Click
to
hide
Water-Year
Summary
instructions
and
information
- Water-Year Summary reports summarize a year of hydrologic data in a printer-friendly format.
- For water years 2014 onward, choose a water year and parameter and an on-demand Water-Year Summary report will be generated.
- For water years 2006 through 2013, choose a water year and an Annual Water Data Report will be provided.
- For water years 2005 and earlier, Annual Water Data Reports may be available in digital format.
- Not all sites have reports available for every water year.
USGS Water-Year Summary 2024
424158076251901 Cy-7, near Moravia NY
Sand and gravel aquifers (glaciated regions)
Lake Deposits
Lake Deposits
LOCATION - Lat 42°41'58.3", long 76°25'17.8" referenced to North American Datum of 1983, Cayuga County, NY, Hydrologic Unit 04140201, near Moravia.
GROUNDWATER RECORDS
WELL CHARACTERISTICS - Depth 28 ft. Upper casing diameter 2.5 in; top of first opening 25.8 ft, bottom of last opening 27.8 ft. Cased to 27.8 ft (screen, 25.8 ft to 27.8 ft). Elevation of land-surface datum is 760.70 ft above NGVD of 1929 and 760.23 ft above NAVD of 1988.
DATUM - Land-surface datum is 760.23 ft above North American Vertical Datum of 1988. Measuring point: Top of shelter shelf, 3.13 ft above land-surface datum, Jun. 26, 2016 to present.
PERIOD OF RECORD - December 1965 to August 1995 and July 2003 to current year. Records for December 1965 to September 1976 are unpublished and available in files of the U.S. Geological Survey. Prior to February 22, 1989, weekly measurements by observer.
GAGE - Water-stage recorder--15 minute; periodic measurements by USGS personnel.
REMARKS - Recorded water levels were below transducer on many days in 2012, September 26 to October 3, 2020, and October 11 to October 20, 2020, record not used. Satellite water-level telemeter at station.
EXTREMES FOR PERIOD OF RECORD - Highest water level measured, 11.91 ft, below land-surface datum, June 26, 1972; lowest water level measured, 25.00 ft below land-surface datum, Sept. 19, 1983, and may have been lower when water levels were below transducer (see REMARKS).
