phase period of neoglaciation have eroded the terrain, depositing tills in contact or interstratified with the volcanic units. Collectively, these processes and the resulting deposits are characteristic of High Cascades development.
Rights
In Copyright. URI: http://rightsstatements.org/vocab/InC/1.0/ This Item is protected by copyright and/or related rights. You are free to use this Item in any way that is permitted by the copyright and related rights legislation that applies to your use. For other uses you need to obtain permission from the rights-holder(s).
Persistent Identifier
https://archives.pdx.edu/ds/psu/18755
Recommended Citation
Gannon, Brian Lee, "Geology of a Volcanic Complex on the South Flank of Mount Jefferson, Oregon" (1981). Dissertations and Theses. Paper 3268.
https://doi.org/10.15760/etd.3259
Geologic Map of the Table and Vicinity, Cascade Range, Oregon
gannon2.pdf (6747 kB)
Geologic Cross Sections
gannon3.pdf (3001 kB)
Lithologic Provenience Map
Comments
A thesis submitted in partial fulfillment of the requirements for the degree of Master of Arts in Geology.
If you are the rightful copyright holder of this dissertation or thesis and wish to have it removed from the Open Access Collection, please submit a request to pdxscholar@pdx.edu and include clear identification of the work, preferably with URL.