Winter Water Level Measurements

whitworth measuring HPWD field personnel have completed the 2014 water level measurements in a network of more than 1,400 privately-owned water wells within the district's 16-county service area.  These measurements reflect 2013 groundwater pumpage.

In previous years, the results of the annual water level measurements were presented in a special issue of The Cross Section, the district's monthly newsletter.  Beginning in 2014, these data are presented in a 76-page magazine-style report.  

 

NOTE:  Persons on the newsletter mailing list will receive the water level measurement report.

NEW:  Click here to view the 2014 HPWD Water Level Measurements report

NEW:  Click here for a chart with the average changes in depth-to-water (feet of change) for 2013 from observation wells in the HPWD.

The first extensive water-level measuring effort in the region was conducted as part of the Federal Work Project Administration (WPA) in the late 1930s. Depth-to-water measurements were made in almost every well in each county in the High Plains. The results of these measurements were published in individual county reports. After the WPA work was completed, depth-to-water level measurements were made annually in a few wells by the U.S. Geological Survey or the State Board of Water Engineers until the creation of the Water District in 1951.

After that time, the District created its own measuring program, and by 1957, had taken over the federal and state water level measuring efforts in the counties it serves. Municipal pumps that were tested reflected similar problems, and when repaired, the energy costs were significantly reduced.

In the early 1950s, people had the perception that the Ogallala Aquifer was a huge underground lake being fed (recharged) from snow melt from the Rocky Mountains in New Mexico and Colorado. There was considerable water waste since people believed that an aquifer held an unlimited water supply.

Historically, observation well data has been used to show water users that the water supply is indeed exhaustible and that if water waste continued (similar to that in the 1950s) the aquifer would be depleted before 1985. However, this has not occurred due to the development and acceptance of new water conservation practices within the district.