Unified Interior Regions
Sprague River Basin, Oregon
Region 9: Columbia-Pacific Northwest
Regions L2 Landing Page Tabs
Raging River Temperature
The Issue: Large, in-channel wood that helps to create and maintain healthy aquatic habitat in rivers throughout the Pacific Northwest was removed from many rivers in the past. In 2009, King County put wood back into the river to restore the Raging River watershed. To guide the county's restoration of the Raging River watershed, managers need to know the effect of restoration...
Lake Spokane
The Issue: Phosphorus from many different sources has caused water quality problems for Lake Spokane in eastern Washington by promoting the growth of algae and aquatic plants. Phosphorus comes from municipal and industrial point-sources upstream of Lake Spokane, as well as non-point sources like septic tanks, agricultural fields, and wildlife. Lake Spokane was listed by the...
North Santiam River Basin Study
The streamflow and water-quality conditions monitored by the USGS in the North Santiam River basin provide valuable information to water resource managers
Seismology in the City
Release Date: May 1, 2015
How seismologists can use noise to see under the ground.
South Fork Nooksack River Basin Groundwater and Surface-water Interactions and Processes
High water temperatures and low instream flows during the summer have been identified as some of the key limitations for the viability of South Fork Nooksack River salmon populations including summer and spring-run Chinook salmon. Restoration strategies including the placement of engineered log jams, the restoration of floodplains and wetlands, and instream flow negotiation have been developed...
White River Bioenergetics
The White River Basin is located in western Washington and drains an area of about 500 square miles. Rivers in the White River Basin are fed by melt water from glaciers on Mt. Rainier, runoff from snowmelt and rain, and groundwater discharge. Beginning in the early to mid-twentieth century, the White River from river mile (RM) 9 to its confluence with the Puyallup River was extensively...
Upper Kittitas County
The Issue: Baseflows in the tributary streams in the western portion of Kittitas County are important in the late summer and fall when demands on these streams peak. An ongoing USGS Yakima River basin study indicates that groundwater and surface water are interconnected, however the hydrogeologic framework and the potential impacts of groundwater withdrawals on tributary streamflow in the...
Recharge and frozen ground in the PNW
The Issue: Seasonally frozen ground occurs over approximately one-third of the contiguous United States, and the extent and duration of frozen ground have been decreasing as a result of global warming. In semi-arid regions such as the Columbia Plateau and Snake River Plain in the Pacific Northwest, nearly all natural recharge occurs between October and March when intermittent...
Nooksack River Streamflow and Network Analysis
The Lummi Nation is partner to six USGS streamflow-gaging stations in the Nooksack River basin that measure streamflow in small streams. The Lummi Nation uses data from these stations to help manage its natural resources and has requested that the USGS analyze the available data record. As a result, the USGS is using streamflow data collected in and near the Nooksack River basin to develop...
Vancouver Lake Nutrient Budget
The Issue: Vancouver Lake in Clark County, WA has been experiencing water quality problems for decades. Recently, harmful algal blooms have been taking place in summer resulting in closures of the lake to swimming/water contact. One potential cause of these algal blooms in the increased loading of nutrients to the lake; however, there is currently little known about the amount and timing of...
Clackamas River Basin Water-Quality Assessment
Starting in 1997, the USGS began routinely studying water resources in the Clackamas River Basin. Whether it be assessing harmful algal blooms, runoff issues, streamflow, or watershed health, the USGS has worked with its partners to maintain one of Oregon's most beloved rivers.
NAS Whidbey Transport Model
The Issue: The carcinogenic compound 1,4-dioxane was recently (2003) found in groundwater in the vicinity of the former landfill at Area 6, Operable Unit 1, Naval Air Station (NAS) Whidbey Island, Island County, Washington. The current extent and potential for further migration of 1,4-dioxane in the vicinity of Area 6 are not well known. Also at area 6, the Navy is exploring...
Land Treatment Digital Library (LTDL)
The Land Treatment Digital Library (LTDL) was created by the USGS to catalog legacy land treatment information on Bureau of Land Management lands in the western United States. The LTDL can be used by federal managers and scientists for compiling information for data-calls, producing maps, generating reports, and conducting analyses at varying spatial and temporal scales.
Data Entry Module for the Land Treatment Digital Library (LTDL)
This software allows agencies, organizations, and individuals to download an empty, stand-alone Land Treatment Digital Library database to individual or networked computers. Data entered in these databases may be submitted to the USGS for possible inclusion in the online Land Treatment Digital Library (https://ltdl.wr.usgs.gov).
