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<br />/'0" ". ~ ~ Q' <br />.';, " . <br />:\;,'..J '-J J.-\ <br /> <br />DESCRIPTION OF DATA <br /> <br />For a number of years, the U.S. Geological Survey and various State and <br />local agencies have cooperated in the measurement of water levels in many of <br />the wells that are located in the northern High Plains of Colorado. Since its <br />inception, this network of wells has changed almost annually. Because some <br />wells simply are more difficult to measure than others, their measurement may <br />be discontinued when consistently accurate water levels are not obtained. <br />Wells also are dropped from the measurement list if measurements cannot be <br />obtained. Some reasons for not being able to measure the water levels are: <br />access to the well is obstructed; the well is destroyed; the water level has <br />dropped below the bottom of the well; or a well owner has withdrawn permission <br />to measure the well. Wells may be added to the network, as resources permit, <br />to provide needed additional information. <br /> <br />The current (1987) water-level monitoring network consists of 641 wells; <br />637 were measured during the winter of 1986-87. Most of these wells are used <br />for irrigation, but several livestock wells and U.S. Government observation <br />wells also are included, especially in areas where there is minimal irriga- <br />tion. <br /> <br />The data in this report are arranged first by county; the counties are <br />listed alphabetically. The wells in each county then are arranged by local <br />well number, in ascending order. <br /> <br />Hydrographs for each of the 641 observation wells in the northern High <br />Plains of Colorado are shown in figure 3 in the "Hydrologic Data" section <br />of this report. A hydrograph is a diagram representing successive water-level <br />measurements throughout a period of time. The hydrographs in figure 3 include <br />measurements made during 1970 through the winter of 1986-87. The line connec- <br />ting the measurements on the hydro graph does not necessarily indicate the <br />actual water level between measurements, but may indicate a trend in the water <br />level. The actual water level between measurements will fluctuate depending <br />on the drawdown of the water table caused by pumpage and on recharge that <br />occurs. <br /> <br />Descriptive information for each well and water-level measurements made <br />during the winter of 1986-87 are listed in table 1. For various reasons, <br />water levels were not obtained during this period for four of the wells, and <br />more than one water level was obtained for other wells. <br /> <br />SELECTED REFERENCES <br /> <br />Blattner, J.L., and Rasmuson, B.D., 1982, Water-level records for the <br />northern High Plains of Colorado, 1978-82: U.S. Geological Survey <br />Open-File Report 82-573, 28 p. <br />1983, Water-level records for the northern High Plains of Colorado, <br />-----1979-83: U.S. Geological Survey Open-File Report 83-253, 34 p. <br />Boettcher, A.J., Hofstra, W.E., and Major, T.J., 1969, Water-level records for <br />the northern High Plains of Colorado: Denver, Colorado Water Conserva- <br />tion Board Ground Water Basic-Data Release No. 20, 189 p. <br />Borman, R.G., 1978, Water-level records for the northern High Plains of <br />Colorado, 1974-78: U.S. Geological Survey Open-File Report 78-499, 31 p. <br /> <br />5 <br />