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Publications

All of our publications are accessible through the USGS Publication Warehouse. Publications by scientists of the Oregon Water Science Center are listed below.

Filter Total Items: 789

Ground-water inflow to the Deschutes River near the Warm Springs Indian Reservation, Oregon, August 1985 Ground-water inflow to the Deschutes River near the Warm Springs Indian Reservation, Oregon, August 1985

Groundwater inflow to the Deschutes River near the Warm Springs Indian Reservation in Oregon was estimated for August 1985 by: (1) measuring streamflow at various sites along the river; (2) determining the part of the streamflow that is groundwater inflow; and (3) analyzing the hydraulic gradients of the groundwater flow system to estimate the amount of groundwater discharge to the...
Authors
E.L. Bolke, Antonius Laenen

Review of edgematchimg procedures for digital cartographic data used in Geographic Information Systems (GIS) Review of edgematchimg procedures for digital cartographic data used in Geographic Information Systems (GIS)

In the process of developing a continuous hydrographic data layer for water resources applications in the Pacific Northwest, map-edge discontinuities in the U.S. Geological Survey 1:100 ,000-scale digital data that required application of computer-assisted edgematching procedures were identified. The spatial data sets required by the project must have line features that match closely...
Authors
D.D. Nebert

Quality of bottom material and elutriates in the lower Willamette River, Portland Harbor, Oregon Quality of bottom material and elutriates in the lower Willamette River, Portland Harbor, Oregon

In October 1983 the U.S. Geological Survey, in cooperation with the U.S. Army Corp of Engineers, collected bottom-material and water samples from Portland Harbor, Oregon to determine concentrations of trace metals and organic compounds in elutriate-test filtrate and bottom material. Of the trace metals examined in bottom material, concentrations of cadmium slightly exceed those of local...
Authors
Gregory J. Fuhrer

Lithology, thickness, and extent of hydrogeologic units underlying the East Portland area, Oregon Lithology, thickness, and extent of hydrogeologic units underlying the East Portland area, Oregon

The lithology, thickness, and extent of eight distinct hydrogeologic units are described and mapped within the East Portland area of Oregon. The thickness, extent, and top of each unit are shown on contour maps at scales of 1:24,000. Their stratigraphic relations are displayed on a diagrammatic cross section. The geologic setting and unit lithology are described within the text. A data...
Authors
S.V. Hartford, W. D. McFarland

The effects of two multipurpose reservoirs on the water temperature of the McKenzie River, Oregon The effects of two multipurpose reservoirs on the water temperature of the McKenzie River, Oregon

A one dimensional, unsteady-state temperature model using the equilibrium temperature approach (with air temperature used to estimate equilibrium temperature) is used to evaluate the effects of two Army Corps of Engineers dams and resulting reservoirs on the McKenzie River, from Delta Park (River Kilometer 99.9) to Leaburg Dam (River Kilometer 62.4). Both Corps of Engineers projects are...
Authors
R. P. Hansen

U.S. Geological Survey ground-water studies in Oregon U.S. Geological Survey ground-water studies in Oregon

The use of groundwater in Oregon is expected to increase owing to continued population growth and to surface water supplies that are inadequate to meet present or future demand. The major groundwater issues in Oregon are: conjunctive use of surface and groundwater; contamination from hazardous wastes, leakage from underground gasoline and diesel tanks, naturally occurring brackish water...
Authors
E.L. Bolke

Geohydrology and digital simulation of the ground-water flow system in the Umatilla Plateau and Horse Heaven Hills area, Oregon and Washington Geohydrology and digital simulation of the ground-water flow system in the Umatilla Plateau and Horse Heaven Hills area, Oregon and Washington

The Columbia Plateau is underlain by massive basalt flows, with a composite thickness of about 10,000 ft. Structural features within the study area include a series of anticline-syncline pairs. The main avenues of groundwater movement in the basalt are the interflow zone between basalt flows. Individual interflow zones may be rather extensive in the lateral direction and are largely...
Authors
A. Davies-Smith, E.L. Bolke, C. A. Collins
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