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<br />natural low lying areas creates a natural storage area for high waters and the lack of <br />structures permits unobstructed flow. <br /> <br />The relatively infrequent flooding in the valley can tend to cause citizens to believe major <br />flooding in the Red River Valley is a random occurrence which statistically should not <br />have happened or expected to occur again, but with greater examination reveals the Red <br />River Valley has many characteristics ideal for flooding (Schwert 2003). Unfortunately, <br />the county will likely be impacted by flooding in the future, making it only a question of <br />when, not if, flooding will occur. <br /> <br />Lakes, Reservoirs, and Wetlands <br /> <br />Cass County has 32 lakes found mostly in the west and southwest averaging 42 acres in <br />size and 10 artificially created lakes averaging 36 acres in size. These lakes and <br />reservoirs provide flood protection, irrigation, and recreation. The remaining sources of <br /> <br />surface water found in the county are wetlands; which are valuable for surface and <br />subsurface water storage, nutrient cycling, retention of sedimentation, and plant and <br /> <br />animal habitats. The fertile soils found in wetland areas make them productive areas for <br />farming and resulted in drainage and removal of many acres of wetlands; many of these <br />wetlands are now protected by federal and state laws. According to the National <br />Wetlands Inventory, Cass County has 21,036 acres of wetlands (excluding lakes and <br />rivers); of this area 7,693 acres are permanently or semi-permanently flooded (Figure <br /> <br />1.6). <br /> <br />Aquifers <br /> <br />The county has several larger aquifers being utilized to varying degrees which possess <br />limited additional development possibility. These aquifers include the West Fargo <br />Aquifer System (WF AS), the Page Aquifer, and the Sheyenne Delta Aquifer (Figure 1.6). <br /> <br />13 <br />