A groundwater irrigation well supplies water to a small channel in southern Oregon.
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 this aquifer, and the amount of recharge occurring. Wells screened in unconfined water table aquifers are more directly influenced by the lack of rain than those screened in deeper confined aquifers. A deep well in a confined aquifer in an area with minimal pumping is less likely to go dry than a shallow, water table well.
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Related
How important is groundwater?
What is groundwater?
How can I find the depth to the water table in a specific location?
What is the Ground Water Atlas of the United States?
A groundwater irrigation well supplies water to a small channel in southern Oregon.
The USGS installs a sensor to monitor groundwater levels in real time at a well located at the City University of New York, York College campus.
The USGS installs a sensor to monitor groundwater levels in real time at a well located at the City University of New York, York College campus.
Flowing groundwater site in Indiana
Flowing groundwater site in Indiana
Flowing well used for stock water, Green River Basin
Flowing well used for stock water, Green River Basin

--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
This month we highlight a new interactive map that allows users to determine the depth to groundwater at any location in the Portland Metropolitan Area, Oregon. This month's episode features an interview with the groundwater project's lead author, USGS hydrologist Daniel Snyder.
Irrigation well in northeastern Arkansas (U.S. Geological Survey photograph by Terrance W. Holland, 2009).
Irrigation well in northeastern Arkansas (U.S. Geological Survey photograph by Terrance W. Holland, 2009).
U.S. Geological Survey National Groundwater Climate Response Network
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
Climate change: evaluating your local and regional water resources
Estimated use of water in the United States in 2010
Summary of estimated water use in the United States in 2010
Groundwater studies: principal aquifer surveys
Land subsidence in the United States
Sustainability of ground-water resources
Land subsidence in the United States
Ground water and the rural homeowner
Related
How important is groundwater?
What is groundwater?
How can I find the depth to the water table in a specific location?
What is the Ground Water Atlas of the United States?
A groundwater irrigation well supplies water to a small channel in southern Oregon.
A groundwater irrigation well supplies water to a small channel in southern Oregon.
The USGS installs a sensor to monitor groundwater levels in real time at a well located at the City University of New York, York College campus.
The USGS installs a sensor to monitor groundwater levels in real time at a well located at the City University of New York, York College campus.
Flowing groundwater site in Indiana
Flowing groundwater site in Indiana
Flowing well used for stock water, Green River Basin
Flowing well used for stock water, Green River Basin

--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
This month we highlight a new interactive map that allows users to determine the depth to groundwater at any location in the Portland Metropolitan Area, Oregon. This month's episode features an interview with the groundwater project's lead author, USGS hydrologist Daniel Snyder.
Irrigation well in northeastern Arkansas (U.S. Geological Survey photograph by Terrance W. Holland, 2009).
Irrigation well in northeastern Arkansas (U.S. Geological Survey photograph by Terrance W. Holland, 2009).