The Big Chino Subbasin is a groundwater basin that includes the Verde River headwaters in Yavapai County in north-central Arizona. Groundwater in the Big Chino Valley discharges to wells (by pumping), by evapotranspiration, and to the upper Verde River springs, which form the headwaters of the Verde River. Groundwater also discharges to short perennial reaches of Williamson Valley Wash, Walnut Creek, and a small number of small, ungaged springs and seeps. To monitor changes in groundwater storage and to identify aquifer-storage properties, a network of repeat microgravity stations and groundwater-level monitoring stations was established in the Big Chino and Williamson Valleys in 2010. In addition, the project maintains a streamgaging station on Williamson Valley Wash (station 09502800).
Summary of study findings (Kennedy and others, 2019):
- Small decreases in groundwater storage were observed throughout the study area from 2010 to 2017.
- The last major groundwater recharge event (when groundwater levels rose regionally in response to prolonged precipitation) was winter 2004-2005.
- During the 2010–2017 period, groundwater levels declined most rapidly in the upland area to the west of Big Chino Wash. The highest rates of decline were near the center of the study area around Walnut Creek, with smaller declines near the northern and southern extents. Groundwater-level declines were also widespread in the Paulden area and to a lesser extent in the Williamson Valley Wash area.
- Based on relatively large water-level changes accompanied by small storage changes, water levels at several locations in the Paulden and Big Chino Water Ranch areas appear to represent semi-confined aquifers.
Monitoring Sites
Sites used in this study are shown in the interactive map at the upper right. Continuous groundwater-level monitoring is ongoing at 5 locations (blue markers), and streamgaging at 4 locations (red markers). Repeat microgravity data is collected at 33 stations (yellow markers).
Additonal Site Information and Data
Groundwater-Level Monitoring Sites
- B-18-02 20DBB [PILOTS REST]
- GIPE WELL (SRP MONITORING WELL)
- B-18-03 26BBC1 [WINEGLASS RANCH]
- B-19-04 10CCB2 [WMW 3]
- B-19-04 05ABA1
- B-20-04 33CBD2 [WMW 2]
Streamgaging Sites
- DEL RIO SPRINGS NEAR CHINO VALLEY, AZ
- BIG CHINO WASH AT PAULDEN, AZ
- VERDE RIVER NEAR PAULDEN, AZ
- WILLIAMSON VALLEY WASH NEAR PAULDEN, AZ
Repeat Microgravity Sites
- Repeat microgravity data collected from 2001-2017 at 33 stations are available in a data release.
Data associated with this project are listed below.
Repeat microgravity data from the Big Chino Subbasin, 2001-2017, Yavapai County, Arizona
Below are publications associated with this project as well as publications relative to the area in and around the Big Chino Subbasin.
Aquifer storage change and storage properties, 2010–2017, in the Big Chino Subbasin, Yavapai County, Arizona
Geochemical assessment of groundwater in the Big Chino subbasin, Arizona, 2011–18
Characterization of Big Chino subbasin hydrogeology near Paulden, Arizona, using controlled source audio-frequency magnetotelluric surveys
Geochemical characterization and modeling of regional groundwater contributing to the Verde River, Arizona between Mormon Pocket and the USGS Clarkdale gage
Hydrogeology of the upper and middle Verde River watersheds, central Arizona
Below are partners associated with this project.
- Overview
The Big Chino Subbasin is a groundwater basin that includes the Verde River headwaters in Yavapai County in north-central Arizona. Groundwater in the Big Chino Valley discharges to wells (by pumping), by evapotranspiration, and to the upper Verde River springs, which form the headwaters of the Verde River. Groundwater also discharges to short perennial reaches of Williamson Valley Wash, Walnut Creek, and a small number of small, ungaged springs and seeps. To monitor changes in groundwater storage and to identify aquifer-storage properties, a network of repeat microgravity stations and groundwater-level monitoring stations was established in the Big Chino and Williamson Valleys in 2010. In addition, the project maintains a streamgaging station on Williamson Valley Wash (station 09502800).
Summary of study findings (Kennedy and others, 2019):
- Small decreases in groundwater storage were observed throughout the study area from 2010 to 2017.
- The last major groundwater recharge event (when groundwater levels rose regionally in response to prolonged precipitation) was winter 2004-2005.
