Unified Interior Regions
Washington
States L2 Landing Page Tabs
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...
Sources of Mercury in Sinclair Inlet Project
The sediments in Sinclair Inlet within Puget Sound, Washington have elevated concentrations of a number of organic compounds and elements including mercury. Following remediation actions under the Comprehensive Environmental Response, Compensation, and Liability Act (CERCLA), it was determined that there is insufficient information to determine whether remedial action taken at OU B Marine with...
Cedar River Peak Flow Management
The Cedar River watershed provides two-thirds of the water supply for the greater Seattle metropolitan region, in addition to being home to numerous federally listed salmon species. The City of Seattle, through Seattle Public Utilities (SPU), works closely with the Cedar River Instream Flow Commission (IFC) to adaptively manage flows on the Cedar River. Seattle operates its water management...
Little Spokane Hydrogeology
The Issue: Groundwater is an important resource for domestic, commercial, and agricultural usage in the Little Spokane River Basin, and groundwater discharge helps maintain streamflow in area streams. Consequently, as the population grows, and commercial and agricultural activity increase, so does the demand for groundwater. However, the quantity of usable groundwater, and the...
Phosphorus SPARROW Model for the Yakima River
The Issue - During the 2004-07 irrigation season, nutrient concentrations in the lower Yakima River were high enough at certain times and locations to support the abundant growth of periphytic algae and macrophytes which resulted in large daily fluctuations in dissolved oxygen concentrations and pH levels that exceeded the Washington State water-quality standards for these...
Chimacum GW Model
Projected increases in population and development in northeastern Jefferson County, Washington, are expected to lead to increased groundwater withdrawals in the Chimacum Creek Basin. Changes in land use and climate could reduce groundwater recharge, thereby reducing groundwater available for drinking and for baseflow to streams that host endangered fish species.
The USGS is developing...
Consumptive Use
The Issue: Fresh groundwater withdrawals for irrigation from 66 principal aquifers in the United States comprised approximately three-fourths of total groundwater withdrawals in the year 2000. The magnitude of these withdrawals is certainly substantial but difficult to quantify because few states actually monitor groundwater withdrawals for irrigation. Water-resource managers...
Chamokane Framework and Model
Chamokane Creek Basin is a 179-square-mile area that borders and partially overlaps the Spokane Indian Reservation in southern Stevens County in northeastern Washington State. In 1979, all water rights in the Chamokane Creek Basin were adjudicated by a Federal court, which gave senior, reserved water rights to the Spokane Tribe of Indians for irrigation and protection of fish in Chamokane...
Stormwater Microarray Study
Evaluation of Juvenile Trout Microarray Tools in the Development of an Ambient Monitoring Approach for Urban Streams
NWIFC Water Assessment
Water resources are essential to Native American Tribes in western Washington for instream and out-of-stream uses. As the demand for water across the region increases, western Washington Tribes need critical information about water availability, water use, and ecological needs for water in order to manage their resources. To assess tribal water resources comprehensively in western Washington,...
White River Basin and Lake Tapps Water Quality
The Issue: Water diverted from the upper White River to maintain water levels in Lake Tapps impacts flows and fish resources in the White River. In the lower White River, releases of warm water from Lake Tapps for hydropower generation frequently lowered concentrations of dissolved oxygen and increased water temperatures at river mile 1.8. In the White River diversion reach, has segments that...
Linking Sources to the Sound
The Issue: Bioaccumulation of toxic chemicals in freshwater and marine aquatic research in the Puget Sound continues to be a concern for environmental managers and general public. With renewed interest, Washington State Department of Ecology (http://www.ecy.wa.gov/programs/wq/pstoxics/) began a phased, coordinated effort...
Distributed energy balance modeling of South Cascade Glacier, Washington and assessment of model uncertainty
We have developed a physically based, distributed surface energy balance model to simulate glacier mass balance under meteorological and climatological forcing. Here we apply the model to estimate summer ablation on South Cascade Glacier, Washington, for the 2004 and 2005 mass balance seasons. To arrive at optimal mass balance simulations, we...
Anslow, Faron S.; Hostetler, S.; Bidlake, W.R.; Clark, P.U.
Atmospheric Deposition and Surface-Water Chemistry in Mount Rainier and North Cascades National Parks, U.S.A., Water Years 2000 and 2005-2006
High-elevation aquatic ecosystems in Mount Rainier and North Cascades National Parks are highly sensitive to atmospheric deposition of nitrogen and sulfur. Thin, rocky soils promote fast hydrologic flushing rates during snowmelt and rain events, limiting the ability of basins to neutralize acidity and assimilate nitrogen deposited from the...
