Warning: Javascript must be enabled to use all the features on this page!

Page Loading - Please Wait...

Click to hideNews Bulletins
  • The issue impacting the delivery of satellite data transmissions in the western United States has been resolved. Current data for impacted locations are now accessible from USGS web portals. The data to fill any resultant gaps in water records will be downloaded from field equipment for manual upload following the next scheduled field visit.
  • Explore the NEW USGS National Water Dashboard interactive map to access real-time water data from over 13,500 stations nationwide.
  • Full News RSS icon

Water-Year Summary for Site 410401112134801

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.
Available Parameters
00010 Temperature, water(Min.,Mean,Max.)  
00060 Discharge(Mean)  
00095 Specific cond at 25C(Mean,Min.,Max.)  

Water year 2020: 2019-10-01 to 2020-09-30

Print this page
USGS Water-Year Summary 2020
LOCATION - Lat 41°04'01", long 112°13'48" referenced to North American Datum of 1927, Davis County, UT, Hydrologic Unit 16020310, near west end of Antelope Island State Park causeway, about 9 miles west-southwest of Syracuse .
DRAINAGE AREA - Not determined.
PERIOD OF RECORD - October 2003 to current year.
GAGE - Water-stage recorder and acoustic velocity meter.
REMARKS - Records poor. Flow between Farmington Bay and Great Salt Lake is mainly controlled by the water surface elevation of Great Salt Lake (GSL) near the causeway bridge, but flow is also affected by wind. Under calm conditions, flow generally occurs from Farmington Bay to GSL. Depending upon the wind velocity, flow at the causeway bridge can increase from Farmington Bay into GSL, or reverse (flow occurs from GSL into Farmington Bay) which is represented by negative discharges.
EXTREMES FOR PERIOD OF RECORD - Maximum daily discharge, 1,620 ft³/s, May 31, 2011; minimum daily discharge, -2,710 ft³/s, Jun 7, 2007.