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The Citys sub-watershed areas are shown in Figure 2. There are a total of 16 sub-watersheds <br />within the City and two landlocked drainage areas. <br />The Citys storm sewer network and overall conveyance and treatment system is in place. <br />Future changes to the system will primarily involve retrofitting to address flooding problems, <br />to incorporate water quality treatment, or incorporate improvements at the time of <br />redevelopment. This storm sewer system consists of: <br />126 miles of pipe, <br />4719 catch basins, <br />2728 manholes, <br />128 ponds, <br />58 special features (infiltration, biofiltration, water reuse, raingardens, ect.) <br />739 inlets and outlets, and <br />six storm-sewer lift stations. <br />The citywide storm sewer map (Figure 3) shows the locations of the majority of these <br />facilities and general direction of flow through the system. <br />2.3Soils and Geology <br />A large portion of the landscape is dominated by Urban land-Zimm <br />and Urban land-Hayden-Kingsley complex (860C), as identified in the Ramsey County Soi <br />Survey. The Natural Resource Conservation Service (NRCS) also classifies soi <br />Hydrologic Soil Group (HSG) based on estimates of runoff potential (Figure 4). These are: <br /> Hydrologic Soil Group A  Low runoff potential  high infiltration rate <br /> Hydrologic Soil Group B  Moderate infiltration rate <br /> Hydrologic Soil Group C  Slow infiltration rate <br /> Hydrologic Soil Group D  High runoff potential  very slow infiltration rate <br />The surficial geology consists of unconsolidated glacial sediments deposited during the <br />Quaternary geologic period of two glacial ice lobes: the Superior lobe and the Grantsburg <br />sublobe of the Des Moines lobe. The glacial deposits found in Ramsey County are primarily <br />in the form of outwash, till, and stream and lake sediments rang <br />400 feet. Below the unconsolidated glacial sediment lies consolidated bedrock formed during <br />the early Paleozoic age. Bedrock units from youngest to oldest in Roseville include: De <br />Shale, Platteville-Glenwood Formation, St. Peter Sandstone, Prairie Du Chien Group <br />Jordan Sandstone. Maps of the surficial geology and bedrock geolfrom the Ramsey <br />County Geological Atlas can be found on Figure 5 and Figure 6, respectively. <br />2.4Land Use and Land Cover <br />The City of Roseville encompasses an area of 13.8 square miles which today is made up of <br />mixed-land uses including established neighborhoods, parks and open s <br />retail, commercial and industrial development. Some key aspects of the existing landuse <br />pattern are: <br />Low-density residential is the dominant land use. This form of housing occupies more <br />than 34% of Rosevilles total land area. <br />Roadways have been a major factor in shaping the development pattern of Roseville. <br />Business (commercial and industrial) uses are primarily concentrated in the western third <br />ComprehensiveSurface Water Management PlanROSEV120222 <br />City of RosevillePage 5 <br /> <br />