Leland Fuhrig
Hydrologist for the Washington Water Science Center
Science and Products
Evaluation of Groundwater Resources in the White River Watershed
The Issue: The White River/Sunrise area of Mount Rainier National Park currently uses surface water for supplying water to local visitor and operational facilities. The Park is considering instead to use groundwater supplies that would likely be more resilient and less prone to contamination, but they need a better understanding of groundwater in the upper White River watershed to assure that park...
Simulated groundwater flow paths and travel times near Joint Base Lewis–McChord, Washington
The Issue: Past activities at Joint Base Lewis–McChord (JBLM)—located in west-central Washington—resulted in releases of hazardous waste and contaminants to the environment, and the most recent chemical of concern is per- and polyfluoroalkyl substances (PFAS). PFAS can enter groundwater and travel through the subsurface. Water-resource managers need to understand where groundwater flows in order...
Quillayute River Temperature
The Issue: The Quillayute River supports habitat for migrating, spawning, and rearing steelhead and salmon. All six miles of the river are influenced by tides, which influence its stage, discharge, and exchange with groundwater. The Quillayute River, like many salmonid-bearing rivers in the Pacific Northwest, is projected to warm in the coming decades due to projected increases in atmospheric...
Aquifer Recharge Area Study of Guemes Island
The Issue: Guemes Island is an 8.2-square-mile island in the northern part of Puget Sound in western Washington State. The population of the island is increasing, as is the demand for groundwater, which is the island's sole source of freshwater. Continued growth and development of the island, particularly in nearshore areas, has led to the increasing failure of nearshore wells due to seawater...
Groundwater Monitoring on Fort Sill Apache Tribal Lands
This USGS investigation will examine the hydraulic properties of the Rush Springs aquifer underlying Fort Sill Apache tribal lands to determine their potential for groundwater development. The information gathered from this investigation will assist the Fort Sill Apache Tribe in identifying well locations with optimal long-term pumping capacity and water quality.
Water Temperature Dynamics in the Quillayute River Basin, Washington, 2021 - 2023
The Quillayute River Basin in northwestern Washington consists of the Quillayute River and the river systems of its major tributaries, the Dickey, Sol Duc, and Bogachiel Rivers. With a drainage area of 629 square miles, the Quillayute River Basin provides important habitat for 23 distinct runs of anadromous steelhead and salmon, representing one of the largest and most productive watersheds on the
MODFLOW-NWT model to simulate the groundwater flow system near Puget Sound, Pierce and King Counties, Washington
A three-dimensional groundwater flow model, constructed in MODFLOW-NWT, was developed to evaluate the groundwater flow system near Puget Sound, Pierce and King Counties, Washington. A steady-state model version was constructed to simulate equilibrium conditions, while a transient model version was constructed to simulate monthly variability from January 2005 to December 2015. The model was used to
MODFLOW-NWT model used in Simulation of Groundwater Flow, and Analysis of Projected Water Use for the Washita River Alluvial Aquifer, Western Oklahoma
In 2020 the U.S. Geological Survey, in cooperation with the Oklahoma Water Resources Board, published a calibrated numerical groundwater-flow model and associated model documentation report that evaluated the effects of potential groundwater withdrawals on groundwater flow and availability in the Washita River alluvial aquifer in western Oklahoma. The results of groundwater-availability scenarios
Numerical model of the groundwater-flow system near the southeastern part of Puget Sound, Washington
Groundwater flow in the active model area (AMA) was simulated using a groundwater-flow model. A steady-state model version of the model simulates equilibrium conditions, and a transient model version simulates monthly variability. The model corresponds to the physical and temporal dimensions of the conceptual model and groundwater budget. The steady-state model version represents average condition
Authors
Andrew J. Long, Elise E. Wright, Leland T. Fuhrig, Valerie A.L. Bright
Evaluation of groundwater resources in the Upper White River Basin within Mount Rainier National Park, Washington State, 2020
The U.S. Geological Survey (USGS), in cooperation with the National Park Service, investigated groundwater gains and losses on the upper White River within Mount Rainier National Park in Washington. This investigation was conducted using stream discharge measurements at 14 locations within 7 reaches over a 6.5-mile river length from near the White River’s origin at the terminus of the Emmons Glaci
Authors
Leland T. Fuhrig, Andrew J. Long, Alexander O. Headman
Hydrogeology, numerical simulation of groundwater flow, and effects of future water use and drought for reach 1 of the Washita River alluvial aquifer, Roger Mills and Custer Counties, western Oklahoma, 1980–2015
The Washita River alluvial aquifer is a valley-fill and terrace alluvial aquifer along the valley of the Washita River in western Oklahoma that provides a productive source of groundwater for agricultural irrigation and water supply. The Oklahoma Water Resources Board (OWRB) has designated the westernmost section of the aquifer in Roger Mills and Custer Counties, Okla., as reach 1 of the Washita R
Authors
John H. Ellis, Derek W. Ryter, Leland T. Fuhrig, Kyle W. Spears, Shana L. Mashburn, Ian M.J. Rogers
Hydrogeology and simulation of groundwater flow and analysis of projected water use for the Canadian River alluvial aquifer, western and central Oklahoma
This report describes a study of the hydrogeology and simulation of groundwater flow for the Canadian River alluvial aquifer in western and central Oklahoma conducted by the U.S. Geological Survey in cooperation with the Oklahoma Water Resources Board. The report (1) quantifies the groundwater resources of the Canadian River alluvial aquifer by developing a conceptual model, (2) summarizes the gen
Authors
John H. Ellis, Shana L. Mashburn, Grant M. Graves, Steven M. Peterson, S. Jerrod Smith, Leland T. Fuhrig, Derrick L. Wagner, Jon E. Sanford
Science and Products
Evaluation of Groundwater Resources in the White River Watershed
The Issue: The White River/Sunrise area of Mount Rainier National Park currently uses surface water for supplying water to local visitor and operational facilities. The Park is considering instead to use groundwater supplies that would likely be more resilient and less prone to contamination, but they need a better understanding of groundwater in the upper White River watershed to assure that park...
