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Water is naturally stored below the surface of the ground between the cracks and fractures in 'pools' refered to as aquifiers. The depth at which water is found is considered to be the water table. In fact, there is more water under us in the water table than all the surface water across groundwaters and lakes combined. This is the reason that groundwater is the primary source for 'useable' water in the nation.
| USGS Site | State | 24hr Change (%) | vs Average (%) | Volatility (%) |
|---|---|---|---|---|
|
MT-49 OH
USGS 394025084162800 |
Ohio | -0.34 | 12.34 | 11.38 |
|
MT-426 OH
USGS 394442084111600 |
Ohio | -0.31 | 12.51 | 11.26 |
|
MT-6 OH
USGS 394533084113800 |
Ohio | -0.31 | -39.05 | 3.5 |
|
FR-366
USGS 394903083015400 |
Ohio | -1.15 | -22.01 | 3.54 |
|
MT-73 OH
USGS 394915084103300 |
Ohio | -0.47 | -8.8 | 10.57 |
|
MU-3 OH
USGS 394933081441701 |
Ohio | 0.19 | -7.78 | 5.66 |
|
FR-126 M13
USGS 395008082593100 |
Ohio | 0.65 | -8.25 | 9.23 |
|
FR-115 TH-67
USGS 395039082585800 |
Ohio | None | None | None |
|
FR-271 PARSONS AVE WTP DEEP WELL AT COLUMBUS OH
USGS 395055082592400 |
Ohio | None | None | None |
|
FR-272 PARSONS AVE WTP SHALLOW WELL AT COLUMBUS OH
USGS 395055082592401 |
Ohio | None | None | None |
|
CL-11 OH
USGS 395316083593100 |
Ohio | -27.13 | -25.4 | 28.61 |
|
MI-3A OH
USGS 395847084085500 |
Ohio | -4.9 | -3 | 6.87 |
|
FR-523 AT NGWA
USGS 400540082540400 |
Ohio | -0.81 | -3.54 | 2.98 |
|
MI-43 OH
USGS 401122084143400 |
Ohio | -5.15 | -3.01 | 12.93 |
|
SH-5 OH
USGS 401707084103100 |
Ohio | -0.21 | 0.48 | 1.94 |
|
HN-2A OH
USGS 404648083412600 |
Ohio | -1.66 | 3.38 | 7.25 |
|
WN-8 OH
USGS 404655081553100 |
Ohio | -0.28 | -1.15 | 3.07 |
|
ST-33
USGS 405843081182300 |
Ohio | 0 | 0.55 | 1.64 |