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.
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Related
How important is groundwater? How important is groundwater?
Groundwater, which is in aquifers below the surface of the Earth, is one of the Nation's most important natural resources. Groundwater is the source of about 37 percent of the water that county and city water departments supply to households and businesses (public supply). It provides drinking water for more than 90 percent of the rural population who do not get their water delivered to them from...
How does an earthquake affect groundwater levels and water quality in wells? How does an earthquake affect groundwater levels and water quality in wells?
Groundwater levels in wells can oscillate up and down when seismic waves pass. The water level might remain higher or lower for a period of time after the seismic waves end, but sometimes a long-term offset of groundwater levels follows an earthquake. The largest recorded earthquake-induced offset in a well is a one meter rise. Water quality can also be affected by earthquakes, typically in...
If the ground filters water, is groundwater always clean? If the ground filters water, is groundwater always clean?
Water drawn from a well was once precipitation that fell onto Earth's surface. It seeped into the ground and, over time, occupied the porous space in some subsurface material. Big particles that are in surface streams, such as leaf chunks, will not be seen in groundwater. So, yes, big particles are filtered out by the ground, along with some minerals and chemicals that are too small to see. But...
Does the use of pesticides affect our Nation's water quality? Does the use of pesticides affect our Nation's water quality?
Pesticide use in the United States has increased because not only must we supply our exploding population with food, but crops and food are also grown for export to other countries. The United States has become the largest producer of food products in the world, partly owing to our use of modern chemicals (pesticides) to control the insects, weeds, and other organisms that attack food crops. But...
Where can I get my well water tested? Where can I get my well water tested?
Some counties offer free well water testing, so check with your county first. If they don't, use this EPA website to find a list of state-certified laboratories in your area that do water testing, or contact your county or state health department or your State Certification Officer for assistance. Prices will vary depending on the laboratory and the test(s), but most people consider the cost to be...
What determines if a well will go dry? What determines if a well will go dry?
A well is said to have gone dry when water levels drop below a pump intake. This does not mean that a dry well will never have water in it again, as the water level may come back through time as recharge increases. The water level in a well depends on a number of things, such as the depth of the well, the type (confined or unconfined) of aquifer the well taps, the amount of pumping that occurs in...
USGS groundwater well (Ma-Wkw 2R) in Wayland, Massachusetts with holiday decorations.
Groundwater-Level Measurement near Jewel Cave National Monument, SD
Groundwater-Level Measurement near Jewel Cave National Monument, SDUSGS 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.
Groundwater-Level Measurement near Jewel Cave National Monument, SD
Groundwater-Level Measurement near Jewel Cave National Monument, SDUSGS 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, MontanaMeasuring the groundwater level in a well near Lame Deer, Montana
Measuring the groundwater level in a well near Lame Deer, Montana
Measuring the groundwater level in a well near Lame Deer, MontanaMeasuring the groundwater level in a well near Lame Deer, Montana
Potential Corrosivity of Untreated Groundwater in the United States
Potential Corrosivity of Untreated Groundwater in the United States- 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.
Potential Corrosivity of Untreated Groundwater in the United States
Potential Corrosivity of Untreated Groundwater in the United States- 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
USGS scientist tests groundwater samples for water quality.
USGS scientist tests groundwater samples for water quality.USGS scientist tests groundwater samples for water quality.
USGS scientist tests groundwater samples for water quality.
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 LaBargeSetting up Groundwater Streamgage on Green River nr LaBarge
Setting up Groundwater Streamgage on Green River nr LaBarge
Setting up Groundwater Streamgage on Green River nr LaBargeSetting up Groundwater Streamgage on Green River nr LaBarge
PubTalk 9/2011 — Tracking the Nation's Groundwater Reserves
PubTalk 9/2011 — Tracking the Nation's Groundwater Reserves--issues facing current and future water supplies
by William Alley, USGS Office of Groundwater
PubTalk 9/2011 — Tracking the Nation's Groundwater Reserves
PubTalk 9/2011 — Tracking the Nation's Groundwater Reserves--issues facing current and future water supplies
by William Alley, USGS Office of Groundwater
Real-time Groundwater Streamgage equipment set up
Creating a groundwater well station on Long Island
Creating a groundwater well station on Long IslandPutting in a groundwater well station on Long Island
Creating a groundwater well station on Long Island
Creating a groundwater well station on Long IslandPutting in a groundwater well station on Long Island
Groundwater is the saturated zone of soil/rock below the land surface
Groundwater is the saturated zone of soil/rock below the land surfaceHow Ground Water Occurs
Hydrogeologic mapping and three-dimensional geologic modeling of glacial deposits in a multicounty area of southeastern Michigan, northeastern Indiana, and northwestern Ohio Hydrogeologic mapping and three-dimensional geologic modeling of glacial deposits in a multicounty area of southeastern Michigan, northeastern Indiana, and northwestern Ohio
U.S. Geological Survey National Groundwater Climate Response Network 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 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 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 Availability of groundwater from the volcanic aquifers of the Hawaiian Islands
Estimated groundwater withdrawals from principal aquifers in the United States, 2015 Estimated groundwater withdrawals from principal aquifers in the United States, 2015
Related
How important is groundwater? How important is groundwater?
