Aerial and Topographic Analysis of Quaternary Faulting at SP Crater Lava Flow, San Francisco Volcanic Field, Arizona, USA: Hightlighting Undergraduate Research in Geology

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Author
Wescott, J.
Rowan, C.
Nations, J.
Muncaster, G.
McCrea, B.
Jablonsky, J.
Barba, W.
Wilson, M.J
Gootee, B.F.
Willard, D.J.
Issue Date
2015-12-15
Keywords
Arizona Geological Survey Open File Reports
late Pleistocene
Historic
Recent
Coconino County
Colorado Plateau
SP Crater
San Fransciso Volcanic field
Flagstaff
Scottsdale Community College
citizen scientist
aerial photography
topography
geomorphology
normal fault

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Citation
Gootee, B.F., Willard, D.J., Wilson, M.J., Barba, W., Jablonsky, J., McCrea, B., Muncaster, Nations, J., Rowan, C. and Wescott, J., 2015, Aerial and Topographic Analysis of Quaternary Faulting at SP Crater Lava Flow, San Francisco Volcanic Field, Arizona, USA: Highlighting Undergraduate Research in Geology. Arizona Geological Survey Open File Report, OFR-15-11, 8 p, 1 appendix
Publisher
Arizona Geological Survey (Tucson, AZ)
Description
Approximately 60,000 years ago SP Crater, situated in the north- central part of the San Francisco volcanic field between Flagstaff and Grand Canyon, Arizona, erupted and flowed into a structural graben bound by late Quaternary faults. SP Crater is one of about 610 cinder cone volcanoes and 8 large dome complexes in the volcanic field which were emplaced between 6 Ma and 900 years ago, covering an area of about 5,000 km2 and volcanic volume of about 500 km3 (Tanaka et al., 1986; Conway et al., 1998).
URI
http://hdl.handle.net/10150/630730
Additional Links
http://repository.azgs.az.gov/uri_gin/azgs/dlio/1667
Language
en
Series/Report no.
OFR-15-11
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