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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

Geology and ground water of the Tualatin Valley, Oregon Geology and ground water of the Tualatin Valley, Oregon

The Tualatin Valley proper consists of broad valley plains, ranging in altitude from 100 to 300 feet, and the lower mountain slopes of the drainage basin of the Tualatin River, a tributary of the Willamette River in northwestern Oregon. The valley is almost entirely farmed. Its population is increasing rapidly, partly because of the expansion of metropolitan Portland. Structurally, the...
Authors
D. H. Hart, R. C. Newcomb

Waterpower resources in Nehalem River basin, Oregon Waterpower resources in Nehalem River basin, Oregon

No abstract available.
Authors
Loyd L. Young, Jesse Lane Colbert, David L. Gaskill, Arthur M. Piper

Water for Oregon Water for Oregon

No abstract available.
Authors
Kenneth N. Phillips, R. C. Newcomb, H. A. Swenson, L.B. Laird

Geological Survey research 1965, Chapter C Geological Survey research 1965, Chapter C

This collection of 44 short papers is the second published chapter of Geological Survey Research 1965. The papers report on scientific and economic results of current work by members of the Conservation, Geologic, and Water Resources Divisions of the U.S. Geological Survey.
Authors
Water Resources Division U.S. Geological Survey

Geology and ground-water resources of the Walla Walla River basin Washington-Oregon Geology and ground-water resources of the Walla Walla River basin Washington-Oregon

The Walla Walla River, whose drainage basin of about 1,330 square miles lies astride the Washington-Oregon boundary, drains westward to empty into the Columbia River. The basin slopes from the 5,000-foot crest of the Blue Mountains through a structural and topographic basin to the terraced lands adjoining the Columbia River at an altitude of about 340 feet. The main unit of the...
Authors
R. C. Newcomb

Selected ground water data in the Eola-Amity Hills area, northern Willamette Valley, Oregon Selected ground water data in the Eola-Amity Hills area, northern Willamette Valley, Oregon

Occurrence, quality, and availability of ground water differ considerably from place to place in the Eola-Amity Hills area because of the highly diversified geologic and hydrologic conditions. A table relates the geologic situation to the availability of ground water for four areas--Eola-Amity Hills, east and west valley plains, and Willamette River flood plain. Tables show well and...
Authors
Don Price, Nyra A. Johnson

Add to e-Shelf Records of wells, water levels and chemical quality of water in Baker Valley, Baker County, Oregon Add to e-Shelf Records of wells, water levels and chemical quality of water in Baker Valley, Baker County, Oregon

Records from 135 representative wells, and chemical analyses of water from 49 wells and 2 springs are tabulated. Drillers' logs of representative wells comprise most of the report.
Authors
G.L. Ducret, D.B. Anderson

The operation and maintenance of a crest-stage gaging station The operation and maintenance of a crest-stage gaging station

The purpose of this manual is to familiarize field personnel with the procedures involved in operating crest-stage gaging stations. Crest-stage gages are used to determine the elevation of a peak stage occurring at a specific location in a stream. A crest-stage gage consists of a length of 14-inch diameter pipe installed in a vertical position in the stream channel (figure 1). The pipe...
Authors
John Friday

Quality of surface waters in the lower Columbia River Basin Quality of surface waters in the lower Columbia River Basin

This report, made during 1959-60, provides reconnaissance data on the quality of waters in the lower Columbia River basin ; information on present and future water problems in the basin; and data that can be employed both in water-use studies and in planning future industrial, municipal, and agricultural expansion within this area. The lower Columbia River basin consists of approximately...
Authors
John F. Santos
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