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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 (%) |
|---|---|---|---|---|
|
Sh:M-040
USGS 350406089444401 |
Tennessee | -0.09 | -7.11 | 3.7 |
|
Sh:L-089
USGS 350506089483101 |
Tennessee | 0.04 | -3.1 | 1.89 |
|
Sh:P-076
USGS 350735089593300 |
Tennessee | -0.02 | -9.27 | 6.82 |
|
Sh:P-099
USGS 350857089591401 |
Tennessee | 0 | -12.1 | 7.9 |
|
Sh:Q-001
USGS 350900089482300 |
Tennessee | 0.05 | -5.56 | 3.12 |
|
SH:Q-094
USGS 351111089512501 |
Tennessee | 0.04 | -3.67 | 2.11 |
|
SH:Q-186
USGS 351113089513401 |
Tennessee | 0 | 1.88 | 0.87 |
|
Ld:F-004
USGS 353839089493500 |
Tennessee | 0.01 | -0.27 | 0.78 |
|
Sv:E-002
USGS 353922083345600 |
Tennessee | -3.36 | -5.05 | 3.54 |
|
Ld:J-006 WU
USGS 354213089282401 |
Tennessee | None | None | None |