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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 (%) |
---|---|---|---|---|
06S-21E-27 AAA 1 MCCURTAIN 27
USGS 340042095051801 |
Oklahoma | 0 | -1.23 | 2.69 |
02S-06E-11 DDA 1 ARB08
USGS 342336096381201 |
Oklahoma | None | None | None |
02S-07E-06 BAA 2 SIMP02
USGS 342510096363901 |
Oklahoma | None | None | None |
01S-07E-26 DAD 1 SIMP01
USGS 342616096315501 |
Oklahoma | None | None | None |
01S-06E-25 CBD 1 ARB03
USGS 342618096380101 |
Oklahoma | None | None | None |
01S-06E-11 AAD 1 ARB07
USGS 342921096381601 |
Oklahoma | None | None | None |
13N-23E-34 BCB 1 Roubidoux9
USGS 353341094513501 |
Oklahoma | None | None | None |
13N-24E-10 CBB 1 Roubidoux5
USGS 353513094482401 |
Oklahoma | 0.41 | 1.23 | 2.92 |