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35 Friends of the Mississippi River Camp Cozy Park NRMP <br />the 1938 and 2010 aerial photos, the water level was much lower in the 1930s, creating a <br />number of smaller islands. As previously noted, the land of Camp Cozy was previous used as a <br />resort with “flues” dug to divert flows from the river into the resort property to form a paddling <br />circuit. These channels have persisted over the last 90 years. Some of the flues have slightly <br />eroded into gullies and have also been an area of dumping over time. <br /> <br />Many land use changes have occurred on the site over the last century. Several buildings were <br />present in the 1930s, vestiges of the Camp Cozy resort of the 1920s. These buildings were later <br />repurposed into a dance hall, roller rink, diner, and bar that served the community into the <br />1930s. A bridge connected Camp Cozy to US Highway 10 to the south until the late 1950s, and <br />the resort structures remained on the property until this time when portions of the resort <br />burned, and the remainder was sold. It does not appear that the land was in agricultural <br />production during the last century, and the property sat vacant for many years until it was <br />donated to the city of Elk River in 1996 and a nature park was established. <br /> <br />Water Resources <br /> <br />A compilation of information related to the surface water resources at Camp Cozy and <br />associated issues such as erosion, impairments and groundwater infiltration is noted below. <br /> <br />The water table elevation at the property is 860-880 feet above sea level (FASL). With site <br />elevations ranging from 874 to 886 FASL, the depth to water table is quite shallow at 0-10 feet. <br />Extra care should be taken when using herbicides, fuels and other potential pollutants, given <br />this shallow depth to water table and the highly permeable sandy soils throughout much of the <br />site where management is planned. The entirety of the property is considered to be highly <br />sensitive to pollution due to its geology and depth to groundwater, as shown in Figure 14. <br />