1:1,000,000-scale potentiometric contours and control points for the Great Basin carbonate and alluvial aquifer system of Nevada, Utah, and parts of adjacent states
This dataset consists of potentiometric contours, control points used to guide the creation of the contours, and a grid of 2 square-mile cells used to average the water-level value of selected control points. Control points are based on water-level measurements at well and spring locations from the USGS National Water Information System (NWIS).
Three-dimensional hydrogeologic framework for the Great Basin carbonate and alluvial aquifer system of Nevada, Utah, and parts of adjacent states
This dataset was created in support of a study focusing on groundwater resources in the Great Basin carbonate and alluvial aquifer system (GBCAAS). The GBCAAS is a complex aquifer system comprised of both unconsolidated and bedrock formations covering an area of approximately 110,000 square miles. The aquifer system is situated in the eastern portion of the Great Basin Province of the western...
1:1,000,000-scale estimated outer extent of areas of groundwater discharge as evapotranspiration for the Great Basin carbonate and alluvial aquifer system of Nevada, Utah, and parts of adjacent states
This dataset was created in support of a study focusing on groundwater resources in the Great Basin carbonate and alluvial aquifer system (GBCAAS). The GBCAAS is a complex aquifer system comprised of both unconsolidated and bedrock formations covering an area of approximately 110,000 square miles. The aquifer system is situated in the eastern portion of the Great Basin Province of the western...
1:1,000,000-scale hydrographic areas and flow systems for the Great Basin carbonate and alluvial aquifer system of Nevada, Utah, and parts of adjacent states
This dataset was created in support of a USGS study focusing on groundwater resources in the Great Basin carbonate and alluvial aquifer system (GBCAAS). The GBCAAS is a complex aquifer system comprised of both unconsolidated and bedrock formations covering an area of approximately 110,000 square miles. The aquifer system is situated in the eastern portion of the Great Basin Province.
1:1,000,000-scale Hydrographic Areas of the Great Basin
This data set consists of hydrographic area and major flow system boundaries and polygons delineated at 1:1,000,000-scale for the Great Basin.
Willamette River Bathymetric Survey
U.S. Geological Survey (USGS) collected bathymetric data from the main stem Willamette River in March of 2002. These cross-sectional and longitudinal profile data were important in filling a large data gap and were instrumental in the creation of a representative model grid for the Willamette River.
Willamette River and Long Tom River Dye Study
As part of the U.S. Geological Survey's support of the technical analyses and temperature model development for Willamette Basin streams, U.S. Geological Survey (USGS) personnel carried out four dye studies in Willamette Basin streams in 2002.
GP1 West Transect – 2016
Permanent Control Site: GP1 West Transect; Depth: 7.9 m (25.9 feet); Distance from river mouth: 19.0 Kilometers (11.8 Miles) east; Pre/Post Dam Removal: 5 years post-dam removal; Lat/Long: 48.11852521,-123.31605203; Site Description: This site was established as the eastern control. Depth is medium-shallow. Substrate is mainly a gravel/sand/cobble mixture surrounding
GP2 West Transect – 2015
Permanent Control Site: GP2 West Transect; Depth: 13.0 Meters (42.6 Feet); Distance from river mouth: 18.8 Kilometers (11.6 Miles) east; Pre/Post Dam Removal: 5 years post-dam removal; Lat/Long: 48.12781102,-123.31712832; Site Description: This site was established as the eastern control. Substrate is mainly a gravel/sand/cobble mixture surrounding boulders. This year red
GP1 East Transect – 2016
Permanent Control Site: GP1 East Transect; Depth: 7.5 m (24.7 feet); Distance from river mouth: 19.0 Kilometers (11.8 Miles) east; Pre/Post Dam Removal: 5 years post-dam removal; Lat/Long:; Site Description: This site was established as the eastern control. Depth is medium-shallow. Substrate is mainly a gravel/sand/cobble mixture surrounding numerous large boulders. Red (1
GP2 East Transect – 2016
Permanent Control Site: GP2 East Transect; Depth: 13.2 Meters (43.4 Feet); Distance from river mouth: 18.8 Kilometers (11.7 Miles) east; Pre/Post Dam Removal: 5 years post-dam removal; Lat/Long: 48.12781102,-123.31645664; Site Description: This site was established as the eastern control. Substrate is mainly a gravel sand mixture. A few large boulders are located off
H1 West Transect – 2016
Permanent Site: H1 West Transect; Depth: 5.7 Meters (18.7 Feet); Distance from river mouth: 2.4 Kilometers (1.5 Miles) east; Pre/Post Dam Removal: 5 years post-dam removal; Lat/Long: 48.14803012,-123.53535558; Site Description: This is a shallow site and one of the farthest removed from the effects of the sediment plume outside of the control sites. Substrate is still
Columbia River Gorge near The Dalles, Oregon
Columbia River Gorge near The Dalles, Oregon, May 2016
The USGS conducts landscape science to help understand what factors are involved in landscape change and how those factors influence the patterns and changes happening in a landscape.
