USGS groundwater well (Ma-Wkw 2R) in Wayland, Massachusetts with holiday decorations.
What is groundwater?
Groundwater is water that exists underground in saturated zones beneath the land surface. The upper surface of the saturated zone is called the water table.
Contrary to popular belief, groundwater does not form underground rivers. It fills the pores and fractures in underground materials such as sand, gravel, and other rock, much the same way that water fills a sponge. If groundwater flows naturally out of rock materials or if it can be removed by pumping (in useful amounts), the rock materials are called aquifers.
Groundwater moves slowly, typically at rates of 7-60 centimeters (3-25 inches) per day in an aquifer. As a result, water could remain in an aquifer for hundreds or thousands of years. Groundwater is the source of about 40 percent of water used for public supplies and about 39 percent of water used for agriculture in the United States.
Learn more:
Related
How important is groundwater?
How does an earthquake affect groundwater levels and water quality in wells?
If the ground filters water, is groundwater always clean?
Does the use of pesticides affect our Nation's water quality?
Where can I get my well water tested?
What determines if a well will go dry?
How much water is used by people in the United States?
How much natural water is there?
How can I find the depth to the water table in a specific location?
What is the Ground Water Atlas of the United States?
USGS groundwater well (Ma-Wkw 2R) in Wayland, Massachusetts with holiday decorations.

USGS groundwater hydrologist, Bill Eldridge, is lowering a transducer into an observation well near Jewel Cave National Monument to monitor water-level changes in the Madison aquifer. The data collected will be used to update previously published groundwater-altitude maps to help better understand groundwater flow.
USGS groundwater hydrologist, Bill Eldridge, is lowering a transducer into an observation well near Jewel Cave National Monument to monitor water-level changes in the Madison aquifer. The data collected will be used to update previously published groundwater-altitude maps to help better understand groundwater flow.

Measuring the groundwater level in a well near Lame Deer, Montana
Measuring the groundwater level in a well near Lame Deer, Montana

- Corrosive groundwater, if untreated, can dissolve lead and other metals from pipes.
- National maps have been prepared to identify the occurrence of potentially corrosive groundwater in the U.S.
- These findings have the greatest implication for the 44 million people dependent on domestic wells for drinking water.
- Corrosive groundwater, if untreated, can dissolve lead and other metals from pipes.
- National maps have been prepared to identify the occurrence of potentially corrosive groundwater in the U.S.
- These findings have the greatest implication for the 44 million people dependent on domestic wells for drinking water.
Flowing groundwater site in Indiana
Flowing groundwater site in Indiana

USGS scientist tests groundwater samples for water quality.
USGS scientist tests groundwater samples for water quality.

Setting up Groundwater Streamgage on Green River nr LaBarge
Setting up Groundwater Streamgage on Green River nr LaBarge

--issues facing current and future water supplies
by William Alley, USGS Office of Groundwater
--issues facing current and future water supplies
by William Alley, USGS Office of Groundwater
Real-time Groundwater Streamgage equipment set up
Real-time Groundwater Streamgage equipment set up

Putting in a groundwater well station on Long Island
Putting in a groundwater well station on Long Island

How Ground Water Occurs
U.S. Geological Survey National Groundwater Climate Response Network
Status of water-level altitudes and long-term and short-term water-level changes in the Chicot and Evangeline (undifferentiated) and Jasper aquifers, greater Houston area, Texas, 2023
Water-level and recoverable water in storage changes, High Plains Aquifer, predevelopment to 2019 and 2017 to 2019
Availability of groundwater from the volcanic aquifers of the Hawaiian Islands
Estimated groundwater withdrawals from principal aquifers in the United States, 2015
Water priorities for the nation—The U.S. Geological Survey next generation water observing system
The quality of our Nation's waters: Water quality in principal aquifers of the United States, 1991-2010
Groundwater studies: principal aquifer surveys
The quality of our nation's waters: Nutrients in the nation's streams and groundwater, 1992-2004
Ground-water availability in the United States
Pesticides in the nation's streams and ground water, 1992-2001 - a summary
Sustainability of ground-water resources
Related
How important is groundwater?
How does an earthquake affect groundwater levels and water quality in wells?
If the ground filters water, is groundwater always clean?
Does the use of pesticides affect our Nation's water quality?
Where can I get my well water tested?
What determines if a well will go dry?
How much water is used by people in the United States?
How much natural water is there?
How can I find the depth to the water table in a specific location?
What is the Ground Water Atlas of the United States?

USGS groundwater hydrologist, Bill Eldridge, is lowering a transducer into an observation well near Jewel Cave National Monument to monitor water-level changes in the Madison aquifer. The data collected will be used to update previously published groundwater-altitude maps to help better understand groundwater flow.
USGS groundwater hydrologist, Bill Eldridge, is lowering a transducer into an observation well near Jewel Cave National Monument to monitor water-level changes in the Madison aquifer. The data collected will be used to update previously published groundwater-altitude maps to help better understand groundwater flow.

Measuring the groundwater level in a well near Lame Deer, Montana
Measuring the groundwater level in a well near Lame Deer, Montana

- Corrosive groundwater, if untreated, can dissolve lead and other metals from pipes.
- National maps have been prepared to identify the occurrence of potentially corrosive groundwater in the U.S.
- These findings have the greatest implication for the 44 million people dependent on domestic wells for drinking water.
- Corrosive groundwater, if untreated, can dissolve lead and other metals from pipes.
- National maps have been prepared to identify the occurrence of potentially corrosive groundwater in the U.S.
- These findings have the greatest implication for the 44 million people dependent on domestic wells for drinking water.
Flowing groundwater site in Indiana
Flowing groundwater site in Indiana

USGS scientist tests groundwater samples for water quality.
USGS scientist tests groundwater samples for water quality.

Setting up Groundwater Streamgage on Green River nr LaBarge
Setting up Groundwater Streamgage on Green River nr LaBarge

--issues facing current and future water supplies
by William Alley, USGS Office of Groundwater
--issues facing current and future water supplies
by William Alley, USGS Office of Groundwater
Real-time Groundwater Streamgage equipment set up
Real-time Groundwater Streamgage equipment set up

Putting in a groundwater well station on Long Island
Putting in a groundwater well station on Long Island

How Ground Water Occurs