Simulated groundwater flow paths and travel times near Joint Base Lewis–McChord, Washington
The Issue: Past activities at Joint Base Lewis–McChord (JBLM)—located in west-central Washington—resulted in releases of hazardous waste and contaminants to the environment, and the most recent chemical of concern is per- and polyfluoroalkyl substances (PFAS). PFAS can enter groundwater and travel through the subsurface. Water-resource managers need to understand where groundwater flows in order...
Quillayute River Temperature
The Issue: The Quillayute River supports habitat for migrating, spawning, and rearing steelhead and salmon. All six miles of the river are influenced by tides, which influence its stage, discharge, and exchange with groundwater. The Quillayute River, like many salmonid-bearing rivers in the Pacific Northwest, is projected to warm in the coming decades due to projected increases in atmospheric...
Aquifer Recharge Area Study of Guemes Island
The Issue: Guemes Island is an 8.2-square-mile island in the northern part of Puget Sound in western Washington State. The population of the island is increasing, as is the demand for groundwater, which is the island's sole source of freshwater. Continued growth and development of the island, particularly in nearshore areas, has led to the increasing failure of nearshore wells due to seawater...
Groundwater Monitoring on Fort Sill Apache Tribal Lands
This USGS investigation will examine the hydraulic properties of the Rush Springs aquifer underlying Fort Sill Apache tribal lands to determine their potential for groundwater development. The information gathered from this investigation will assist the Fort Sill Apache Tribe in identifying well locations with optimal long-term pumping capacity and water quality.
Water Temperature Dynamics in the Quillayute River Basin, Washington, 2021 - 2023
The Quillayute River Basin in northwestern Washington consists of the Quillayute River and the river systems of its major tributaries, the Dickey, Sol Duc, and Bogachiel Rivers. With a drainage area of 629 square miles, the Quillayute River Basin provides important habitat for 23 distinct runs of anadromous steelhead and salmon, representing one of the largest and most productive watersheds on the
MODFLOW-NWT model to simulate the groundwater flow system near Puget Sound, Pierce and King Counties, Washington
A three-dimensional groundwater flow model, constructed in MODFLOW-NWT, was developed to evaluate the groundwater flow system near Puget Sound, Pierce and King Counties, Washington. A steady-state model version was constructed to simulate equilibrium conditions, while a transient model version was constructed to simulate monthly variability from January 2005 to December 2015. The model was used to
MODFLOW-NWT model used in Simulation of Groundwater Flow, and Analysis of Projected Water Use for the Washita River Alluvial Aquifer, Western Oklahoma
In 2020 the U.S. Geological Survey, in cooperation with the Oklahoma Water Resources Board, published a calibrated numerical groundwater-flow model and associated model documentation report that evaluated the effects of potential groundwater withdrawals on groundwater flow and availability in the Washita River alluvial aquifer in western Oklahoma. The results of groundwater-availability scenarios
Numerical model of the groundwater-flow system near the southeastern part of Puget Sound, Washington
Groundwater flow in the active model area (AMA) was simulated using a groundwater-flow model. A steady-state model version of the model simulates equilibrium conditions, and a transient model version simulates monthly variability. The model corresponds to the physical and temporal dimensions of the conceptual model and groundwater budget. The steady-state model version represents average condition
Authors
Andrew J. Long, Elise E. Wright, Leland T. Fuhrig, Valerie A.L. Bright
Evaluation of groundwater resources in the Upper White River Basin within Mount Rainier National Park, Washington State, 2020
The U.S. Geological Survey (USGS), in cooperation with the National Park Service, investigated groundwater gains and losses on the upper White River within Mount Rainier National Park in Washington. This investigation was conducted using stream discharge measurements at 14 locations within 7 reaches over a 6.5-mile river length from near the White River’s origin at the terminus of the Emmons Glaci
Authors
Leland T. Fuhrig, Andrew J. Long, Alexander O. Headman
Hydrogeology, numerical simulation of groundwater flow, and effects of future water use and drought for reach 1 of the Washita River alluvial aquifer, Roger Mills and Custer Counties, western Oklahoma, 1980–2015
The Washita River alluvial aquifer is a valley-fill and terrace alluvial aquifer along the valley of the Washita River in western Oklahoma that provides a productive source of groundwater for agricultural irrigation and water supply. The Oklahoma Water Resources Board (OWRB) has designated the westernmost section of the aquifer in Roger Mills and Custer Counties, Okla., as reach 1 of the Washita R
Authors
John H. Ellis, Derek W. Ryter, Leland T. Fuhrig, Kyle W. Spears, Shana L. Mashburn, Ian M.J. Rogers
Hydrogeology and simulation of groundwater flow and analysis of projected water use for the Canadian River alluvial aquifer, western and central Oklahoma
This report describes a study of the hydrogeology and simulation of groundwater flow for the Canadian River alluvial aquifer in western and central Oklahoma conducted by the U.S. Geological Survey in cooperation with the Oklahoma Water Resources Board. The report (1) quantifies the groundwater resources of the Canadian River alluvial aquifer by developing a conceptual model, (2) summarizes the gen
Authors
John H. Ellis, Shana L. Mashburn, Grant M. Graves, Steven M. Peterson, S. Jerrod Smith, Leland T. Fuhrig, Derrick L. Wagner, Jon E. Sanford