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Confining Beds Piezometer CWO2-A | |
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County: | Carlton |
Township: | Red Clover (T49N R20W) |
Location: | In mowed/fenced area, west of Villa Court Senior Living building |
Land-surface elevation: | 1332.28 feet, NAVD88 |
Installation: | 9 July 2015, by the USGS |
Well information | |
This piezometer is the shallowest till-screened piezometer of a 5-well nest referred to as "CWO2" (also referred to as "Cromwell Near Nest"). This piezometer is screened in a glacial till layer, which is the confining unit above where nearby city wells pump from a confined aquifer. | |
Depth: | 35.17 feet |
Open interval: | 32.30–34.96 feet |
Original & current use: | monitoring, USGS Confining Beds Hydrology study |
Aquifer information | |
Type: | screened in glacial till layer; no contributing aquifer |
This site was operated (2015-2017) in cooperation with the Environment and Natural Resources Trust Fund, Iowa State University, Minnesota Geological Survey, and the U.S. Geological Survey.
Water levels below land surface are accurate to 0.01 feet. Water levels above National American Vertical Datum of 1988 (sea level) are calculated by subtracting recorded water levels from the land surface elevation, which is accurate only to ± 0.1 feet based on a differential GPS survey and an optical level survey. Water-level differences are accurate to within 0.01 feet.
Water temperatures are accurate to ± 0.1°C.
Precipitation is accurate to 0.01 inches except during freezing periods (about Dec. through early Apr.). The rain gage is unheated and uncovered. The precipitation data during freezing periods result from melting of snow (accumulated in the rain gage) during warm periods and do NOT represent actual precipitation. Precipitation totals during freezing periods May underestimate actual totals because the rain gage funnel may be full of snow (preventing further accumulation) or because snow in the funnel may sublimate instead of melt.