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Groundwater Level Hydrograph




Point IDEB-019
Alternate Site ID353358106054301
Formation112ANCH Formation LookUp
Elevation (ft ASL)6140
Well Depth (ft BGS)80
UTM Easting*400304
UTM Northing*3935932

* 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
1973-06-12 00:00:00 41.54 Water level not affected by status Reported, method not known Another agency
1983-03-10 00:00:00 40.05 Water level not affected by status Reported, method not known Another agency
1988-03-17 00:00:00 40.82 Water level not affected by status Reported, method not known Another agency
1989-02-11 00:00:00 40.89 Water level not affected by status Reported, method not known Another agency
1991-07-01 00:00:00 43.9 Water level not affected by status Reported, method not known Private geologist, consultant or university associate
1992-07-01 00:00:00 41.8 Water level not affected by status Reported, method not known Private geologist, consultant or university associate
1993-02-02 00:00:00 41.47 Water level not affected by status Reported, method not known Another agency
1993-07-01 00:00:00 41.7 Water level not affected by status Reported, method not known Private geologist, consultant or university associate
1994-07-01 00:00:00 42.1 Water level not affected by status Reported, method not known Private geologist, consultant or university associate
1995-07-18 00:00:00 41.9 Water level not affected by status Reported, method not known Private geologist, consultant or university associate
2003-01-22 00:00:00 43.2 Water level not affected by status Steel-tape measurement NMBGMR NMBGMR
2004-03-23 00:00:00 43.34 Water level not affected by status Electric tape measurement (E-probe) NMBGMR NMBGMR
2011-10-05 00:00:00 44.85 Water level not affected by status Steel-tape measurement NMBGMR NMBGMR Water level accurate to within two hundreths of a foot
2012-02-14 00:00:00 44.2 Water level not affected by status Steel-tape measurement NMBGMR NMBGMR Water level accurate to within two hundreths of a foot
2015-04-14 00:00:00 44.46 Water level not affected by status Steel-tape measurement NMBGMR NMBGMR Water level accurate to within two hundreths of a foot
2015-10-05 00:00:00 45.16 Water level not affected by status Steel-tape measurement NMBGMR NMBGMR Water level accurate to within two hundreths of a foot
2016-04-05 00:00:00 44.36 Water level not affected by status Steel-tape measurement NMBGMR NMBGMR Water level accurate to within two hundreths of a foot
2016-10-05 00:00:00 45.28 Water level not affected by status Steel-tape measurement NMBGMR NMBGMR Water level accurate to within two hundreths of a foot
2017-04-05 15:47:00 44.42 Water level not affected by status Steel-tape measurement NMBGMR NMBGMR Water level accurate to within two hundreths of a foot
2017-10-18 16:12:00 45.13 Water level not affected by status Steel-tape measurement NMBGMR NMBGMR Water level accurate to within two hundreths of a foot
2018-04-10 10:27:00 44.51 Water level not affected by status Steel-tape measurement NMBGMR NMBGMR Water level accurate to within two hundreths of a foot
2019-04-17 16:29:00 44.42 Water level not affected by status Steel-tape measurement NMBGMR NMBGMR Water level accurate to within two hundreths of a foot
2020-05-19 13:38:00 44.64 Water level not affected by status Steel-tape measurement NMBGMR NMBGMR Water level accurate to within two hundreths of a foot
2021-04-21 10:09:00 44.66 Water level not affected by status Steel-tape measurement NMBGMR NMBGMR Water level accurate to within two hundreths of a foot
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