Clow, David W.; Campbell, Donald H. Survival and migration behavior of juvenile salmonids at McNary Dam, 2006
During 2006, we used acoustic telemetry and a route-specific survival model (RSSM, Skalski et al. 2002) to estimate behavior, passage, and survival of juvenile salmonids during two different spill operations and diel periods at McNary Dam. An evaluation of 12-h versus 24-h spill was proposed for the spring migration period at McNary Dam. However,...
Landslides Mapped from LIDAR Imagery, Kitsap County, Washington
Landslides are a recurring problem on hillslopes throughout the Puget Lowland, Washington, but can be difficult to identify in the densely forested terrain. However, digital terrain models of the bare-earth surface derived from LIght Detection And Ranging (LIDAR) data express topographic details sufficiently well to identify landslides. Landslides...
McKenna, Jonathan P.; Lidke, David J.; Coe, Jeffrey A. Survival and migration behavior of juvenile salmonids at Lower Granite Dam, 2006
We described behavior and estimated passage and survival parameters of juvenile salmonids during spring and summer migration periods at Lower Granite Dam in 2006. During the spring, the study was designed to examine the effects of the Behavioral Guidance Structure (BGS) by using a randomized-block BGS Stored / BGS Deployed treatment design. The...
Beeman, John W.; Fielding, Scott D.; Braatz, Amy C.; Wilkerson, Tamara S.; Pope, Adam C.; Walker, Christopher E.; Hardiman, Jill M.; Perry, Russell W.; Counihan, Timothy D. Cascadia Subduction Zone
The geometry and recurrence times of large earthquakes associated with the Cascadia Subduction Zone (CSZ) were discussed and debated at a March 28-29, 2006 Pacific Northwest workshop for the USGS National Seismic Hazard Maps. The CSZ is modeled from Cape Mendocino in California to Vancouver Island in British Columbia. We include the same...
Frankel, Arthur D.; Petersen, Mark D. White sturgeon mitigation and restoration in the Columbia and Snake rivers upstream from Bonneville Dam, Annual Progress Report April 2006 - March 2007. Report C
Describe reproduction and early life history characteristics of white sturgeon populations in the Columbia River between Bonneville and Priest Rapids dams. Define habitat requirements for spawning and rearing white sturgeon and quantify the extent of habitat available in the Columbia River between Bonneville and Priest Rapids dams. Progress...
Parsley, M.J.; Kofoot, P. Characterization of estuary use by Nisqually Hatchery Chinook based on Otolith analysis
INTRODUCTION The Nisqually Fall Chinook population is one of 27 stocks in the Puget Sound evolutionarily significant unit listed as threatened under the federal Endangered Species Act (ESA). Preservation and extensive restoration of the Nisqually delta ecosystem are planned to assist in recovery of the stock. A pre-restoration baseline...
Lind-Null, Angie M.; Larsen, Kim A.; Reisenbichler, Reg Needs Assessment and Scoping Study for Sinking Ships as Diving Sites in Puget Sound
BACKGROUND There is growing interest in starting a program to sink ships in Puget Sound to create one or more underwater dive sites. Experience in other parts of the world has indicated that sunken vessels are highly popular with divers and could provide a basis for increased recreation and attraction of out-of-state divers with attendant...
Rubin, Steve; Grossman, Eric E.; Koontz, Lynne; Paulson, Anthony; Sexton, Natalie; Reisenbichler, Reg
Chemistry, mineralogy, and petrology of amphibole in Mount St. Helens 2004-2006 dacite
Textural, compositional, and mineralogical data are reported and interpreted for a large population of clinoamphibole phenocrysts in 22 samples from the seven successive dacite spines erupted at Mount St. Helens between October 2004 and January 2006. Despite the uniformity in bulk composition of magma erupted since 2004, there is striking...
Sherrod, David R.; Scott, William E.; Stauffer, Peter H.; Thornber, Carl R.; Pallister, John S.; Lowers, Heather; Rowe, Michael C.; Mandeville, Charles W.; Meeker, Gregory P.