Groundwater, which is in aquifers below the surface of the Earth, is one of the Nation's most important natural resources. Groundwater is the source of about 37 percent of the water that county and city water departments supply to households and businesses (public supply). It provides drinking water for more than 90 percent of the rural population who do not get their water delivered to them from...
How does an earthquake affect groundwater levels and water quality in wells? How does an earthquake affect groundwater levels and water quality in wells?
Groundwater levels in wells can oscillate up and down when seismic waves pass. The water level might remain higher or lower for a period of time after the seismic waves end, but sometimes a long-term offset of groundwater levels follows an earthquake. The largest recorded earthquake-induced offset in a well is a one meter rise. Water quality can also be affected by earthquakes, typically in...
If the ground filters water, is groundwater always clean? If the ground filters water, is groundwater always clean?
Water drawn from a well was once precipitation that fell onto Earth's surface. It seeped into the ground and, over time, occupied the porous space in some subsurface material. Big particles that are in surface streams, such as leaf chunks, will not be seen in groundwater. So, yes, big particles are filtered out by the ground, along with some minerals and chemicals that are too small to see. But...
Does the use of pesticides affect our Nation's water quality? Does the use of pesticides affect our Nation's water quality?
Pesticide use in the United States has increased because not only must we supply our exploding population with food, but crops and food are also grown for export to other countries. The United States has become the largest producer of food products in the world, partly owing to our use of modern chemicals (pesticides) to control the insects, weeds, and other organisms that attack food crops. But...
Where can I get my well water tested? Where can I get my well water tested?
Some counties offer free well water testing, so check with your county first. If they don't, use this EPA website to find a list of state-certified laboratories in your area that do water testing, or contact your county or state health department or your State Certification Officer for assistance. Prices will vary depending on the laboratory and the test(s), but most people consider the cost to be...
What determines if a well will go dry? What determines if a well will go dry?
A well is said to have gone dry when water levels drop below a pump intake. This does not mean that a dry well will never have water in it again, as the water level may come back through time as recharge increases. The water level in a well depends on a number of things, such as the depth of the well, the type (confined or unconfined) of aquifer the well taps, the amount of pumping that occurs in...
Groundwater-Level Measurement near Jewel Cave National Monument, SD
Groundwater-Level Measurement near Jewel Cave National Monument, SDUSGS 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.
Groundwater-Level Measurement near Jewel Cave National Monument, SD
Groundwater-Level Measurement near Jewel Cave National Monument, SDUSGS 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, MontanaMeasuring the groundwater level in a well near Lame Deer, Montana
Measuring the groundwater level in a well near Lame Deer, Montana
Measuring the groundwater level in a well near Lame Deer, MontanaMeasuring the groundwater level in a well near Lame Deer, Montana
Potential Corrosivity of Untreated Groundwater in the United States
Potential Corrosivity of Untreated Groundwater in the United States- 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.
Potential Corrosivity of Untreated Groundwater in the United States
Potential Corrosivity of Untreated Groundwater in the United States- 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
USGS scientist tests groundwater samples for water quality.
USGS scientist tests groundwater samples for water quality.USGS scientist tests groundwater samples for water quality.
USGS scientist tests groundwater samples for water quality.
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 LaBargeSetting up Groundwater Streamgage on Green River nr LaBarge
Setting up Groundwater Streamgage on Green River nr LaBarge
Setting up Groundwater Streamgage on Green River nr LaBargeSetting up Groundwater Streamgage on Green River nr LaBarge
PubTalk 9/2011 — Tracking the Nation's Groundwater Reserves
PubTalk 9/2011 — Tracking the Nation's Groundwater Reserves--issues facing current and future water supplies
by William Alley, USGS Office of Groundwater
PubTalk 9/2011 — Tracking the Nation's Groundwater Reserves
PubTalk 9/2011 — Tracking the Nation's Groundwater Reserves--issues facing current and future water supplies
by William Alley, USGS Office of Groundwater
Real-time Groundwater Streamgage equipment set up
Creating a groundwater well station on Long Island
Creating a groundwater well station on Long IslandPutting in a groundwater well station on Long Island
Creating a groundwater well station on Long Island
Creating a groundwater well station on Long IslandPutting in a groundwater well station on Long Island
Groundwater is the saturated zone of soil/rock below the land surface
Groundwater is the saturated zone of soil/rock below the land surfaceHow Ground Water Occurs