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Groundwater Level Hydrograph




Point IDSO-0189
Alternate Site ID---
Formation--- Formation LookUp
Elevation (ft ASL)4555
Well Depth (ft BGS)22
UTM Easting*328859
UTM Northing*3755359

* UTM coordinates in Zone 13, NAD83

Export CSV
Date Depth To Water
Continuous (ft BGS)		 Depth To Water
Manual (ft BGS)		 Status Measurement Method Data Source Measuring Agency Data Quality
2016-04-12 00:00:00 8.32 Water level not affected by status Reported, method not known Another agency NMISC
2016-09-22 00:00:00 14.1 Water level not affected by status Electric tape measurement (E-probe) NMBGMR NMBGMR Water level accurate to within two hundreths of a foot
2017-05-02 13:43:00 6.3 Water level not affected by status Electric tape measurement (E-probe) NMBGMR NMBGMR Water level accurate to within two hundreths of a foot
2017-10-09 13:45:00 9.54 Water level not affected by status Electric tape measurement (E-probe) NMBGMR NMBGMR Water level accurate to within two hundreths of a foot
2018-04-11 12:09:00 10.71 Water level not affected by status Electric tape measurement (E-probe) NMBGMR NMBGMR Water level accurate to within two hundreths of a foot
2018-11-29 15:13:00 12.26 Water level not affected by status Electric tape measurement (E-probe) NMBGMR NMBGMR Water level accurate to within two hundreths of a foot
2020-10-02 00:00:00 14.6 Water level not affected by status Electric tape measurement (E-probe) NMBGMR NMBGMR Water level accurate to within two hundreths of a foot
2020-11-13 00:00:00 12.88 Water level not affected by status Electric tape measurement (E-probe) NMBGMR NMBGMR Water level accurate to within two hundreths of a foot
2020-12-15 00:00:00 10.11 Water level not affected by status Electric tape measurement (E-probe) NMBGMR NMBGMR Water level accurate to within two hundreths of a foot
2021-01-20 13:40:00 8.57 Water level not affected by status Electric tape measurement (E-probe) NMBGMR NMBGMR Water level accurate to within two hundreths of a foot
2021-02-14 08:05:00 8.29 Water level not affected by status Electric tape measurement (E-probe) NMBGMR NMBGMR Water level accurate to within two hundreths of a foot
2021-03-13 15:17:00 7.99 Water level not affected by status Electric tape measurement (E-probe) NMBGMR NMBGMR Water level accurate to within two hundreths of a foot
2021-04-09 15:55:00 9.11 Water level not affected by status Electric tape measurement (E-probe) NMBGMR NMBGMR Water level accurate to within two hundreths of a foot
2021-05-07 17:30:00 7.66 Water level not affected by status Electric tape measurement (E-probe) NMBGMR NMBGMR Water level accurate to within two hundreths of a foot
2021-06-18 19:00:00 9.01 Water level not affected by status Electric tape measurement (E-probe) NMBGMR NMBGMR Water level accurate to within two hundreths of a foot
2021-07-14 10:50:00 11.04 Water level not affected by status Electric tape measurement (E-probe) NMBGMR NMBGMR Water level accurate to within two hundreths of a foot
2021-08-20 14:48:00 13.5 Water level not affected by status Electric tape measurement (E-probe) NMBGMR NMBGMR Water level accurate to within two hundreths of a foot
2021-09-19 10:45:00 Site was dry Electric tape measurement (E-probe) NMBGMR NMBGMR Water level accurate to within two hundreths of a foot
2021-10-25 07:25:00 Site was dry Electric tape measurement (E-probe) NMBGMR NMBGMR Water level accurate to within two hundreths of a foot
2021-11-13 12:33:00 Site was dry Electric tape measurement (E-probe) NMBGMR NMBGMR Water level accurate to within two hundreths of a foot
2022-02-03 10:55:00 Site was dry Electric tape measurement (E-probe) 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