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
Polallie Creek debris flow and subsequent dam-break flood of 1980, East Fork Hood River basin, Oregon Polallie Creek debris flow and subsequent dam-break flood of 1980, East Fork Hood River basin, Oregon
No abstract available.
Authors
Gary L. Gallino, Thomas C. Pierson
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 2, western Oregon Statistical summaries of streamflow data in Oregon; Volume 2, western Oregon
No abstract available.
Authors
John Friday, S. J. Miller
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