Petrology of the 2004-2006 Mount St. Helens lava dome -- implications for magmatic plumbing and eruption triggering
Eighteen years after dome-forming eruptions ended in 1986, and with little warning, Mount St. Helens began to erupt again in October 2004. During the ensuing two years, the volcano extruded more than 80×106 m3 of gas-poor, crystal-rich dacite lava. The 2004-6 dacite is remarkably uniform in bulk-rock composition and, at 65 percent SiO2 ,...
Sherrod, David R.; Scott, William E.; Stauffer, Peter H.; Pallister, John S.; Thornber, Carl R.; Cashman, Katharine V.; Clynne, Michael A.; Lowers, Heather; Mandeville, Charles W.; Brownfield, Isabelle K.; Meeker, Gregory P. Numerical modeling of rainfall thresholds for shallow landsliding in the Seattle, Washington, area
The temporal forecasting of landslide hazard has typically relied on empirical relations between rainfall characteristics and landslide occurrence to identify conditions that may cause shallow landslides. Here, we describe an alternate, deterministic approach to define rainfall thresholds for landslide occurrence in the Seattle, Washington, area....
Godt, Jonathan W.; McKenna, Jonathan P.
Small debris flows originating above Butte Camp, Mount St. Helens, WA
Path of small debris flows originating above Butte Camp, Mount St. Helens, Washington.
Scientist stands on the bank of a still river
USGS hydrologist Mark Reid looks at one of the many grabens (extensional basins) that formed as the Oso landslide swept across the North Fork Stillaguamish River valley.
K1 West Transect – 2015
Permanent Site: K1 West Transect; Depth: 6.0 Meters (19.8 Feet); Distance from river mouth: 4.5 Kilometers (2.8 Miles) east; Pre/Post Dam Removal: 4 years post-dam removal; Lat/Long: 48.13592923,-123.51082988; Site Description: This is a shallow site. Sediment is a gravel/sand mixture. Both red (1:30 seconds) and brown seaweed was abundant and appears close to pre-dam
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A2 East Transect – 2015
Permanent Site: A2 East Transect; Depth: 12.4 Meters (Feet 40.8); Distance from river mouth: Kilometers 1.8 (1.1 Miles); Pre/Post Dam Removal: 4 years post-dam removal; Lat/Long: 48.14130295, -123.58766124; Site Description: One of our deeper sites at over 40 feet. Sediment is primarily sand/sandy mud. Seaweeds have returned, mainly bull kelp Nereocystis luetkeana (0:14, 0
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A2 West Transect – 2015
Permanent Site: A2 West Transect; Depth: 12.9 Meters (Feet 42.3); Distance from river mouth: Kilometers 1.8 (1.1 Miles); Pre/Post Dam Removal: 4 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 a few scattered boulders. Seaweeds have returned but are sparse and
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F2 West Transect – 2015
Permanent Site: F2 West Transect; Depth: 11.2 Meters (36.9 Feet); Distance from river mouth: 1.5 Kilometers (0.9 Miles) east; Pre/Post Dam Removal: 4 years post-dam removal; Lat/Long: 48.15672004,-123.55036603; Site Description: Visibility is poor on video due to a large amount of surge on the day of the dive. Substrate is mainly a gravel - cobble mixture with an
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4SP1 West Transect – 2015
Permanent Site: 4SP1 - West Transect; Depth: 6.1 Meters (19.9 Feet); Distance from river mouth: 0.8 Kilometers (0.5 Miles) East; Pre/Post Dam Removal: 3 years post-dam removal; Lat/Long: 48.15257, -123.557376; Site Description: The site has converted from gravel/cobble substrate to all sand. Seaweed is completely absent.
L1 East Transect – 2015
Permanent Site: L1 East Transect; Depth: 11.6 Meters (38.0 Feet); Distance from river mouth: 2.3 Kilometers (1.4 Miles) west; Pre/Post Dam Removal: 4 years post-dam removal; Lat/Long: 48.13957527,-123.59359993; Site Description: This transect is medium depth. Substrate is mainly fine sediment/sand/mud with a few scattered boulders (1:15 seconds). Seaweed has returned.