A2 West Transect – 2016
Permanent Site: A2 West Transect; Depth: 13.2 Meters (43.2 Feet); Distance from river mouth: Kilometers 1.8 (1.1 Miles); Pre/Post Dam Removal: 5 years post-dam removal; Lat/Long: 48.14130295, -123.5883331; Site Description: One of our deeper sites at over 40 feet. Sediment is primarily sand/sandy mud with scattered boulders. Seaweeds are still sparse and mainly acid kelp
H1 East Transect – 2016
Permanent Site: H1 East Transect; Depth: 5.7 Meters (18.8 Feet); Distance from river mouth: 2.4 Kilometers (1.5 Miles) east; Pre/Post Dam Removal: 5 years post-dam removal; Lat/Long: 48.1479177,-123.53472865; Site Description: This is a shallow site and one of the farthest removed from the effects of the sediment plume outside of the control sites. Substrate is still
English Sole
English Sole - Scuba divers from the U.S. Geological Survey’s Western Fisheries Research Center, Washington Sea Grant, EPA and the Lower Elwha Klallam Tribe collected data and images from a long-term study of the Elwha River dam removals and the resulting effects on the nearshore ecosystem.
Location: Strait of Juan de Fuca, near the
...
C2 West Transect – 2016
Permanent Site: C2 West Transect; Depth: 16.5 Meters (54.2 Feet); Distance from river mouth: 0.7 Kilometers (0.5 Miles); Pre/Post Dam Removal: 5 years post-dam removal; Lat/Long: 48.147841,-123.57663268; Site Description: One of our deepest sites. Substrate is all muddy sand. Seaweed is absent. Woody debris is present (1:18 seconds). The featherduster tubeworms that were
C2 East Transect – 2016
Permanent Site: C2 East Transect; Depth: 16.1 Meters (52.8 Feet); Distance from river mouth: 0.7 Kilometers (0.4 Miles); Pre/Post Dam Removal: 5 years post-dam removal; Lat/Long: 48.147841,-123.57596074; Site Description: One of our deepest sites. Substrate is all muddy sand. Seaweed is absent. A very large pile of woody debris lying in an indentation in the sand is seen
L1 West Transect – 2016
Permanent Site: L1 West Transect; Depth: 11.1 Meters (36.5 Feet); Distance from river mouth: 2.3 Kilometers (1.4 Miles) west; Pre/Post Dam Removal: 5 years post-dam removal; Lat/Long: 48.13957527,-123.59427175; Site Description: This transect is medium depth. The first 20 meters contains scattered boulders (0:17 seconds). Where there are no boulders, substrate is mainly
Geologic barriers, the intermixing of water between aquifers through wells, and groundwater pumping contribute to the pattern of declines of groundwater levels of the Columbia Plateau, according to a report published by the U.S. Geological Survey.
SANTA CRUZ, Calif. — The largest dam-removal project in history has increased river water cloudiness caused by suspended particles, known as turbidity, a process that could affect aquatic life. The dismantling of two large dams on the Elwha River in Washington began in September of last year and has increased river turbidity significantly, even though most of the sediment trapped behind the...
TACOMA, Wash. — Water management in the Chamokane Creek Basin can now be guided by a new computer model to run "what-if" simulations to evaluate the potential effects of groundwater withdrawals on streamflows in the basin, according to a report released today by the U. S. Geological Survey.
PORTLAND, Ore. — The United States Geological Survey, in cooperation with several Klamath Basin stakeholders, has developed hydrologic datasets for the upper Klamath Basin of south-central Oregon that can help water managers identify and prioritize water uses that could be voluntarily set aside and reallocated to yield an additional 30,000 acre feet of water to Upper Klamath Lake.
