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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: 785

Chemical analyses of elutriates, native water, and bottom material from the Chetco, Rogue, and Columbia rivers in western Oregon Chemical analyses of elutriates, native water, and bottom material from the Chetco, Rogue, and Columbia rivers in western Oregon

Chemical analyses of elutriates, bottom sediment, and water samples for selected metals, nutrients and organic compounds including insecticides, herbicides, and acid/neutral extractables have been made to provide data to determine short-term water-quality conditions associated with dredging operations in rivers and estuaries. Between April and August 1982, data were collected from the...
Authors
Gregory J. Fuhrer

Statistical summaries of streamflow data in Oregon; Volume 1, eastern Oregon Statistical summaries of streamflow data in Oregon; Volume 1, eastern Oregon

Statistical summaries of streamflow data at 335 streamgaging sites are presented in this two volume report to aid in appraising the hydrology of river basins in Oregon. Records for 31 gaging stations were compiled into separate periods owing to changes in regulation during the period of data collection. The periods before and after regulation are presented for comparison. A brief station
Authors
John Friday, S. J. Miller

The 1980 Polallie Creek debris flow and subsequent dam-break flood, East Fork Hood River basin, Oregon The 1980 Polallie Creek debris flow and subsequent dam-break flood, East Fork Hood River basin, Oregon

At approximately 9 p.m. on December 25, 1980, intense rainfall and extremely wet antecedent conditions combined to trigger a landslide of approximately 5,000 cubic yards at the head of Polallie Creek Canyon on the northeast flank of Mount Hood. The landslide was transformed rapidly into a debris flow, which surged down the channel at velocities between about 40 and 50 ft/s, eroding and
Authors
Gary L. Gallino, Thomas C. Pierson

Water-resources of western Douglas County, Oregon Water-resources of western Douglas County, Oregon

In western Douglas County, Quaternary coastal dune sands and marine terrace deposits may have the best potential for ground-water development. Yields of 200 gallons per minute have been reported from wells completed in Quaternary fluvial deposits along the lower Umpqua River. The entire area is underlain by Tertiary marine sediments that yield quantities of water barely adequate for...
Authors
D. A. Curtiss, C. A. Collins, E. A. Oster

Oregon ground-water quality and its relation to hydrogeologic factors — A statistical approach Oregon ground-water quality and its relation to hydrogeologic factors — A statistical approach

An appraisal of Oregon ground-water quality was made using existing data accessible through the U.S. Geological Survey computer system. The data available for about 1,000 sites were separated by aquifer units and hydrologic units. Selected statistical moments were described for 19 constituents including major ions. About 96 percent of all sites in the data base were sampled only once...
Authors
T. L. Miller, J. B. Gonthier

Ground-water resources in the Hood Basin, Oregon Ground-water resources in the Hood Basin, Oregon

The Hood Basin, an area of 1,035 square miles in north-central Oregon, includes the drainage basins of all tributaries of the Columbia River between Eagle Creek and Fifteenmile Creek. The physical characteristics and climate of the basin are diverse. The Wasco subarea, in the eastern half of the basin, has moderate relief, mostly intermittent streams, and semiarid climate. The Hood...
Authors
Stephen J. Grady

Water-quality data for Smith and Bybee Lakes, Portland, Oregon, June to November, 1982 Water-quality data for Smith and Bybee Lakes, Portland, Oregon, June to November, 1982

Water-quality monitoring at Smith and Bybee Lakes included measurement of water temperature, dissolved oxygen concentration and percent saturation, pH, specific conductance, lake depth, alkalinity, dissolved carbon, total dissolved solids, secchi disk light transparency, nutrients, and chlorophyll a and b. In addition, phytoplankton, zooplankton, and benthic invertebrate populations were
Authors
Daphne G. Clifton

Characteristics of Columbia River sediment following the eruption of Mount St. Helens on May 18, 1980 Characteristics of Columbia River sediment following the eruption of Mount St. Helens on May 18, 1980

During several periods of volcanic-ash eruption at Mount St. Helens, Wash., (March 30, May 25-26, May 30-June 2, and June 12-13, 1980) strong winds from the north occurred at high altitudes. As a result, the volcanic ash fell some 50 miles to the south in the Bull Run watershed, the principal water-supply source for the metropolitan area of Portland, Oreg. Water samples collected from...
Authors
David Wellington Hubbell, Julija M. Laenen, Stuart W. McKenzie
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