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


Page Loading - Please Wait...

Click to hideNews Bulletins

Water-Year Summary for Site 361334120035101

Click to hide state-specific text

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
50012 Compaction, aquifer system(Max.,Min.,Med.) [Cumulative since 1/11/1965]  
50012 Compaction, aquifer system(Min.,Med.,Max.) [Cumulative since 4/4/2012]  
72019 Water level, depth LSD(Max.,Min.,Med.)  

Water year 2024: 2024-10-01 to 2025-09-30
 

Print this page
USGS Water-Year Summary 2024
361334120035101 020S018E06D001M
Central Valley aquifer system
Alluvium Below E-Clay (Miocene-Pleistocene)
LOCATION - Lat 36°13'34.7", long 120°03'54.6" referenced to North American Datum of 1983, in NW 1/4 NW 1/4 sec.06, T.20 S., R.18 E., Fresno County, CA, Hydrologic Unit 18030012,
GROUNDWATER RECORDS
WELL CHARACTERISTICS - Depth 1,007 ft. Upper casing diameter 6 in; top of first opening 716 ft, bottom of last opening 872 ft.
DATUM - Land-surface datum is 327 ft above North American Vertical Datum of 1988. Measuring point: Undefined, 1.0 ft above land-surface datum, Dec. 1, 1964 to Nov. 2, 2011; Top of concrete shelter foundation, 0 ft above land-surface datum, Nov. 1, 2011 to present.
PERIOD OF RECORD -

Water years 1964 to current year.

GAGE -

Electronic data logger and pressure sensor; potentiometer and dial gage

REMARKS -

Record is rated excellent. Sudden water-level changes may be attributed to nearby anthropogenic effects such as pumping and sampling or natural events such as earthquakes. The effects of friction in the extensometer apparatus, likely caused by contact between the extensometer cable and the casing, are evident periodically in the record by periods of little change which are terminated by small vertical offsets, which resulted in a frictional deadband in the record. The friction was sometimes overcome without intervention but sometimes was overcome by manually oscillating the cable during field visits, which involved applying force to the cable to free it from the friction. Therefore, the magnitude of compaction that occurred during periods of friction was recorded when the friction was overcome; however, the time delay between actual compaction and recording of the compaction during these periods is unknown.

 Site consists of 1 continuous record groundwater well and 1 subsidence monitoring site, located in a building.

PERIOD OF DAILY RECORD -

April 2012 to current year.

EXTREMES FOR PERIOD OF RECORD -

Highest daily maximum water level recorded, 245.25 ft depth to water below land surface, Jan 5, 1984; lowest daily minimum water level recorded, 626.76 ft depth to water below land surface, Aug 11, 2015.