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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 (%) |
|---|---|---|---|---|
|
CT-CL 223 CLINTON, CT
USGS 411832072325501 |
Connecticut | 3.02 | 35.76 | 23.72 |
|
CT-NT 15 NEWTOWN, CT
USGS 412429073165101 |
Connecticut | 1.77 | 18.28 | 33.03 |
|
CT-D 117 DURHAM, CT
USGS 412825072410501 |
Connecticut | 0.96 | 4.67 | 6.8 |
|
CT-SB 42 SOUTHBURY, CT
USGS 412916073121701 |
Connecticut | 0.7 | -1.07 | 8.53 |
|
CT-MB 32 MARLBOROUGH, CT
USGS 413535072253701 |
Connecticut | 0.88 | 12.59 | 48.1 |
|
CT-SC 22 SCOTLAND
USGS 414240072033201 |
Connecticut | 0.09 | 2.58 | 10.54 |
|
CT-MS 44 MANSFIELD, CT
USGS 414741072134501 |
Connecticut | 4.28 | 41.52 | 50.88 |
|
CT- MS 80 MANSFIELD, CT
USGS 414831072173002 |
Connecticut | 0.41 | 3.39 | 12.82 |