Cirque orientation in the major highlands of Oregon

Graduate Project

Public Deposited

Citeable URL: https://ir.library.oregonstate.edu/concern/graduate_projects/xd07gt534

Descriptions

Attribute Name	Values
Creator	McEwan, Duncan
Abstract	Cirque aspects and elevations in the major highlands of Oregon indicate a pattern of climate during the Pleistocene similar to that of today. Mean cirque floor elevation increases toward the drier interior. Concentrations of cirques facing northeast, and steep gradients of cirque floor trend surfaces to the southwest, indicate a predominant southwesterly winter wind. No specific relationship exists between cirque aspect and cirque elevation. Local topography probably has a greater influence on cirque elevation than has been previously acknowledged.
Resource Type	Capstone Project
Date Available	2012-07-19T22:14:51+00:00
Date Issued	1980-05
Degree Level	Master's
Degree Name	Master of Science (M.S.)
Degree Field	Geography
Degree Grantor	Oregon State University
Commencement Year	1980
Advisor	Rosenfeld, Charles L.
Committee Member	Kimerling, A. Jon Brauner, David R.
Academic Affiliation	Geography
Déclaration de droits	In Copyright
Publisher	Oregon State University
Peer Reviewed	No
Language	English [eng]
Digitization Specifications	File scanned at 300 ppi (Monochrome) using ScandAll PRO 1.8.1 on a Fi-6770A in PDF format. CVista PdfCompressor 4.0 was used for pdf compression and textual OCR.
Replaces	http://hdl.handle.net/1957/31247

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