Skip to Main Content
Fire and water: volcanology, geomorphology, and hydrogeology of the Cascade Range, central OregonAuthor(s): Katharine V. Cashman; Natalia I. Deligne; Marshall W. Gannett; Gordon E. Grant; Anne Jefferson
Source: The Geological Society of America. Field Guide15: 539-582
Publication Series: Scientific Journal (JRNL)
Station: Pacific Northwest Research Station
PDF: View PDF (3.03 MB)
DescriptionThis field trip guide explores the interactions among the geologic evolution, hydrology, and fluvial geomorphology of the central Oregon Cascade Range. Key topics include the geologic control of hydrologic regimes on both the wet and dry sides of the Cascade Range crest, groundwater dynamics and interaction between surface and groundwater in young volcanic arcs, and interactions between rivers and lava flows. As we trace the Willamette and McKenzie Rivers back to source springs high in the young volcanic rocks of the Cascade Range, there is abundant evidence for the large permeability of young lava flows, as manifested in streams that dewater into lava flows, lava-dammed lakes in closed basins, and rivers that emerge from single springs. These dynamics contrast sharply with the older, lower permeability Western Cascades terrane and associated runoff-dominated fluvial systems. On the east side of the Cascades we encounter similar hydrologic characteristics resulting in complex interactions between surface water and groundwater as we follow the Deschutes River downstream to its confluence with the Crooked River. Here, deep canyons have cut through most of the permeable part of the geologic section, have been invaded by multiple large intracanyon lava flows, and are the locus of substantial regional groundwater discharge. The groundwater and surface-water interaction in the Deschutes Basin is further complicated by surface-water diversions and an extensive network of leaking irrigation canals. Our west-to-east transect offers an unparalleled opportunity to examine the co-evolution of the geology and hydrology of an active volcanic arc.
- You may send email to firstname.lastname@example.org to request a hard copy of this publication.
- (Please specify exactly which publication you are requesting and your mailing address.)
- We recommend that you also print this page and attach it to the printout of the article, to retain the full citation information.
- This article was written and prepared by U.S. Government employees on official time, and is therefore in the public domain.
CitationCashman, Katharine V.; Deligne, Natalia I.; Gannett, Marshall W.; Grant, Gordon E.; Jefferson, Anne. 2009. Fire and water: volcanology, geomorphology, and hydrogeology of the Cascade Range, central Oregon. The Geological Society of America. Field Guide15: 539-582.
Keywordsgeology, geomorphology, field guides, fire, hydrology, volcanic
- Coevolution of hydrology and topography on a basalt landscape in the Oregon Cascade Range, USA
- Overview of geology, hydrology, geomorphology, and sediment budget of the Deschutes River Basin, Oregon.
- Running dry: Where will the West get its water?
XML: View XML