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<br />c. Existing Natural & Recreational Resources <br /> <br />The following information is a distillation of the important natural resource issues of the TCMP. It is based on a <br />significant amount of background information gathered by many local naturalists and resource professionals. <br />Figures 8 and 9 show much of this information in visual form. <br /> <br />1. Natural Characteristics of the Site <br /> <br />Geology, Soils and Topography <br /> <br />The high "hill" on TCMP, actually a kame, is the higbest point in Ramsey County and offers vistas in all <br />directions. This hill is of particular importance to the natural history of the area as a relict of the glacial landscape <br />that once occupied most of Minnesota. These glacial hills, known as kames, are a less common feature of the <br />landscape here than in other parts of Minnesota. The TCMP kame has been recorded in the Minnesota natural <br />history database as a geologic feature of the glacial period, and it provides a diverse environment for plant and <br />anirnallife fonns. <br /> <br />Upland soils surrounding the kame are a variety of well- to moderately well-draining loamy fme sands. The steeper <br />slopes of the kame are sandy loam with high erosion potential. The Rice Creek corridor contains poorly draining <br />loamy sand. The soil has low organic matter and drains rapidly, but flooding and a high water table make it a <br />seasonal wetland. <br /> <br />Erosion potential is severe in the disturbed gravel pit area atop the kame. Phase I measures being undertaken now <br />include revegetation with prairie sandreed grass in trial areas. Phase II measures will be implemented soon through <br />a 1992 SCS (Natural Resources Conservation Service) erosion control and surface-water management plan. <br /> <br />Surface Water <br /> <br />Surface water drains into the Rice Creek Watershed. Most of the water flows into the Marsden Lake wetlands, then <br />uorth, eventually to Rice Creek. In the northwest corner of the site water flows directly into Rice Creek. This <br />drainage includes water from the west slope of the kame. <br /> <br />The quality of the wetlands on TCAAP supports a diversity of wetland wildlife (see following discussion). <br />Maintaining good water quality requires management of both the quantity and quality of storm water runoff from <br />developed areas. Fluctuations in water levels above existing conditions will adversely impact habitat for several <br />wetland wildlife species, including Blanding's turtle and trumpeter swan. Proposed new stormwater runoff will <br />include treatment measures with features that avoid changes in existing water quality and levels in the wetlands. <br /> <br />Wetlands <br /> <br />The TCAAP wetlands, as well as Sunfish Lake, are identified by the State of Minnesota as protected waters and <br />wetlands. Three major wetland areas in particular are worth noting for their value within the natural community: <br />. Riparian wetlands are located along Rice Creek. Riparian wetlands buffer the flow of flood waters and diversify <br />the aquatic stream habitat. <br />. A large complex of small wetlands and interspersed uplaud extends in an arc around the north region of Turtle <br />Lake. The western tail of this complex extends onto the northern portion ofTCAAP. Interspersed upland and <br />wetland complexes are generally known for a high level of biodiversity -- that is, the numbers of species <br />typically finding a home in the upland-wetland edge is very bigh compared to other habitat areas. <br />. Marsden Lake is a large wetland complex of deep and shallow marsh, scrub-shrub, and wet meadow. The only <br /> <br />Camiros. Ltd.lSEH. Inc.lLHDL. Ltd. <br /> <br />TCAAP Framework Plan <br />Page 13 <br /> <br />Chapter II <br /> <br />I <br /> <br />J <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />I <br />.. <br /> <br />I <br /> <br />- <br /> <br />I <br /> <br />I <br /> <br />I <br /> <br />- <br /> <br />.- <br />I <br /> <br />I <br />