SEATTLE — The U.S. Geological Survey has named fish pathologist Dr. Jill Rolland the director of its Western Fisheries Research Center (WFRC), headquartered in Seattle.
TACOMA, Wash. — Roughly enough sediment to fill a football field to the height of six Space Needles is delivered into the Puget Sound each year through a complex delivery network of rivers, according to a fact sheet published by the U.S. Geological Survey. The sediment delivery has both positive and negative effects on the environment, with some significant unknowns.
PORT ANGELES, Wash. — Scuba-diver scientists from the U.S. Geological Survey, with support teams from the U.S. Environmental Protection Agency, the Lower Elwha Klallam Tribe, and Washington Sea Grant, are returning to the mouth of Washington’s Elwha River this week to explore and catalogue the effect of released sediment on marine life following the nation’s largest dam removal effort.
SPOKANE, Wash. — Starting Friday, scientists will be using sound waves to look down into the Earth, and the result will be a picture of the geology beneath Spokane, perhaps including faults that cause shallow earthquakes.
PORTLAND, Ore.– The U.S. Geological Survey has developed models to help water managers identify strategies to use groundwater for meeting competing water demands in the semi-arid upper Klamath Basin.
PORTLAND, Ore.–-Human activities, such as industrial production, transportation, and day-to-day living, are sources of many contaminants that flow into the Columbia River.
VANCOUVER, Wash. — May is Volcano Awareness Month in Washington State. While no volcanoes in Washington currently show indications of immediate reawakening, experience has taught us that volcanoes often give just a few days’ warning before an eruption begins.
BOISE, Idaho — The U.S. Geological Survey has named Michael E. Lewis as the new director of its Idaho Water Science Center, headquartered in Boise.
Contacts
Locations
Idaho Water Science Center
Phone: Phone: (208) 387-1300
Fax: (208) 387-1372
Washington Water Science Center
Phone: (253) 552-1600
Fax: (253) 552-1581
Western Fisheries Research Center (WFRC)
Phone: (206) 526-6282
Fax: (206) 526-6654
Oregon Water Science Center
info-or@usgs.gov
Phone: (503) 251-3200
Fax: (503) 251-3470
USGS Volcano Science Center
Phone: 360-993-8900
Forest and Rangeland Ecosystem Science Center (FRESC) Headquarters
fresc_outreach@usgs.gov
Phone: 541-750-1030
Fax: 541-750-1069
Northwest Climate Adaptation Science Center
USGS Cascades Volcano Observatory (CVO)
vhpweb@usgs.gov
Phone: 360-993-8900
Fax: 360-993-8980
Columbia River Research Laboratory
Phone: (509) 538-2299
Fax: (509) 538-2843
Oregon Cooperative Fish And Wildlife Research Unit
Idaho Water Science Center - Idaho National Laboratory Project Office
Phone: 208-526-2438
Forest and Rangeland Ecosystem Science Center (FRESC) Snake River Field Station
fresc_outreach@usgs.gov
Phone: 208-426-5200
Fax: 208-426-5210
Forest and Rangeland Ecosystem Science Center (FRESC) Olympic Field Station
fresc_outreach@usgs.gov
Phone: 360-565-3041
Forest and Rangeland Ecosystem Science Center (FRESC) Cascadia Field Station
fresc_outreach@usgs.gov
Phone: 206-616-1874
Fax: 206-685-0790
Forest and Rangeland Ecosystem Science Center (FRESC) Corvallis Research Group
fresc_outreach@usgs.gov
Phone: 541-750-1030
Klamath Falls Field Station
Phone: (541) 273-8689
Fax: (541) 273-8692
Marrowstone Marine Field Station
Phone: (360) 385-1007
Fax: (360) 385-7207
Idaho Water Science Center - Boise Field Office
Phone: (208) 387-1300
Fax: (208) 387-1372
Idaho Water Science Center - Post Falls Field Office
Phone: 208-773-4938
Idaho Water Science Center - Groundwater Training Facility
Phone: 208-387-1392
Northwest Washington Field Office
Phone: (360) 312-8155 x2001
Fax: (360) 312-8565
Medford Field Office
Phone: 541-776-4256
Fax: 541-776-4257
Klamath Falls Field Office
Phone: 541-273-8689
Mid-Columbia Field Office
Phone: (509) 735-3739
Fax: (509) 735-3723
Upper Columbia Field Office
Phone: (509) 353-2649
Idaho Water Science Center - Idaho Falls Field Office
Phone: 208-529-4287