- During the 2010–2017 period, groundwater levels declined most rapidly in the upland area to the west of Big Chino Wash. The highest rates of decline were near the center of the study area around Walnut Creek, with smaller declines near the northern and southern extents. Groundwater-level declines were also widespread in the Paulden area and to a lesser extent in the Williamson Valley Wash area.
- Based on relatively large water-level changes accompanied by small storage changes, water levels at several locations in the Paulden and Big Chino Water Ranch areas appear to represent semi-confined aquifers.
Monitoring Sites
Sites used in this study are shown in the interactive map at the upper right. Continuous groundwater-level monitoring is ongoing at 5 locations (blue markers), and streamgaging at 4 locations (red markers). Repeat microgravity data is collected at 33 stations (yellow markers).
Additonal Site Information and Data
Groundwater-Level Monitoring Sites
A-10 absolute gravity meter near a monitoring well - B-18-02 20DBB [PILOTS REST]
- GIPE WELL (SRP MONITORING WELL)
- B-18-03 26BBC1 [WINEGLASS RANCH]
- B-19-04 10CCB2 [WMW 3]
- B-19-04 05ABA1
- B-20-04 33CBD2 [WMW 2]
Streamgaging Sites
- DEL RIO SPRINGS NEAR CHINO VALLEY, AZ
- BIG CHINO WASH AT PAULDEN, AZ
- VERDE RIVER NEAR PAULDEN, AZ
- WILLIAMSON VALLEY WASH NEAR PAULDEN, AZ
Repeat Microgravity Sites
- Repeat microgravity data collected from 2001-2017 at 33 stations are available in a data release.
- Data
Data associated with this project are listed below.
Repeat microgravity data from the Big Chino Subbasin, 2001-2017, Yavapai County, Arizona
This dataset contains absolute-gravity measurements made using an A-10 absolute gravity meter (Micro-g Lacoste, Inc.) between 2009 and 2017 in the Big Chino Subbasin, Yavapai County, Arizona. Measurements were made about 3 times per year at a total of 33 different stations. Data are presented in tabular form, including relevant parameters used for processing. Data were output by g software (Micro- - Publications
Below are publications associated with this project as well as publications relative to the area in and around the Big Chino Subbasin.
Aquifer storage change and storage properties, 2010–2017, in the Big Chino Subbasin, Yavapai County, Arizona
The Big Chino Subbasin is a groundwater basin that includes the Verde River headwaters in Yavapai County in north-central Arizona. Groundwater in the southern part of the subbasin is found primarily in the Big Chino and Williamson Valleys. The former is a potential municipal water source for growing communities in Yavapai County, particularly groundwater from the Big Chino Water Ranch, about 15 miGeochemical assessment of groundwater in the Big Chino subbasin, Arizona, 2011–18
A geochemical characterization of groundwater in the Big Chino subbasin of Arizona was conducted by the U.S. Geological Survey, in cooperation with the City of Prescott, the Town of Prescott Valley, and the Salt River Project, to understand groundwater evolution through the study area and the source of water to springs along the gaining reach of the Verde River just downstream from its confluenceCharacterization of Big Chino subbasin hydrogeology near Paulden, Arizona, using controlled source audio-frequency magnetotelluric surveys
The Big Chino subbasin is located in central-northwest Arizona in the transition zone between the Colorado Plateau and the Basin and Range Province. The controlled source audio-frequency magnetotelluric (CSAMT) geophysical method, a low-impact, non-intrusive, electrical resistance sounding technique, was used to evaluate the subsurface hydrogeology of the southern third of the Big Chino subbasin.Geochemical characterization and modeling of regional groundwater contributing to the Verde River, Arizona between Mormon Pocket and the USGS Clarkdale gage
We use synoptic surveys of stream discharge, stable isotopes, and dissolved noble gases to identify the source of groundwater discharge to the Verde River in central Arizona. The Verde River more than doubles in discharge in Mormon Pocket over a 1.4 km distance that includes three discrete locations of visible spring input to the river and other diffuse groundwater inputs. A detailed study of thHydrogeology of the upper and middle Verde River watersheds, central Arizona
The upper and middle Verde River watersheds in central Arizona are primarily in Yavapai County, which in 1999 was determined to be the fastest growing rural county in the United States; by 2050 the population is projected to more than double its current size (132,000 in 2000). This study combines climatic, surface-water, ground-water, water-chemistry, and geologic data to describe the hydrogeologi - Partners
Below are partners associated with this project.