Groundwater Level Hydrograph




Point IDEB-014
Alternate Site ID353749105580801
Formation121TSUQs Formation LookUp
Elevation (ft ASL)6827
Well Depth (ft BGS)300
UTM Easting*412216
UTM Northing*3943495

* UTM coordinates in Zone 13, NAD83

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Date Depth To Water
Continuous (ft BGS)
Depth To Water
Manual (ft BGS)
Status Measurement Method Data Source Measuring Agency Data Quality
1992-07-07 00:00:00 213.4 Water level not affected by status Steel-tape measurement Private geologist, consultant or university associate
1993-07-01 00:00:00 214.4 Water level not affected by status Reported, method not known Private geologist, consultant or university associate
1994-07-12 00:00:00 210.5 Water level not affected by status Reported, method not known Private geologist, consultant or university associate
1995-07-01 00:00:00 231.12 Water level not affected by status Reported, method not known Private geologist, consultant or university associate
2004-04-30 00:00:00 222.52 Water level not affected by status Steel-tape measurement NMBGMR NMBGMR
2005-03-28 00:00:00 240.39 Water level not affected by status Steel-tape measurement Another agency USGS Water level accurate to nearest tenth of a foot (USGS accuracy level)
2005-03-29 00:00:00 240.39 Water level not affected by status Steel-tape measurement Private geologist, consultant or university associate
2005-10-25 00:00:00 222.1 Water level not affected by status Reported, method not known Another agency
2006-03-15 00:00:00 222.45 Water level not affected by status Steel-tape measurement Private geologist, consultant or university associate
2006-09-06 00:00:00 222.33 Water level not affected by status Reported, method not known Another agency
2007-05-18 00:00:00 223.75 Water level not affected by status Steel-tape measurement Another agency
2008-10-02 00:00:00 225.38 Water level not affected by status Steel-tape measurement Another agency
2009-02-04 00:00:00 225.68 Water level not affected by status Steel-tape measurement Another agency
2010-02-18 00:00:00 226.46 Water level not affected by status Steel-tape measurement Another agency
2011-03-10 00:00:00 226.24 Water level not affected by status Steel-tape measurement Another agency
2012-01-13 00:00:00 227.3 Water level not affected by status Electric tape measurement (E-probe) Another agency
2013-02-11 00:00:00 228.35 Water level not affected by status Steel-tape measurement Another agency Water level accurate to within two hundreths of a foot
2014-02-26 00:00:00 229.54 Water level not affected by status Steel-tape measurement Another agency Water level accuracy not to nearest foot or water level not repeatable
2015-02-16 00:00:00 229.06 Water level not affected by status Steel-tape measurement Another agency USGS Water level accurate to nearest one-hundredth of a foot (USGS accuracy level)
Disclaimer:
At NMBGMR, we use different tools to collect groundwater level measurements, including continuous data recorders and manual measurements. All data provided here are in feet, depth to water, below ground surface (BGS). We use pressure transducers to record pressure of water over a device installed in the well, which is converted to feet of water and depth to water. We provide here up to one measurement per hour where the data are that frequent. In some locations we have more data available. We also use continuous acoustic sounder devices which convert a sound reflection into a measurement of depth to water. These can be used for long term trends in groundwater levels. While we do our best to review and quality check these data, please use these data with caution. Site-specific conditions should be verified, especially for legally binding decisions. Data are subject to changes, deletion, or being moved without notice at any time and should not be relied on for any critical application. Any opinions expressed may not necessarily reflect the official position of the New Mexico Bureau of Geology, New Mexico Tech, or the State of New Mexico. No warranty expressed or implied, is made regarding the accuracy or utility of the data for general or scientific purposes.

For more information on this project contact Stacy Timmons or Cathryn Pokorny