USGS Scientific Investigations Report
The Cascade Range in central Oregon has been shaped by tectonics, volcanism, and hydrology, as well as geomorphic forces that include glaciations. As a result of the rich interplay between these forces, mafic volcanism here can have surprising manifestations, which include relatively large tephra footprints and extensive lava flows, as well as water shortages, transportation and agricultural disruption, and forest fires. Although the focus of this multidisciplinary field trip will be on mafic volcanism, we will also look at the hydrology, geomorphology, and ecology of the area, and we will examine how these elements both influence and are influenced by mafic volcanism. We will see mafic volcanic rocks at the Sand Mountain volcanic field and in the Santiam Pass area, at McKenzie Pass, and in the southern Bend region. In addition, this field trip will occur during a total solar eclipse, the first one visible in the United States in more than 25 years (and the first seen in the conterminous United States in more than 37 years).
Volcanism--Oregon; Volcanology--Oregon; Cascade Range
Citation: Pilot Scholars Version (Modified MLA Style)
Deligne, Natalia I.; Mckay, Daniele; Conrey, Richard M.; Grant, Gordon E.; Johnson, Emily R.; O'Connor, Jim; and Sweeney, Kristin, "Field-Trip Guide to Mafic Volcanism of the Cascade Range in Central Oregon— A Volcanic, Tectonic, Hydrologic, and Geomorphic Journey" (2017). Environmental Studies Faculty Publications and Presentations. 46.