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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 (%) |
|---|---|---|---|---|
|
02N 31E 35DCC1 USGS 1
USGS 432700112470801 |
Idaho | 0.01 | 0.3 | 0.18 |
|
02N 28E 35AAC1 USGS 9
USGS 432740113044501 |
Idaho | -0.01 | -0.22 | 0.18 |
|
03N 02E 11BACD1
USGS 433700116111001 |
Idaho | -0.14 | -2.55 | 2.06 |
|
03N 02E 11BABD1
USGS 433705116110601 |
Idaho | None | None | None |
|
04N 30E 07ADB1 USGS 12
USGS 434126112550701 |
Idaho | -0.01 | -0.25 | 0.34 |
|
05N 32E 36ADD1 USGS 21
USGS 434307112382601 |
Idaho | 0.14 | 0.89 | 0.61 |
|
05N 30E 07CAC1 USGS 138
USGS 434615112553501 |
Idaho | -0.01 | 3.51 | 9.11 |
|
05N 34E 09BDA1 USGS 4
USGS 434657112282201 |
Idaho | 0.06 | -0.33 | 0.37 |
|
06N 31E 13DBB1 USGS 24
USGS 435053112420801 |
Idaho | 0.02 | 1.8 | 1.45 |
|
07N 31E 34BDD1 USGS 25
USGS 435339112444601 |
Idaho | 0.05 | 0.28 | 0.44 |
