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r , <br /> CMP Part 3A. Environmental Protection Plan <br /> ponds); (4) applying chemicals to precipitate out the orthophosphorus (alum <br /> treatments); (5) encouraging growth of certain aquatic plants; and (6) design of <br /> outlet structure to provide extended detention of large runoff events. Whether <br /> each of these enhancements can or should be incorporated is dependent on the <br /> desired level of control and other site specific conditions. <br /> Constructed wetlands have potential benefits as well as drawbacks. <br /> Additionally, the cost of constructing storniwater ponds and storm sewer systems <br /> is enormous compared to the cost of wetland preservation. Ve�etated buffers, <br /> �reen strips adjacent to hard surfaces. permeable pavements that incorporate <br /> runoff treatment features, and rain �ardens are just some of the additional tools <br /> available for supplementin� runoff mana�ement. <br /> �e-v� �Nutrient management technologies such as NURP ponds or alum <br /> treatments will give Orono an added tool to manage runoff from rural densities, <br /> but Orono cannot and will not rely solely on man-made systems for preserving <br /> water quality. <br /> ORONO'S NATURAL RESOURCES <br /> Orono's land forms are highly varied as the result of four separate glacial <br /> scourings. Surface features include islands, peninsulas, narrow land bridges, the <br /> lakes, bays and marshes, and a few shallow outwash basins. The highest <br /> elevations range from about 1060 feet above mean sea level in the northern part <br /> of the City down to the normal water level of Lake Minnetonka at elevation <br /> 929.4 MSL. Steep slopes and numerous glacial depressions add interest to the <br /> City's landscape but cause development limitations. <br /> The soils in the City of Orono (Map 3A-3 - use soils map from Orono NRI)) <br /> originated from drift materials deposited by meltwaters of the glaciers. Due to <br /> the range in type and location of deposited materials, the composition of the soils <br /> is complex and highly varied. Generally, the soil types consist primarily of clay <br /> and loam materials on the uplands and organic, wet materials in the lowland <br /> areas. Consequently, the ability of each soil type to adequately accommodate <br /> development varies considerably in Orono. Careful examination of each site is <br /> needed to determine the most appropriate land use for individual properties. <br /> Orono's native vegetation is �c .,^--;�a ^� ;*c '^ra ''^r-�c primarily woodland <br /> interspersed with localized areas of wet prairie marshlands. r'r^^^ �^a r �'�o <br /> Northern Orono and many areas along Lake Minnetonka's shore, contain vestiges <br /> of Minnesota's Big Woods with hardwood forests of oak, maple, elm, and <br /> basswood. Much of these have been thinned into scattered stands, as shown on <br /> Map 3A-4, but major forests remain in north central and north east Orono, <br /> especially around Lydiard Lake and in the Mn. DNR's Wolsfeld Woods and <br /> Wood Rill nature areas. In addition, 100 year old settlements have by now added <br /> mature stands of various evergreens and other decorative trees and shrubs. <br /> City of Orono CommuniTy Management Plan 2008-2030 Page 3A-8 <br />