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L1 West Transect – 2015
Permanent Site: L1 West Transect; Depth: 11.4 Meters (37.3 Feet); Distance from river mouth: 2.3 Kilometers (1.4 Miles) west; Pre/Post Dam Removal: 4 years post-dam removal; Lat/Long: 48.13957527,-123.59427175; Site Description: This transect is medium depth. The first 20 meters contains scattered boulders (0:18 seconds). Where there are no boulders, substrate is still
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A1 East Transect – 2015
Permanent Site: A1 East Transect; Depth: 8.3 Meters (27.1 Feet); Distance from river mouth: 1.8 Kilometers (1.1 Miles) West; Pre/Post Dam Removal: 4 years post-dam removal; Lat/Long: 48.13870775, -123.5855312; Site Description: Transect is in eastern part of Freshwater Bay. Sediment is primarily sand/sandy mud. Previous small boulders appear to be buried. Seaweeds are very
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K1 East Transect – 2015
Permanent Site: K1 East Transect; Depth: 6.7 Meters (22.0 Feet); Distance from river mouth: 4.5 Kilometers (2.8 Miles) east; Pre/Post Dam Removal: 4 years post-dam removal; Lat/Long: 48.13592923,-123.5101581; Site Description: This is a shallow site. Sediment is a gravel/sand mixture. Both red (0:44, 0:48 seconds) and brown seaweed was abundant and appears close to pre-dam
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A1 West Transect – 2015
Permanent Site: A1 West Transect; Depth: 8.7 Meters (28.5 Feet); Distance from river mouth: 1.9 Kilometers (1.2 Miles) West; Pre/Post Dam Removal: 4 years post-dam removal; Lat/Long: 48.13870775, -123.586203; Site Description: Transect is in eastern part of Freshwater Bay. Sediment is primarily sand/sandy mud with patches of boulders. Seaweeds have returned. A boulder
...A new assessment of shoreline change along the Pacific Northwest coast from the late 1800s to present found that while the majority of beaches are stable or slightly accreting (adding sand), many Oregon beaches have experienced an increase in erosion hazards in recent decades.
Scientsts from the Pacific Northwest and Colombia work together to understand and communicate volcano hazards.
Officials from South America are helping to save lives in communities around Cascade Range volcanoes by sharing their expertise in a bi-national exchange that brings Colombian emergency managers and scientists to the Pacific Northwest, following a recent visit to Colombia by U.S. counterparts.
Officials from South America are helping to save lives in communities around Cascade Range volcanoes by sharing their expertise in a bi-national exchange that brings Colombian emergency managers and scientists to the Pacific Northwest, following a recent visit to Colombia by U.S. counterparts.
A new computer model of the Chimacum Creek Basin built to simulate “what-if” scenarios for basin groundwater managers indicates that most of the water recharging the groundwater system flows directly out to marine waters and coastal areas, according to a report by the U.S. Geological Survey.
TACOMA, Wash. — Scientists have sorted out and mapped the aquifers in the Little Spokane River Basin, giving the first detailed picture of the groundwater system, according to a report published by the U.S. Geological Survey, in cooperation with Spokane County.
The spread of a highly virulent fish virus in four separate coastal Washington watersheds from 2007-2011 has been described in a new research paper by the U.S. Geological Survey. The most probable source of the virus was identified as steelhead trout originating from the Columbia River Basin.
USGS scientists took high-tech sensors typically found in devices such as smart phones and embedded them into a new method to monitor riverbed movements that can help protect spawning habitat for endangered salmon. Developed in cooperation with Seattle Public Utilities for the Cedar River, the new method is published in the Journal of Hydrology.
North America's largest vulture, the California condor, once graced the skies of the Pacific Northwest from northern California to British Columbia and was deeply woven into the fabric of many Native American cultures. A new book by two federal scientists documents the condors history in the region, from prehistoric times to the early 20th century.
The Columbia River Gorge Commission and the United States Geological Survey have initiated an agreement that will put the Columbia River Gorge National Scenic Area in the vanguard locally and nationally with an innovative multi-agency resource management and community development partnership.
The U.S. Geological Survey's Western Fisheries Research Center (WFRC), headquartered in Seattle, has led cutting-edge research on fish and aquatic environments for nearly 80 years – first in the Pacific Northwest, then nationwide and throughout the world.
For about one month, an airplane operated under contract to the U.S. Geological Survey will be making low-level flights over a 1000-square-mile area centered over Spokane and including parts of eastern Washington and western Idaho.
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Locations
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
USGS Volcano Science Center
Phone: 360-993-8900
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
Marrowstone Marine Field Station
Phone: (360) 385-1007
Fax: (360) 385-7207
Northwest Washington Field Office
Phone: (360) 312-8155 x2001
Fax: (360) 312-8565
Mid-Columbia Field Office
Phone: (509) 735-3739
Fax: (509) 735-3723
Upper Columbia Field Office
Phone: (509) 353-2649
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