2 edition of Availability of ground water in York County, Nebraska found in the catalog.
Availability of ground water in York County, Nebraska
C.F Keech
Published
1967
by U.S. Government Printing Office in Washington, DC
.
Written in
Edition Notes
| Statement | by C.F. Keech, V.H. Dreeszen, and P.A. Emery. |
| Series | Contributions to the hydrology of the United States, U.S. Geological Survey water-supply paper -- 1839-F |
| Contributions | Dreeszen, V.H., Emery, P.A., Geological Survey (U.S.) |
| The Physical Object | |
|---|---|
| Pagination | iii, 17 p. : |
| Number of Pages | 17 |
| ID Numbers | |
| Open Library | OL20575356M |
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The York County Water and Sewer Department operates and maintains water and sewer systems in defined service areas in eastern York County and western York County. The department purchases water from the City of Rock Hill. The county has in excess of 10, retail customers in its service areas.
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Below, find data and tools relevant to a wide range of water resources and conditions including streamflow, groundwater, water quality, and water use and. The Natural Resources Data Bank, statutorily created inis administered by the Department of Natural Resources.
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LandWatch has hundreds of farms, ranches and other land for sale in York County. York County is in Pennsylvania's Dutch Country Roads region. Based on recent LandWatch data, York County, Pennsylvania ranks 21st among the 67 counties in the state for its total acres of farms, ranches and other land currently advertised forLocation: York County, PA.
The Ogallala Aquifer (oh-guh-LAH-luh) is a shallow water table aquifer surrounded by sand, silt, clay, and gravel located beneath the Great Plains in the United States.
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Aquifers: Ground Water Atlas of the United States. The Ground Water Atlas of the United States, USGS Hydrologic Atlas (Miller, ), describes the location, hydrologic characteristics, and geologic characteristics of the principal aquifers throughout the 50 States, Puerto Rico, and the U.S.
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Pick the perfect room & save. Skip to main content. Welcome to We can only book a single room if a reservation includes children. For assistance with your booking, please call Ground water is always moving by the force of gravity from recharge areas to discharge areas.
Ground-water movement in most areas is slow-a few feet per year. But, in more permeable zones, such as solution channels in limestone, movement can be as much as several feet per day.
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Here you'll find current best sellers in books, new releases in books, deals in books, Kindle eBooks, Audible audiobooks, and so much more.Come and join us from a.m. - 3 p.m. on Monday, March 2nd, at the Eastern Nebraska Research and Extension Center ( County Road G, Ithaca, NE) for the .The USGS annually monitors groundwater levels in thousands of wells in the United States.
Groundwater level data are collected and stored as either discrete field-water-level measurements or as continuous time-series data from automated recorders. Data from some of the continuous record stations are relayed to USGS offices nationwide through telephone lines or by satellite transmissions.
