Scientific Investigations Report 2004–5270
By Stephen L. Harden, Stephen S. Howe, and Silvia Terziotti
Local well name | Land-surface altitude (ft) |
Depth to water (ft BLS) |
Water-level altitude (ft) |
---|---|---|---|
G10MW1 | 42.56 | 5.72 | 36.84 |
G10MW2 | 16.34 | 3.82 | 12.52 |
G10MW3 | 41.02 | 5.91 | 35.11 |
G10MW4 | 17.42 | 6.29 | 11.13 |
G10MW5 | 33.38 | 13.01 | 20.37 |
G10MW6 | 38.27 | 3.74 | 34.53 |
G10MW7 | 42.47 | 4.45 | 38.02 |
G10MW8 | 29.18 | 10.62 | 18.56 |
G10MW9 | 29.33 | 10.39 | 18.94 |
G10MW10 | 36.08 | 5.28 | 30.80 |
G10MW11 | 39.87 | 3.37 | 36.50 |
G10MW12 | 52.19 | 5.78 | 46.41 |
G10MW13 | 43.70 | 4.39 | 39.31 |
K2MW1 | 21.79 | 7.31 | 14.48 |
K2MW2 | 12.52 | 7.79 | 4.73 |
K2MW3 | 24.49 | 6.30 | 18.19 |
K2MW4 | 32.15 | 1.12 | 31.03 |
K2MW5 | 21.49 | 8.39 | 13.10 |
K2MW6 | 27.79 | 2.03 | 25.76 |
K2MW7 | 24.64 | 3.18 | 21.46 |
K2MW8 | 2.57 | 1.20a | 1.37 |
K2MW9 | 1.99 | 2.95a | -0.96 |
ON-294 | 29.83 | 4.53 | 25.30 |
a Because of access restrictions at site K-2, it was not possible to measure the water levels at wells K2MW8 and K2MW9 on August 23, 2004, when all other wells were measured; thus, it was necessary to use the water levels obtained during installation of wells K2MW8 and K2MW9 on February 11, 2004, and March 11, 2004, respectively. Based on the low land-surface altitude and position of wells K2MW8 and K2MW9 along the New River (fig. 4), the magnitude of seasonal water-level change at these sites is likely similar to the tidal fluctuation of about 2 feet for the New River. The water levels utilized for wells K2MW8 and K2MW9 in developing the regression equation for estimating water-table altitudes at the Impact Areas are considered to be fairly represen-tative of those that would have been obtained on August 23, 2004, when the other wells were measured.
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