The Wisconsin Groundwater Flow System in Pierce, Polk and St. Croix Counties is an important aquifer system that supplies groundwater to the region. This system consists of two main types of aquifers: glacial-drift aquifers and bedrock aquifers. Glacial-drift aquifers are composed of glacial deposits, which are unconsolidated sediments that were deposited during the last glaciation. These deposits are typically sand and gravel, and provide excellent conditions for groundwater flow. The most productive glacial-drift aquifer in the region is the St. Croix Valley Aquifer, which is located in St. Croix County. Bedrock aquifers are composed of consolidated sedimentary rocks, such as sandstone and limestone. These aquifers have lower permeability than glacial-drift aquifers, but can still provide groundwater resources. The most productive bedrock aquifer in the region is the Kinnickinnic Formation, which is located in Pierce and Polk Counties. The Wisconsin Groundwater Flow System in Pierce, Polk and St. Croix Counties provides an important source of groundwater for the region, and is managed by the Wisconsin Department of Natural Resources. This system is monitored to ensure that groundwater resources are used sustainably, and to protect water quality.
Wisconsin Groundwater Flow System in Pierce, Polk and St. Croix Counties
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Nitrate is Wisconsin's most widespread groundwater contaminant. Nitrate contamination of groundwater is increasing in the state. About 90% of nitrate in groundwater is due to agricultural inputs, including manure spreading and fertilizer application.
Groundwater Flow and the Water Cycle It's more like water in a sponge. Gravity and pressure move water downward and sideways underground through spaces between rocks. Eventually it emerges back to the land surface, into rivers, and into the oceans to keep the water cycle going.
In our area, the average wells range from 60'-80' in depth depending on elevation and geology.
Sand and gravel aquifer These deposits are more than 300 feet thick in some places in Wisconsin.
Aquifers occur from near-surface to deeper than 9,000 metres (30,000 ft). Those closer to the surface are not only more likely to be used for water supply and irrigation, but are also more likely to be replenished by local rainfall.
Wisconsin's groundwater reserves are held in four principal aquifers: the sand and gravel aquifer, the eastern dolomite aquifer, the sandstone and dolomite aquifer, and the crystalline bedrock aquifer.
The Ogallala Aquifer is the largest aquifer in the U.S. and includes nearly all of Nebraska and large sections of Colorado, Kansas, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming.